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                           _Barr's Buffon._
                               ------

                       Buffon's Natural History.


                              CONTAINING
                        A THEORY OF THE EARTH,
                               A GENERAL
                           _HISTORY OF MAN_,
                     OF THE BRUTE CREATION, AND OF
                         VEGETABLES, MINERALS,
                               _&c. &c._



                           FROM THE FRENCH.
                     WITH NOTES BY THE TRANSLATOR.
                            IN TEN VOLUMES.

                               ========

                                VOL. X.

                               ========

                                London:

                      PRINTED FOR THE PROPRIETOR,
              AND SOLD BY H. D. SYMONDS, PATERNOSTER-ROW.
                                 1807.

            T. Gillet, Printer, Crown-Court, Fleet-Street.




                               CONTENTS.
                                  OF
                           THE TENTH VOLUME.


                                                                _Page_

  _Of the Degeneration of Animals_                                  1


          Nature and Properties of Minerals, Vegetables, &c.

  _Light, Heat, and Fire_                                          27
  _Of Air, Water, and Earth_                                       75
  _Experiments on the Progress of Heat in Mineral Substances_     109
  _A Table of the Relations of different Mineral Substances_      135
  _Observations on the Nature of Platina_                         156


         Experiments on Light, and on the Heat it can produce.

  _Invention of Mirrors to burn at great distances_                193
  _Observations and Experiments on Trees and other Vegetables_     245
  _On the Temperature of the Planets_                              279


                       General Views of Nature.
  _First View_                                                     325
  _Second View_                                                    343




BUFFON'S NATURAL HISTORY.




_OF THE DEGENERATION OF ANIMALS._


The deer-kind whose horns are a sort of wood, and of a solid texture,
although ruminating, and internally formed like those whose horns are
hollow and porous, seem to form a separate family, in which the elk is
the trunk, and the rein-deer, stag, axis, fallow-deer, and roe-buck,
are the lesser and collateral branches; for there are only six species
of animals whose heads are armed with branched horns that fall off and
are renewed every year. Independently of this generic character, they
resemble each other still more in formation and natural habitude; we
should, therefore, sooner expect mules from the stag or fallow-deer,
joined with the rein-deer or the axis, than from a union of the stag
with the cow.

We might be still better authorised to regard all the different kinds
of sheep and goats as composing but one family, since they produce
together mules, which immediately, and in the first generation, ascend
to the species of sheep. We might even add to this numerous family
of sheep and goats those of the gazelles and bubalus, which are not
less in number. The muflon, the wild goat, the chamois, the antelope,
the bubalus, the condoma, &c. seem to be the principal trunks of this
genus, which contains more than thirty different species, and the
others are only accessory branches which have retained the principal
characters of the stocks from which they issued; but which, at the same
time, have prodigiously varied by the influence of the climate, the
difference of the food, and by the state of slavery to which man has
reduced most animals.

The dog, the wolf, the fox, the jackal, and the isatis, form another
genus, the different species of which resemble each other so strongly,
especially in their internal conformation, and in the organs of
generation, that it is difficult to conceive why they do not intermix.
From the experiments which I made to form a union of the dog with the
wolf and fox, the repugnance to copulate seemed to proceed from the
wolf and fox rather than from the dog, that is, from the wild animal
and not from the tame; for those bitches which I put to the trial would
readily have permitted the wolf and fox, whereas the females of the
two latter would never suffer the approaches of the dog. The domestic
state seems to render animals less faithful to their species: It
gives them also a greater degree of heat and fecundity, for the bitch
generally produces twice a year, while the females of the wolf and fox
litter only once; and it is to be presumed, that those dogs which have
been left in desert countries, and which have so greatly multiplied in
the island of Juan Fernandes, and in the mountains of St. Domingo, &c.
produce only once a year, like the wolf and the fox. This circumstance,
if it were proved to be the fact, would fully establish the unity of
genus in these three animals, which resemble each other in conformation
so strongly as to oblige us to attribute their repugnance to some
external circumstances.

The dog seems to be the intermediate species between the fox and the
wolf. The ancients have stated, that the dog, in some countries, and
under particular circumstances, engenders with the wolf and fox. I was
desirous of verifying this assertion, and although I did not succeed
in the trials I made, yet we must not conclude that it is impossible,
for my experiments were with captive animals; and it is known that in
some species captivity alone is sufficient to extinguish desire, and
to give them a repugnance to copulation, even with their own kind;
consequently they would still more refuse to unite with individuals
of another species: but I am persuaded, that when in a state of
freedom, and deprived of his own female, the dog would unite with the
wolf and fox, particularly if he had become wild, lost his domestic
cast, and approached the manner and natural habits of these animals.
The fox and wolf, however, never unite, though they live in the same
climate and country, but support their species pure and unmixed; we
must, therefore, suppose a more ancient degeneration than history has
recorded, if they ever belonged to one species; it was for this reason
I asserted that the dog was an intermediate species between the fox and
wolf; and his species is also common, since it can unite with both; and
if any thing could shew that they all three originally sprang from the
same stock, it is this common affinity between the dog, the fox, and
the wolf, and which seems to bring their species nearer than all the
conformities in their figures and organization. To reduce the fox and
wolf, therefore, into one species, we must return to a state of nature
very ancient indeed; but in their present condition, we must look upon
the wolf and fox as the chief trunks in the genus of the five animals.
The dog, the jackal, and the isatis, are only lateral branches placed
between the two first; the jackal participates of the dog and wolf, and
the isatis of the jackal and fox. From a great number of testimonies
it appears that the jackal and the dog engender easily together; and
it is observable, from the description and history of the isatis, that
it almost entirely resembles the fox in its form and temperament,
that they are equally found in cold countries, but that, at the same
time, it inclines to the jackal in its disposition, continual barking,
clamorous voice, and the habit of always going in packs.

The shepherd's dog, which I have considered as the original stock of
every other dog, is, at the same time, that which approaches nearest
in figure to the fox. He is of the same size, and, like the fox, he
has erect ears, a pointed muzzle, and a strait trailing tail. He
also approaches the fox in voice, sagacity, and instinct. The dog,
therefore, may originally have been the issue of the fox, if not in
a direct, at least in a collateral line. The dog, which Aristotle
calls _canis-laconicus_, and which he affirms to have proceeded from
an union of the fox and dog, might, possibly, be the same as the
shepherd's dog, or, at least, it has more relation to him than to
any other dog. We might, therefore, be inclined to imagine, that the
epithet _laconicus_, left uninterpreted by Aristotle, was only given
to this dog because he was found in Laconia, a province of Greece; and
of which Lacedæmon was the capital; but if we attentively consider the
origin of this _laconic_ dog we shall perceive that the breed was not
confined to the country of Laconia, alone but must have been found in
every country where there were foxes; and this induces me to presume,
that the epithet _laconicus_ might possibly have been used by Aristotle
in a moral sense, to express the brevity and acuteness of his voice,
because he did not bark like other dogs, but had a shorter and shriller
note, like that of the fox. Now our shepherd's dog is that to which we
can justly apply this term of _laconic_, for of all dogs his voice is
the sharpest and most rarely employed. Besides, the characters which
Aristotle gives to his _laconic_ dog agree with those of the shepherd's
dog, and perfectly persuade me they are the same.

The genus of cruel and rapacious animals is one of the most numerous
and most diversified; evils here, as in other cases, seem to be
produced under every shape, and to assume various natures; the lion
and the tiger, being detached species, rank in the first line; all the
others, as the panther, the ounce, the leopard, the lynx, the caracal,
the jaguar, the cougar, the ocelot, the serval, the margai, and the
cat, compose only one cruel family, whose different branches are
more or less extended and diversified according to the difference of
climate. All these animals resemble each other in natural dispositions,
although they are very different with respect to size and figure.
They all have sparkling eyes, short muzzles, and sharp, crooked, and
retractile claws. They are all destructive, ferocious, and untameable.
The cat, which is the last and the least species, although reduced
to slavery, continues its ferocity, and is no less perfidious. The
wild cat has preserved the character of the family, and is as cruel
and mischievous as any of his larger kindred. They are all equally
carnivorous, and enemies to other animals. Man, with all his art and
power, has not been able to annihilate them: fire, steel, poison,
pits, and every method has been used against them without attaining
that point. As the individuals are very prolific, and the species
numerous, the efforts of man have been limited to keeping them at a
distance, and confining them in the deserts, whence they never sally
without spreading terror, and making great depredations. A single tiger
issuing from the forest is sufficient to alarm a multitude of people,
and oblige them to take up arms. What then would be the consequence
if these sanguinary animals came in numbers, like wolves or jackals,
to commit their depredations? Nature has given this instinct to timid
animals, but fortunately denied it to the bold tribes; they go singly,
and depend upon their courage and strength for their safety and
support. Aristotle observed, and justly remarked, that of all animals
furnished with talons not any of them are sociable, or go together in
troops.[A] This observation, which was then confined to four or five
species only, being all that were known in his time, is extended and
verified over ten or twelve other species since discovered. Other
carnivorous animals, such as the wolf, the fox, the dog, the jackal,
and the isatis, whose claws are straight, go mostly in troops, and are
all timid, and even cowardly.

[A] Nullum animal cui ungues adunci, gregatile esse perpendimus. Arist.
Hist. Anim. Lib. i. Cap. 1.

By thus comparing every quadruped, and ranking each with its proper
genus, we shall find, that the two hundred species of which we have
given the history, may be reduced to a small number of families, or
principal stems, from which it is not impossible all the others have
derived their origin.

To place this reduction in a regular method, we shall observe that
all the animals of the two continents, as well as all those peculiar
to the Old World, may be reduced to fifteen genera, and nine solitary
species. These genera are, first, the whole hoofed genus, properly
so called, which includes the horse, the zebra, and the ass, with
all the prolific and barren mules. 2. The large cloven-hoofed with
hollow horns, as the ox and the buffalo, with their varieties. 3. The
small cloven-hoofed animals with hollow horns, such as the sheep,
the goat, the gazelle, the antelope, and every other species which
participates of their nature. 4. The cloven-hoofed with solid horns,
which are shed and renewed every year; this family contains the elk,
the rein-deer, the stag, the fallow-deer, the axis, and the roe-buck.
5. The ambiguous cloven-hoofed, which is composed of the wild boar,
and all the varieties of the hog, such as that of Siam, with a hanging
belly, that of Guinea, with long ears, pointed and turned backwards,
and that of the Canary islands with thick and long tusks, &c. 6. The
very extensive race of digitated carnivorous animals with crooked and
retractile claws, in which we must comprehend the panther, leopard,
guepard, ounce, serval, and cat, with all their varieties. 7. The
digitated carnivorous animals with straight and fixed claws, which
include the wolf, fox, jackal, isatis, and the dog, with all their
varieties. 8. The digitated carnivorous animals with fixed claws, and
a pouch under their tails. This consists of the hyæna, civet, zibet,
badger, &c. 9. The digitated carnivorous animals with long bodies, five
toes to each foot, and the great toe, or thumb, divided from the rest;
this genus is composed of the ferret, martin, pole-cat, weasel, sable,
ichneumon, &c. 10. The numerous family of digitated quadrupeds which
have two large incisive teeth in each jaw, and no bristles on their
bodies; this contains the hare, rabbit, and every kind of squirrels,
dor-mice, marmots, and rats. 11. The digitated quadrupeds, whose bodies
are covered with spiny quills, as the porcupine and hedge-hog. 12. The
digitated animals covered with scales, as the long and short-tailed
manis, or scaly lizards. 13. The amphibious digitated genus, which
includes the beaver, otter, musk-rats, walrus, and seals. 14. The
four-handed genus, which comprehends the apes, baboons, monkeys,
makis, loris, &c. 15. The winged quadrupeds, which includes bats, &c.
with all their varieties. The nine detached species are the elephant,
rhinoceros, hippopotamus, giraffe, camel, lion, tiger, bear, and mole,
which are all subject to a greater or smaller number of varieties.

Of those fifteen genera, and nine detached species, seven genera, and
two species are common to both continents. The two species are, the
bear and the mole; and the seven genera are, 1. The great cloven-hoofed
with hollow horns, for the ox is found in America, under the form of
the bison. 2. The cloven-hoofed, with solid horns, for the elk exists
in Canada, under the name of original; the rein-deer, under that of
caribou; and stags, fallow-deer, and roe-bucks, are found in all the
provinces of North America. 3. The digitated carnivorous animals with
fixed claws; for the wolf and fox are found in the New World as well as
in the Old. 4. The digitated animals with long bodies, as the weasel,
martin, and pole-cat, are met with in America as well as in Europe. 5.
We find also in America, part of the digitated genus with two large
incisive teeth in each jaw, as the squirrels, marmots, rats, &c. 6.
The digitated amphibious genus, as the walrus, seal, beaver, and otter,
exist in the North of the New Continent. 7. The winged genus exist also
in America, as the bat and vampire.

There remains, therefore, only eight genera, and five detached species,
which are peculiar to the Old Continent. These eight genera are, 1.
The whole-hoofed, properly so called, for neither the horse, ass,
zebra, nor mule, were met with in the New Continent. 2. The small
cloven-hoofed beasts with hollow horns; for sheep, goats, gazelles, or
antelopes existed in America. 3. The family of hogs; for the species
of wild boar is not to be found in America; and although the pecari,
and its varieties, are related to this family, yet they differ in a
sufficient number of remarkable characters to justify their separation.
4. It is the same with carnivorous animals with retractile claws; we do
not meet with either the panther, leopard, guepard, ounce, or serval,
in America; and although the jaguar, couguar, ocelot, and margai, seem
to belong to this family, there is not, one of these species of the
New World found in the Old, nor one of the Old to be met with in the
New. 5. The same remark may be applied to the digitated quadrupeds
whose bodies are covered with prickles; for although the coendou and
the urson approach very nigh to this genus, nevertheless, these species
are very different from those of the porcupine and hedge-hog. 6. The
digitated carnivorous genus with fixed claws, and a pouch under the
tail; for the hyæna, civets, and the badger, do not exist in America.
7. The four-handed genus; for neither apes, baboons, monkeys, nor
makis, have ever been seen in America. The sapajous, sagons, opossums,
&c. although quadrumanous, yet they essentially differ from those of
the Old Continent. 8. The digitated genus whose bodies are covered with
scales; for none of the scaly lizards are found in America, and the
ant-eaters, to whom they may be compared, are covered with hair, and
differ too much from the scaly lizards to be considered of the same
family.

Of the nine detached species, seven, namely, the elephant, rhinoceros,
hippopotamus, giraffe, camel, lion, and tiger, are found only in
the Old World; and two, viz. the bear and mole, are common to both
continents.

If we, in the same manner, enumerate the animals which are peculiar to
the New World, we shall find, that there are about fifteen different
species which may be reduced to ten genera and four detached species.
These four species are the tapir, the cabiai, the lama, and the pecari;
but there is only the tapir we can absolutely term detached; for the
pecari has varieties; and the pacos may be united to the lama, and
the Guinea hog to the cabiai. The ten genera are, 1. Eight species
of sapajous. 2. Six species of sagoins. 3. The opossums, phalangers,
tarsiers, &c. 4. The jaguars, couguars, ocelots, margais, &c. 5. Three
or four species of coatis. 6. Four or five species of mouffettes. 7.
The agouti genus, which comprehends the acouchi, the paca, the aperea,
and the tapeti. 8. That of the armadillos, which consists of seven or
eight species. 9. Two or three species of ant-eaters; and, 10thly, The
sloth, of which we are acquainted with but two species.

Now these ten genera, and four detached species, to which the fifty
species of animals peculiar to the New World may be reduced, though
they differ from those of the Old Continent, nevertheless have some
relations which seem to indicate some common affinity in their
formation, and lead us to causes of degeneration, more ancient than any
of the rest. We have already made the general remark, that all animals
of the New World were much smaller than those of the Old. This great
diminution in size, whatever maybe the cause, is a primary kind of
degeneration, which could not be made without having a great influence
on the figure of the animal, and we must not lose sight of this effect
in comparing them together.

The largest is the tapir, which though not bigger than the ass, can
only be compared with the elephant, rhinoceros, and hippopotamus; he
claims the first place for size in the New Continent, as the elephant
does in the Old. Like the rhinoceros, his upper lip is muscular and
projecting; and, like the hippopotamus, he often enters the water.
In some respects he represents them all three, and his figure, which
partakes more of the ass than of any other animal, seems to be as
degraded as his stature is diminished. The horse, the ass, the zebra,
the elephant, the rhinoceros, and the hippopotamus, had no existence
in America; neither was there an animal in this New Continent which
could be compared with them, either with respect to size or figure. The
tapir appears to have some affinity to the whale, but he is so mixed,
and approaches so little to any one of them, that it is not possible
to attribute his origin to the degradation of any particular species.
And, notwithstanding these trifling relations which he is found to have
with the rhinoceros, the hippopotamus, and the ass, we must look on him
not only as a peculiar species, but even as a single genus.

The tapir, therefore, does not belong to any species of the Old
Continent, and scarcely does he bear any characters which approximate
him to those animals with which we have just been comparing him. The
nature of the cabiai is likewise averse from our comparison: externally
he has no resemblance with any other animal, and only approaches the
Indian hog of the same continent, by his internal parts, and both
species are absolutely different from all those of the Old Continent.

The lama and the pacos appear to have more significant marks of their
ancient parents: the first with the camel, and the second in the sheep.
The lama, like the camel, has a long neck and legs, slender head, and
the upper lip divided. He resembles the latter also by his gentle
manners, servility of disposition, endurance of thirst, and aptness
for labour. This was the first and most useful domestic animal of the
Americans: they made use of him to carry burdens, in the same manner
as the Arabs do the camel. Here therefore are sufficient resemblances
in the nature of these animals, to which we can yet add the permanent
marks of labour; for though the back of the lama is not deformed by
hunches like that of the camel, he, nevertheless, has callosities on
his breast, occasioned by the like habit he is used to of resting on
that part of his body. Yet, notwithstanding all these affinities, the
lama is a very distinct and different species from the camel. He is
much smaller, not exceeding a fourth or a third part of the camel's
magnitude. The shape of his body, and the quality and colour of his
hair, are also very different. His temperament is still more so; for
he is a phlegmatic animal, and delights only to live on the mountains,
whereas the camel is of a dry temperament, and willingly inhabits the
most scorching sands. On the whole, there are more specific differences
between the camel and the lama, than between the camel and the giraffe.
These three animals have many characters in common, by which they
might be referred to one genus, but, at the same time, they differ so
much in other respects, that we cannot suppose them to be the issue of
one another; they are, therefore, only neighbours and not relations.
The height of the giraffe is nearly double that of the camel, and
the camel double that of the lama. The two first belong to the Old
Continent, and form separate species. The lama, therefore, which is
only found in the New, must be a distinct species from both.

It is not the same with respect to the pecari, for though a different
species from the hog, he, nevertheless, belongs to the same genus. He
resembles the hog in shape, and every external appearance, and only
differs from it in some trifling characters, such as the aperture on
his back, shape of the stomach, intestines, &c. We might, therefore, be
led to suppose that this animal sprung from the same stock as the hog,
and that he formerly passed from the Old World to the New, where, by
the influence of the soil, he had degenerated to so great a degree as
now to constitute a distinct species.

With regard to the pacos, though it appears to have some affinities
with the sheep, in its wool and habit of body, yet it differs so
greatly in every other respect, that this species cannot be looked
on either as neighbours or allies. The pacos is rather a small lama,
and has not a single mark which indicates its having passed from one
continent to the other. Thus of the four detached species peculiar to
the New World, three, namely, the tapir, the cabiai, and the lama, with
the pacos, appear to belong originally to this continent, whereas the
pecari, which forms the fourth, seems to be only a degenerated species
of the hog, and to have formerly derived its origin from the Old
Continent.

By examining and comparing, in the same manner, the ten genera, to
which we have reduced the other animals peculiar to South America, we
shall discover, not only singular relations in their nature, but marks
of their ancient origin and degeneration. The sapajous and sagoins bear
so great a resemblance to the monkeys, that they are commonly included
under that name. We have proved, however, that their species, and even
their genera, are different. Besides, it would be very difficult to
conceive how the monkeys of the Old Continent could assume in America
a different-shaped visage, a long, muscular, and prehensile tail,
a large partition between the nostrils, and other characters, both
specific and generic, by which we have distinguished and separated them
from the sapajous. But as the monkeys, apes, and baboons, are only
found in the Old Continent, we must look upon the sapajous and sagoins
as their representatives in the New, for these animals have nearly
the same form, as well externally as internally, and also have many
things in common in their natural habits and dispositions. It is the
same with respect to the makis, none of which are found in America,
yet they seem to be represented there by the opossums, or four-handed
animals, with pointed muzzles, which are found in great numbers in the
New Continent, but exist not in the Old. We must, however, observe,
that there is much more difference between the nature and the form of
the makis, and of these four-handed American animals, than between the
monkeys and the sapajous; and that there is so great a distance between
the opossums and the maki that we cannot form an idea that the one
ever proceeded from the other, without supposing that degeneration can
produce effects equal to those of a new nature; for the greatest number
of these American four-handed animals have a pouch under the belly, ten
incisive teeth in each jaw, and a prehensile tail; whereas the maki has
a flaccid tail, no pouch under the belly, and only four incisive teeth
in the upper jaw, and six in the lower; therefore, though all these
animals have hands and fingers of the same form, and also resemble each
other in the elongation of the muzzle, yet their species, and even
their genera, are so different, that we cannot imagine them to be one
and the same issue, or that such great and general disparities have
ever been produced by degeneration.

On the other hand, the tigers of America, which we have indicated by
the names of jaguars, couguars, ocelots, and margais, though different
in species from the panther, leopard, ounce, guepard, and serval, of
the Old Continent, are, nevertheless, of the same genera. All these
animals greatly resemble each other, both externally and internally;
they have also the same natural dispositions, the same ferocity, the
same vehement thirst for blood, and what approximates them still nearer
in genus, those which belong to the same continent differ more from
each other than from those of the other Continent. For instance, the
African panther differs less from the Brasilian jaguar than the latter
does from the couguar, though they are natives of the same country. The
Asiatic serval, and the margai of Guiana, likewise differ less from
one another than from the species peculiar to their own continents.
We, therefore, may justly suppose, that these animals had one common
origin, and that, having formerly passed from one continent to the
other, their present differences have proceeded only from the long
influence of their new situation. The mouffettes, or stinkards, of
America, and the pole-cat of Europe, seem to be of the same genus. In
general, when a genus is common to both continents the species which
compose it are more numerous in the Old than in the New; but in this
instance it is quite the reverse, for there are four or five kinds
of pole-cats in America, while we have only one, the nature of which
is inferior to that of all the rest; so that the New World, in its
turn, seems to have representatives in the Old; and if we judged only
from the fact, we might think these animals had taken the opposite
road, and passed from America to Europe. It is the same with respect
to some other species. The roe-bucks and the fallow-deer, as well as
the stinkards, are more numerous, larger, and stronger in the New
Continent than in the Old; we might, therefore, imagine them to be
originally natives of America; but as we cannot doubt that every animal
was created in the Old Continent, we must, consequently, admit of
their migration from the Old to the New World, and at the same time
suppose, that instead of having degenerated, like other animals, they
have improved their original nature by the influence of the soil and
climate.

The ant-eaters, which are singular animals, and of which there are
three or four species in the New World, seem also to have their
representatives in the Old. The scaly lizards resemble them in the
peculiar character of having no teeth, and of being obliged to put out
their tongues and feed upon ants; but if we would suppose them to have
one common origin, it is strange, that instead of scales, with which
they are covered in Asia, they are clothed with hair in America.

With respect to the agoutis, pacos, and other animals of the seventh
genus peculiar to the New Continent, we can only compare them with the
hare and rabbit, from which, however, they all differ in species. What
renders their being of a common origin doubtful is, the hare being
dispersed almost over every climate of the Old Continent, without
having undergone any other alteration than in the colour of its hair.
We cannot, with any foundation, therefore, imagine that the climate of
America has so far changed the nature of our hares to so great a degree
as to make them tapetis or apereas, which have no tail; or agoutis with
pointed muzzles, and short round ears; or pacos, with a large head,
short ears, and a coarse hair marked with white stripes.

On the whole, the coatis, the armadillos, and the sloths, are so
different, not only in species, but also in genus, from every animal
of the Old World, that we cannot compare them with any one; it is
also impossible to refer them to any common origin, or attribute to
the effects of degeneration the prodigious differences found in their
nature from that of every other animal.

Thus, of ten genera, and four detached species, to which we have
endeavoured to reduce all the animals peculiar to the New World, there
are only two, the genus of the jaguars, ocelots, &c. and the species
of the pecari, with their varieties, which can with any foundation
be connected with the animals of the Old Continent. The jaguars and
ocelots may be regarded as a species of the leopard or panther, and
the pecari as a species of hog. After these are five genera and one
detached species, namely the species of the lama, and the genera of
sapajous, sagoins, stinkards, agoutis, and ant-eaters, which may be
compared, though in a very distant and equivocal manner, with the
camel, monkey, pole-cat, hare, and scaly lizards. There then remain
four genera and two detached species, namely, the opossums, the
coatis, the armadillos, the sloths, the tapir, and the cabiai, which
can neither be referred nor compared to any genera or species of the
Old Continent. This sufficiently proves that the origin of these
animals, peculiar to the New world, cannot be attributed merely to
degeneration. However, great and powerful the effects of degeneration
may be supposed, we cannot, with any appearance of reason, persuade
ourselves that these animals were originally the same as those of the
Old Continent. It is more reasonable to imagine that the two continents
were formerly joined, and that those species which inhabited the New
World, because they found the climate and soil most suitable to their
nature, were separated from the rest by the irruption of the sea when
it divided Asia from America. This is a natural cause, and similar ones
might be conceived which would produce the same effect; for example, if
the sea should make an irruption from the eastern to the western side
of Asia, and thus separate the southern parts of Africa and Asia from
the rest of the Continent, all the animals peculiar to the southern
countries, such as the elephant, the rhinoceros, the giraffe, the
zebra, the orang-outang, &c. would be, relatively to the others, the
same as those of South America at present are; they would be entirely
separated from the animals of the temperate countries, and could not
be referred to an origin common to any of the species or genera which
inhabit these countries, on the sole foundation that some imperfect
resemblances, or distant relations, might be observed between them.

We must, therefore, to find out the origin of these animals, turn back
to the time when the two continents were not separated, and refer to
the first changes which happened on the surface of the globe. We must,
at the same time, place before our view the two hundred species of
quadrupeds as constituting thirty-eight families; and although this is
not the state of nature, such as it is come down to us, and as we have
represented it, but, on the contrary, a much more ancient state, which
we can only attain by inductions and relations nearly as fugitive as
time, which seems to have effaced their traces, we have endeavoured, by
facts and monuments still existing, to return to those first ages of
nature, and to exhibit those epochas which appear to be most clearly
indicated.




AND PROPERTIES OF MINERALS, VEGETABLES, &c.




LIGHT, HEAT, AND FIRE.


All the powers of Nature with which we are acquainted, may be reduced
to two primitive forces; the one which causes weight, and that which
produces heat. The force of impulsion is subordinate to them; it
depends on the first for its particular, and on the latter for its
general effects. As impulsion cannot exercise itself but by the means
of a spring, and the spring only acts by virtue of the force which
approximates the remote parts, it is clear, that to perform its
power it has need of the concurrence of attraction: for if matter
ceased to attract, if bodies lost their coherence, every spring would
be destroyed, every motion intercepted, and every impulsion void;
since motion cannot transmit itself from one body to another but by
elasticity, it is demonstrable, that one body absolutely hard and
inflexible, would be absolutely immoveable, and entirely incapable
of receiving the action of another. Attraction being a general and
permanent effect, impulsion, which in most bodies is neither constant
nor fixed, depends on it as a particular effect; for, if all impulsion
were destroyed, attraction would still equally subsist and act; it is,
therefore, this essential difference which makes impulsion subordinate
to attraction in all inanimate and purely passive matter.

But this impulsion depends still more immediately, and generally, on
the power which produces heat; for it is principally by the means
of heat, that impulsion penetrates organized bodies; it is by heat
that they are formed, grow, and develope themselves. We may refer to
attraction alone all the effects of inanimate matter; and in this same
power of attraction, joined to that of heat, every phenomena of live
matter. By live matter I understand not only every thing that lives,
or vegetates, but also every living organic molecule, dispersed in the
waste or remains of organized bodies. In it I comprehend also light,
heat, fire, and all matter which appears to be active in itself. Now
this live matter always tends from the centre to the circumference,
whereas brute or inanimate matter tends from the circumference to the
centre. It is an expansive power which animates the live matter, and
it is an attractive force to which the inanimate matter is obedient.
Although the directions of these two powers be diametrically opposite,
yet they balance themselves without ever being destroyed, and from the
combination of these two powers equally active, all the phenomena of
the universe result.

But it may be said, by reducing all the powers of Nature to attraction
and expansion, without giving the cause of either, and by rendering
impulsion, (which is the only force whose cause is known and
demonstrated to our senses) subordinate to both, do you not abandon
a clear idea, and substitute two obscure hypotheses in its place? To
this I answer, that as we know nothing except by comparison, we shall
never have an idea of what general effect will produce, because such
an effect belonging to every thing, we should be unable to compare it
to any, and consequently there is no hope of ever knowing the cause or
reason why all matter attracts, although we are sensible such is the
fact. If, on the contrary, the effect were particular, like that of the
attraction of the loadstone and steel, we might expect to discover the
cause, because it might be compared to other particular effects. To ask
why matter is extended, heavy, and impenetrable, are ill-conceived
propositions, and merit not an answer; it is the same with respect
to every particular property, when it is essential to the subject,
and we might as well be interrogated why red is red? The philosopher
becomes a child when he puts such questions; and however much they may
be forgiven to the last, the former ought to exclude them from his
thoughts.

It is sufficient that the forces of attraction and expansion are two
general, real, and fixed effects, for us to receive them for causes
of particular ones; and impulsion is one of these effects, which we
must not look upon as a general cause, known and demonstrated by our
senses, since we have proved that this force of impulsion cannot exist
nor act, but by the means of attraction, which does not fall upon our
senses. Nothing is more evident, nay, certain, than the communication
of motion by impulsion; it is sufficient for one body to strike another
to produce this effect. But even in this sense, is not the cause of
attraction most evident, and that motion, in all cases, belongs more to
attraction than impulsion?

The first reduction being made, it might perhaps be possible to adduce
a second, and to bring back the power even of expansion to that of
attraction, insomuch that all the forces of matter would depend solely
on a primitive one; at least this idea seems to be worthy of that
sublime simplicity with which nature works. Now cannot we conceive
that this attraction changes into repulsion every time that bodies
approach near enough to rub together, or strike one against the
other? Impenetrability, which we must not regard as a force, but as a
resistance essential to matter, not permitting two bodies to occupy
the same place, what must happen when two molecules, which attract the
more powerfully as they approach nearer, suddenly strike against each
other? Does not then this invincible resistance of impenetrability,
become an active force, which, in the contact, drives the bodies with
as much velocity, as they had acquired at the moment they touched? And
from hence the expansive force will not be a particular force opposed
to the attractive one, but an effect derived therefrom. I own, that we
must suppose a perfect spring in every molecule, and in every atom of
matter, to have a clear conception how this change of attraction into
repulsion is performed. But even this is sufficiently indicated by
facts; the more matter is attenuated, the more it takes a spring. Earth
and water, which are the most gross aggregates, have a less spring
than air; and fire, which is the most subtle of all the elements, is
also that which has the most expansive force. The smallest molecules
of matter, the smallest atoms with which we are acquainted are those
of light, and we are sensible of their being perfectly elastic, since
the angle under which the light is reflected, is always equal to that
under which it comes. We may therefore infer, that all the constitutive
parts of matter in general, are a perfect spring; and that this spring
produces all the effects of the expansive force, every time that bodies
strike by meeting in opposite directions.

We know of no other means of producing fire, but by striking or rubbing
bodies together[B]; since by supposing man without any burning glasses,
and without actual fire, he will have no other means of producing it;
for the fire produced by uniting the rays of light, or by application
of fire already produced, had the same origin.

[B] The fire, which arises from the fermentation of herbs heaped
together, and which manifests itself in effervescences, is not an
exception that can be opposed to me, since this production of fire
depends, like all the rest, from the action of the shock of the parts
of matter one against the other.

Expansive force, therefore, in reality might be only the re-action
of the attractive, a re-action which operates every time that the
primitive molecules of matter, always attracted one by the other,
happen immediately to touch; for then it is necessary, that they be
repelled with as much velocity as they had acquired in a contrary
direction, at the moment of contact; and when these molecules are
absolutely free from all coherence and only obey the motion alone
produced by their attraction, this acquired velocity is immense in the
point of contact. Heat, light, and fire, which are the greatest effects
of expansive force, will be produced every time that bodies are either
artificially or naturally divided into very minute parts, and meet in
opposite directions; and the heat will be so much the more sensible,
the light so much the more bright, the fire so much the more violent,
according as the molecules are precipitated one against the other with
more velocity by their force of mutual attraction.

From the above it must be concluded, that all matter may become
light, heat, and fire; and that this matter of fire and light is
not a substance different from every other, but preserves all its
essential qualities; and even most of the attributes of common matter,
is evidently proved by, first, light, though composed of particles
almost infinitely minute, is, nevertheless, still divisible, since
with the prism we separate the rays, or different coloured atoms one
from another. Secondly, light, though in appearance endowed with a
quality quite opposite to that of weight, that is, with a volatility
which we might think essential, is, nevertheless, heavy like all
matter, since it bends every time it passes near other bodies, and
finds itself inclined to their sphere of attraction. It is very
heavy, relatively to its volume, which is very minute, since the
immense velocity with which light moves in a direct line, does not
prevent it from feeling sufficient attraction near other bodies, for
its direction to incline and change in a manner very sensible to our
eyes. Thirdly, the substance of light is not more simple than all
other matter, since it is composed of parts of unequal weight; the red
rays are much heavier than the blue; and between these two extremes
there are an infinity of intermediate rays, which approach more or
less the weight of the red, or the lightness of the blue according to
their shades. All these consequences are necessarily derived from the
phenomena of the inflection of light, and of its refraction, which, in
reality, is only an inflexion which operates when light passes across
transparent bodies. Fourthly, it may be demonstrated, that light is
massive, and that it acts, in some cases, as all other bodies act;
for, independently of its ordinary effect, which is to shine before
our eyes, and by its own action, always accompanied with lustre, and
often with heat, it acts by its mass when it is condensed, and it acts
to the point of putting in motion heavy bodies placed in the focus of a
good burning glass: it turns a needle on a pivot placed in its focus:
it displaces leaves of gold or silver before it melts or even sensibly
heats them. This action, produced by its mass, precedes that of heat:
it operates between the condensed light and the leaves of metal in
the same manner as it operates between two other bodies which become
contiguous, and, consequently, have still this property in common with
all other matter. Fifthly, light is a mixture, like common matter, not
only of more gross and minute parts, more or less heavy or moveable,
but also differently shaped. Whoever has observed the phenomena which
Newton calls _the access of easy reflection_, and of _easy transmission
of light_; and on the effects of double refraction of rock and Iceland
chrystal, must have perceived that the atoms of light have many sides,
many different surfaces, which, according as they present themselves,
constantly produce different effects.

This, therefore, is sufficient to demonstrate that light is neither
particular nor different from common matter; that its essence, and
its essential properties are the same; and that it differs only from
having undergone, in the point of contact, the repulsion whence its
volatility proceeds; and in the same manner as the effect of the force
of attraction extends, always decreasing as the space augments, the
effects of repulsion extend and decrease the more, but in an inverted
order, insomuch that we can apply to the expansive force all that is
known of the attractive. These are two instruments of the same nature,
or rather the same instrument, only managed in two opposite directions.

All matter will become light, for if all coherence were destroyed
it would be divided into molecules sufficiently minute, and these
molecules, being at liberty, will be determined by their mutual
attraction to rush one against the other. In the moment of the shock
the repulsive force will be exercised, the molecules will fly in all
directions with an almost infinite volatility, which, nevertheless,
is not equal to their velocity acquired in the moment of contact, for
the law of attraction being augmented as the space diminishes, it is
evident, that at the contact the space is always proportionable till
the square of the distance becomes nil, and, consequently, the velocity
acquired by virtue of the attraction must at this point become almost
infinite: and it would be perfectly so if the contact were immediate,
and, consequently, the distance between the two bodies void; but there
is nothing in nature entirely nil, and nothing truly infinite; and all
that I have observed of the _infinite_ minuteness of the atoms which
constitute light, of their _perfect_ spring, and of the _nil_ distance
in the moment of contact, must be understood only relatively. If this
metaphysical truth were doubted, a physical demonstration may be given.
It is pretty generally known that light employs seven minutes and a
half to come from the sun to the earth; supposing, therefore, the sun
at thirty-six millions of miles, light darts through this enormous
distance in that short space, that is (supposing its motion uniform),
80,000 miles in one second. But this velocity, although prodigious,
is yet far from being infinite, since it is determinable by numbers.
It will even cease to appear so prodigious, when we reflect on the
celerity of the motion of the comets to their perihelia, or even that
of the planets, and by computing that, we shall find that the velocity
of those immense masses may pretty nearly be compared to that of the
atoms of light.

So, likewise, as all matter can be converted into light by the
division and expulsion of its parts, when they feel a shock one against
another, we shall find that all the elements are convertible; and if it
have been doubted whether light, which appears to be the most simple
element, may be converted into a solid substance, it is because we have
not paid sufficient attention to every phenomena, and were infected
with the prejudice, that being essentially volatile it can never become
fixed. But it is plain that the fixity and volatility depend on the
same attractive force in the first case, and become repulsive in the
second; and from thence are we led to think that this change of matter
into light, and from light into matter, is one of the most frequent
operations of Nature.

Having shewn that impulsion depends on attraction; that the expansive
force, like the attractive, becomes negative; that light, heat, and
fire, are only modes of the common existing matter; in one word, that
there exists but one sole force, and one sole matter, ever ready to
attract or repel, according to circumstances; let us see how, with this
single spring, and this single subject, Nature can vary her works, _ad
infinitum_. In a general point of view, light, heat, and fire, only
make one object, but in a particular point of view they are three
distinct objects, which, although resembling in a great number of
properties, differ nevertheless in a few others, sufficiently essential
for us to consider them as three distinct things.

Light, and elementary fire, compose, it is said, only one and the same
thing. This may be, but as we have not yet a clear idea of elementary
fire we shall desist from pronouncing on this first point. Light and
fire, such as we are acquainted with, are two distinct substances,
differently composed. Fire is, in fact, very often luminous, but it
sometimes also exists without any appearance of light. Fire, whether
luminous or obscure, never exists without a great heat, whereas light
often burns with a noise without the least sensible heat. Light appears
to be the work of nature while fire is only the produce of the industry
of man. Light subsists of itself, and is found diffused in the immense
space of the whole universe. Fire cannot subsist without food, and
is only found in some parts of this space where man preserves it,
and in some parts of the profundity of the earth, where it is also
supported by suitable food. Light when condensed and united by the art
of man, may produce fire, but it is only as much as it lets fall on
combustible matters. Light is therefore no more, and in this single
instance, only the principle of fire and not the fire itself: even this
principle is not immediate, for it supposes the intermediate one of
heat, and which appears to appertain more than light to the essence of
fire. Now heat exists as often without light as light exists without
heat: these two principles might, therefore, appear not to bind them
necessarily together; their effects are not contemporary, since in
certain circumstances we feel heat long before light appears, and in
others we see light long before we feel any heat. Hence is not heat
a mode of being, a modification of matter, which, in fact, differs
less than all the rest from that of light, but which can be considered
apart, and still more easily conceived? It is, nevertheless, certain,
that much fewer discoveries have been made on the nature of heat than
on that of light; whether man better catches what he sees than what
he feels; whether light, presenting itself generally as a distinct
and different substance from all the rest, has appeared worthy of a
particular consideration; whereas heat, the effect of which is the most
obscure, and presents itself as a less detached and less simple object,
has not been regarded as a distinct substance but as an attribute of
light and fire.

The first thing worthy of remark, is, that the seat of heat is quite
different from that of light: the latter occupies and runs through
the void space of the universe; heat, on the contrary, is diffused
through all solid matter. The globe of the earth, and the whole matter
of which it is composed, have a considerable degree of heat. Water has
its degree of heat which it does not lose but by losing its fluidity.
The air has also heat, which we call its temperature, and which varies
much, but is never entirely lost, since its springs subsist even in
the greatest cold. Fire has also its different degrees of heat, which
appear to depend less on its own nature, than on that of the aliments
which feed it. Thus all known matter possesses warmth; and, hence, heat
is a much more general affection than that of light.

Heat penetrates every body without exception which is exposed to it,
while light passes through transparent bodies only, and is stopped and
in part repelled, by every opaque one. Heat, therefore acts in a much
more general and palpable manner than light, and although the molecules
of heat are excessively minute, since they penetrate the most compact
bodies, it seems, however, demonstrable, that they are much more gross
than those of light; for we make heat with light, by collecting it in
a great quantity. Besides, heat acting on the sense of feeling, it is
nececssary that its action be proportionate to the grossness of this
sense, the same as the delicacy of the organs of sight appears to be to
the extreme fineness of the parts of light; these parts move with the
greatest velocity, and act in the instant at immense distances, whereas
those of heat have but a slow progressive motion, and only extend to
small intervals from the bodies whence they emanate.

The principle of all heat seems to be the attrition of bodies; all
friction, that is, all contrary motion between solid matters produces
heat; and if the same effect do not happen to fluids, it is because
their parts do not touch close enough to rub one against the other;
and that, having little adherence between them, their resistance to
the shock of other bodies is too weak for the heat to be produced to
a sensible degree; but we often see light produced by an attrition of
a fluid, without feeling any heat. All bodies whether great or little
become heated as soon as they meet in a contrary direction; heat is,
therefore, produced by the motion of all palpable matter; while the
production of light, which is also made by motion, but in a contrary
direction, supposes also the division of matter into very minute parts:
and as this operation of Nature is the same with respect to both, we
must conclude, that the atoms of light are solid of themselves, and are
hot at the moment of their birth. But we cannot be equally certain,
that they preserve their heat in the same degree as their light, nor
that they cease to be hot before they cease to be luminous.

It is well known, that heat grows less, or cold becomes greater, the
higher we ascend on the mountains. It is true that the heat which
proceeds from the terrestrial globe, is of course sensibly less on
those advanced points, than it is on the plains; but this cause is not
proportionable to the effect; the action of heat, which emanates from
the terrestrial globe, not being able to diminish but by the square of
the distance, it does not appear that at the height of half a mile,
which is only the three thousandth part of the semi-diameter of the
globe, whose centre must be taken for the focus of heat, that this
difference, which in this supposition is only a unit and nine millions,
can produce a diminution of heat nearly so considerable; for the
thermometer lowers at that height, at all times of the year, to the
freezing point. It is not probable, that this great difference of heat
simply proceeds from the difference of the earth; and of that we must
be fully convinced, if we consider, that at the mouth of the volcanos,
where the earth is hotter than in any other part on the surface of the
globe, the air is nearly as cold as on other mountains of the same
height.

It may then be supposed that the atoms of light, though very hot at the
moment of quitting the sun, are greatly cooled during the seven minutes
and a half in which they pass from that body to the earth; and this
in fact would be the case if they were detached; but, as they almost
immediately succeed each other, and are the more confined as they are
nearer the place of their origin, the heat lost by each atom falls on
the neighbouring ones; and this reciprocal communication supports the
general heat of light a longer time; and as their constant direction is
in divergent rays, their distance from each other increases according
to the space they run over; and as the heat which flies from each
atom, as a centre, diminishes also in the same ratio, it follows, that
the light of the solar rays, decreasing in an inverted ratio from the
square of the distance, that of their heat decreases in an inverted
ratio of the square of the same distance.

Taking therefore the semi-diameter of the sun for a unit, and supposing
the action of light to be as 1000 to the distance of a demi-diameter
of the surface of this planet, it will not be more than as 1000/4
to the distance of two demi-diameters; as 1000/9 to that of three
demi-diameters, as 1000/16 to the distance of four demi-diameters; and
finally, when it arrives at us, who are distant from the sun thirty-six
millions of leagues, that is about two hundred and twenty-four of its
demi-diameters, the action of light will be no more than as 1000/50625,
that is, more than 50,000 times weaker than at its issuing from the
sun; and the heat of each atom of light being also supposed 1000 at its
issuing from the sun, will not be more than as 1000/16 1000/81 1000/256
to the successive of 1, 2, 3, demi-diameters, and, when arrived at
us, as 1000/2562890625 that is, more than two thousand five hundred
millions of times weaker than at issuing from the sun.

If even this diminution of the heat of light should not be admitted
by reason of the squared square of the distance to the sun, it will
still be evident that heat, in its propagation, diminishes more than
light. If we excite a very strong heat, by kindling a large fire, we
shall only feel it at a moderate distance but we shall see the light
at a very great one. If we bring our hands by degrees nearer and nearer
a body excessively hot, we shall perceive that the heat increases
much more in proportion than as the space diminishes; for we may warm
ourselves with pleasure at a distance which differs only by a few
inches from that at which we should be burnt. Every thing, therefore,
appears to indicate, that heat diminishes in a greater ratio than
light, in proportion as both are removed from the focus whence they
issued.

This might lead us to imagine, that the atoms of light would be very
cold when they came to the surface of our atmosphere; but that by
traversing the great extent of this transparent mass, they receive a
new heat by friction. The infinite velocity with which the particles
of light rub against those of the air, must produce a heat so much the
stronger as the friction is more multiplied: and it is, probably, for
this reason, that the heat of the solar rays is found much stronger in
the lower parts of the atmosphere, and that the coldness of the air
appears to augment as we are elevated. Perhaps, likewise, as light
receives heat only by uniting, a great number of atoms of light is
required to constitute a single atom of heat, and this may be the
cause why the feeble light of the moon, although in the atmosphere,
like that of the sun, does not receive any sensible degree of heat.
If, as M. Bouguer says, the intensity of the light of the sun to
the surface of the earth is 300,000 times stronger than that of the
moon, the latter must be almost insensible, even by uniting it in the
focus of the most powerful burning glasses, which cannot condense it
more than 2000 times; subtracting the half of which for the loss by
reflexion or refraction, there remains only a 300dth part intensity to
the focus of the glass.

Thus, we must not infer that light can exist without any heat, but
only that the degrees of this heat are very different, according to
different circumstances, and always insensible when light is very weak.
Heat, on the contrary, seems to exist habitually, and even to cause
itself to be strongly felt without light; for in general it is only
when it becomes excessive, that light accompanies it. But the very
essential difference between these two modifications of matter is,
that heat, which penetrates all bodies, does not appear to fix in any
one, whereas light incorporates and extinguishes in all those which do
not reflect, or permit it to pass freely; heat bodies of all kinds
to any degree, in a very short time they will lose the acquired heat,
and return to the general temperature. If we receive light on black
or white bodies, rude or polished, it will easily be perceived, that
some admit, and others repel it; and that instead of being affected in
a uniform manner as they are by heat, they are only so relatively to
their nature, colour, and polish. Black will absorb more light than
white, and the rough more than the smooth. Light once absorbed remains
fixed in the body which received it, nor quits it like heat; whence
we must conclude, that atoms of light may become constituent parts of
bodies by uniting with the matter which composes them; whereas heat
not fixing at all, seems to prevent the union of every part of matter,
and only acts to keep them separate. Nevertheless, there are instances
where heat remains fixed in bodies, and others where the light they
have absorbed re-appears, and goes out like heat.

After all there appear to be two kinds of heat, the one luminous, of
which the sun is the focus; the other obscure, of which the grand
reservoir is the terrestrial globe. Our body, as making part of the
globe, participates of this obscure heat; and it is for this reason,
that it is still obscure to us, because we do not perceive it by any
one of our senses. It is with respect to this heat of the globe, as
with its motion, we are subject to and participate thereof without
feeling or doubting of it: from hence it happened that physicians at
first carried all their views and enquiries on the heat of the sun,
without suspecting that it makes but a very small part of what we
really feel; but having made instruments to discover the difference of
the immediate heat of the rays of the sun, they with astonishment found
that the heat of them was sixty-six times stronger in summer than in
winter, notwithstanding the strongest heat of our summer differs only
a seventh from the strongest cold of our winter; from whence they have
concluded, that, independent of the heat we receive from the sun, there
emanates another, even from this terrestrial globe, which is much more
considerable; insomuch, that it is at present demonstrable, that this
heat, which escapes from the bowels of the earth, is in our climate at
least twenty-nine times in summer, and four hundred times in winter,
stronger than the heat which comes to us from the sun.

This strong heat which resides in the interior part of the globe, and
which, without ceasing to emanate externally, must, like an element,
enter into the combination of all the other elements. If the sun is
the parent of Nature, the heat of the earth must be the mother; they
both unite to produce, support, and animate organized beings, and to
assimilate and compose inanimate substances. This internal heat of the
globe, which tends always from the centre to the circumference, is, in
my opinion, a great agent in nature. We can scarcely doubt but it is
the principal influence on the perpendicularity of the trunks of trees,
on the phenomena of electricity, on the effects of magnetism, &c. But
as I do not pretend to make a physical treatise here, I shall confine
myself to the effects of this heat on the other elements. It is alone
sufficient to maintain the rarefaction of the air to the degree that
we breathe in: it is more than sufficient to keep water in its state
of fluidity, for we have lowered the thermometers to the depth of 120
fathoms, and have found the temperature of the water was there nearly
the same as at the like depth in the earth, namely, ten degrees two
thirds. We must not, therefore, be surprized, especially as salt acts
as a prevention, that the sea in general does not freeze, that fresh
water freezes but to a certain thickness, and that the water at bottom
always remains liquid, even in the most intense frosts.

But of all the elements the earth is that on which this internal
heat must necessarily have produced, and still produces the greatest
effects. This heat originally was doubtless much greater than it is
at present; therefore we must refer to it, as to the first cause, all
the sublimations, precipitations, aggregations, and separations, which
have been, and still continue to be made in the internal part of the
globe, especially in the external layer which we have penetrated, and
the matter of which has been removed by the convulsions of Nature, or
by the hands of man. The whole mass of the globe having been melted, or
liquefied, by fire, the internal is only a concrete or discreet glass,
whose simple substance cannot receive any alteration by heat alone;
there is, therefore, only an upper and superficial layer, which being
exposed to the action of external causes united to that of the internal
heat, will have undergone all the modifications, differences, and
forms, in one word, of Mineral Substances, which their combined actions
were enabled to produce.

Fire, which at first sight appears to be only a compound of heat and
light, might also be a modification of the matter, though it does
not essentially differ from either, and still less from both taken
together. Fire never exists without heat, but it can exist without
light. Heat alone, deprived of all appearance of light, can produce the
same effects as the most violent fire; so can also light, when it is
united. Light seems to carry a substance in itself which has no need
of fuel; but fire cannot subsist without absorbing the air, and it
becomes more violent in proportion to the quantity it absorbs; whereas
light, concentrated and received into a vessel exhausted of air, acts
as fire in air; and heat, confined and retained in a narrow space,
subsists and even augments with a very small quantity of food. The most
general difference between fire, heat, and light, appears, therefore,
to consist in the quantity, and perhaps quality, of their food.

Air is the first food of fire; combustible matters are only the second.
It has been demonstrated, by experiments, that a little spark of
fire, placed in a vessel well closed, in a short time absorbs a great
quantity of air, and becomes extinguished as soon as the quantity or
quality, of this food becomes deficient. By other experiments it is
proved, that the most combustible matters will not consume in vessels
well closed, although exposed to the action of the greatest fire. Air
is, therefore, the first and true food of fire, and combustible matters
would not be able to supply it without the assistance and mediation of
this element.

We have observed that heat is the cause of all fluidity, and we find,
by comparing some fluids together, that more heat is requisite to keep
iron in fusion than gold; and more to keep gold than tin; much less
is necessary for wax, for water less than that, and still less for
spirits of wine, and a mere trifle is sufficient for mercury, since
the latter goes 187 degrees below what water can without losing its
fluidity; mercury, therefore, is the most fluid of all matter, air
excepted. Now this superior fluidity in air indicates the least degree
of adherence possible between its constituting parts, and supposes them
of such a figure as only to be touched at one point. It may be also
imagined, that, being endowed with so little apparent energy and mutual
attraction, they are, for that reason, less massive, and more light,
than those of every other body; but that conclusion appears unfounded,
from the comparison of mercury, the next fluid body, but of which the
constituting parts appear to be more massive and heavy than those of
any other matter, excepting gold. The greater or lesser fluidity, does
not, therefore, indicate that the parts of the fluid are more or less
weighty, but only that their adherence is so much the less, and their
separation so much the easier.

Air, therefore, of all known matter, is that which heat divides the
easiest, and is very near the nature of fire, whose property consists
in the expansive motions of its parts; and it is from this similarity
that air so strongly augments the activity of fire, to which it is the
most powerful assistant, and the most intimate and necessary food.
Even combustible matters will not keep it alive if deprived of air,
for under this privation the most intense fire will not burn; but a
single spark of air is sufficient to kindle them, and in proportion as
it is supplied with that element the fire becomes strong, extended, and
devouring.

Artificial phosphorus, and gunpowder, seem, at first, to be an
exception, for they have no need of the assistance of renewed air to
inflame and wholly consume them: their combustion may be performed in
the closest vessels, but that is because those matters, which are also
the most combustible, contain the necessary quantity of air in their
substance, therefore they have no need of the assistance of foreign
air.

This seems to indicate that the most essential difference between
combustible matters and those which are not so, consists in the latter
containing only a few or none of the light, ethereal, and oily matters
susceptible of an expansive motion, or, at least, if they contain them,
that they are fixed, so that they cannot exercise their volatility
whenever the force of the fire is not strong enough to surmount the
force of adhesion which retains them united to the fixed parts of
matter. It may be said that this induction is confirmed by a number of
observations well known to chemists; but what appears to be less so,
and which, nevertheless, is a necessary consequence of it, is, that
all matter may become volatile when the expansive force of the fire
can be rendered superior to the attractive force which holds the parts
of matter united; for though to produce a fire sufficiently strong it
may require better constructed mirrors than any at present known, yet
we are certain that fixity is only a relative quality, and that there
is no matter absolutely so, since heat dilates the most fixed bodies.
Now is not this dilation the index of a beginning separation, that may
be augmented with a degree of heat to fusion, and with a still greater
heat to volatilisation?

Combustion supposes something more than volatilisation; it is not
sufficient that the parts of matter be sufficiently separated to be
carried off by those of heat; they must also be of an analogous nature
to fire; without that, mercury, being the most fluid next to air, would
also be the most combustible, whereas experience demonstrates, that
though very volatile it is not combustible. Matter is, in general,
composed of four principal substances, called _elements_, that is,
earth, water, air, and fire. Those in which earth and water predominate
will be fixed, and will only become volatile by the action of heat;
and those which contain most air and fire will be the only real
combustibles. The great difficulty here is clearly to conceive how air
and fire, both so volatile, can fix and become constituent parts of all
bodies.

Fire, by absorbing air, destroys the spring. Now there are but two
methods of destroying a spring, either by compressing it till it
breaks, or extending it till it loses its effect. It is plain that
fire cannot destroy air by compression, since the least degree of heat
rarefies it; on the contrary, by a very strong heat the rarefaction of
the air will be so great that it will occupy a space thirteen times
more extended than that of its general volume; and by this means the
spring becomes weakened, and it is in this state that it can become
fixed, and unite with other bodies.

Light, which falls on bodies, is not merely reflected, but remains in
quantities on the small thickness of the surface which it strikes;
consequently it loses its motion, extends, is fixed, and becomes a
constituent part of all that it penetrates. Let us add this light,
transformed and fixed in bodies, to the above air, and to both, the
constant and actual heat of the terrestrial globe, whose sum is much
greater than that which comes from the sun, and then it will appear to
be not only one of the greatest springs of the mechanism of Nature, but
an element with which the whole matter of the globe is penetrated.

If we consider more particularly the nature of combustible matters,
we shall find, that they all proceed originally from vegetables and
animals; in a word, from bodies placed on the surface of the globe,
which the sun enlightens, heats, and vivifies. Wood, bitumen, resins,
coals, fat and oil, by expression, wax, and suet, are substances
proceeding immediately from animals and vegetables. Turf, fossil, coal,
amber, liquid, or concrete bitumens, are the productions of their
mixture, and their decomposition, whose ulterior waste forms sulphurs,
and the combustible parts of iron, tin, pyrites, and every inflammable
mineral. I know, that this last assertion will be rejected by those
who have studied nature only by the mode of chemistry; but I must
request them to consider, that their method is not that of nature, and
that it cannot even approach it without banishing all those precarious
principles, those fictitious beings which they play upon, without being
acquainted with them.

But, without pressing longer on those general considerations, let
us pursue in a more direct and particular manner the examination of
fire and its effects. The action of fire depends much on the manner
in which it is applied; and the effects of its motion, on similar
substances, will appear different according to the mode in which it
is administered. I conceive that fire should be considered in three
different states, first relative to its velocity; secondly, as to its
volume; and thirdly, as to its mass. Under each of these points of
view, this element, so simple, and so uniform to all appearance, will
appear extremely different. The velocity of fire is augmented without
the apparent volume being increased, every time that in a given space
and filled with combustible matters, its action and expansion is
pressed by augmenting the velocity of the air by bellows, caverns,
ventilators, aspirative tubes, &c. all of which accelerate more or less
the rapidity of the air directed on the fire. The action of fire is
augmented by its volume, when a great quantity of combustible matters
is accumulated, and the heat and fire are driven into the reverberatory
furnaces, which comprehend those of our glass, porcelain, and pottery
manufactories, and all those wherein metals and minerals are melted,
iron excepted. Fire acts here by its volume, and has only its own
velocity, since the rapidity is not augmented by the bellows, or other
instruments which carry air to the fire.

There are many modes of augmenting the action of fire by its velocity
or volume; but there is only one way of augmenting its mass; namely,
by uniting it in the focus of a burning glass. When we receive on the
refracting, or reflecting mirror, the rays of the sun, or even those of
a well-kindled fire, we unite them in so much the less space, as the
mirror is longer, and the focus shorter; for example, by a mirror of
four feet diameter, and one inch focus, it is clear, that the quantity
of light, or fire, which falls on the four-feet mirror, will be united
in the space of one inch, that is, it will be 2304 times denser than
it was, if all the incident matter arrived to this focus without any
loss, and when even the loss is two thirds or three fourths, the mass
of fire concentrated in the focus of this mirror, will always be six
or seven hundred times denser than on the surface. In this, as in all
other cases, the mass goes by the contraction of the volume; and the
fire which we thus augment the density of, has all the properties of a
mass of matter; for, independently of the action of heat, by which it
penetrates bodies, it impels and displaces them as a solid moving body
which strikes another would do.

Each of these modes of administering fire, and increasing either the
velocity, volume, or mass, often produce very different effects on the
same substances; insomuch, that no reliance is to be placed on any
thing that cannot be worked at the same time, or successively, by all
three. In the like manner, as I divide into three general proceedings
the administration of this element, I divide every matter that can
be submitted to its action into three classes. Passing over for the
present those which are purely combustible, and which immediately
proceed from animals and vegetables; we proceed to minerals, in the
first class of which we reckon those mineral matters, which this
action, continued for a long time, renders lighter, as iron; in the
second, such as it renders heavier, as lead; and in the third class,
are those matters on which, as gold, this action of fire does not
appear to produce any sensible effect, since it does not at all alter
their weight. All existing matters, that is, all substances simple and
compounded, will necessarily be comprized under one of these three
classes; and experiments on them by the three proceedings, which are
not difficult to be made, and only require exactness and time, might
develope many useful discoveries, and prove very necessary to build
on real principles the theory of chemistry, which has hitherto been
carried on by a precarious nomenclatura, and on words the more vague as
they are the more general.

Fire is the lightest of all bodies, notwithstanding which it has
weight, and it may be demonstrated, that even in a small volume it is
really heavy, as it obeys, like all other matters, the general law of
gravity, and consequently must have connections or affinities with
other bodies. All matters it renders more weighty will be those with
which it has the greatest affinity. One of the effects of this affinity
in the matters is to retain the substance even of fire, with which it
is incorporated, and this incorporation supposes that fire not only
loses its heat and elasticity, but even all its motion, since it fixes
itself in these bodies, and becomes a constituent part. From which it
may be imagined that there is fire under a fixed and concrete form in
almost every body.

It is evident, that all matters, whose weight increases by the
action of fire, are endowed with an attractive force superior to the
expansive, the fiery particles of which are animated; this being
extinguished the motion ceases, and the elastic and fugitive particles
become fixed, and take a concrete form. Thus matters, whose weight is
increased by fire, as tin, lead, &c. are substances which, by their
affinity with fire, attract and incorporate. All matters, on the
contrary, which, like iron, copper, &c. become lighter in proportion as
they are calcined, are substances whose attractive forces, relative to
the igneous particles, is less than the expansive force of fire; and
hence the fire, instead of fixing in these matters, carries off and
drives away the least adherent parts which cannot resist its impulsion.
Those which, like gold, platina, silver, &c. neither lose nor acquire
by the application of fire, are substances which, having no affinity
with fire, and not being able to unite, cannot, consequently, either
retain or accompany it when it is carried off. It is evident that the
matters of the two first classes have a certain degree of affinity with
fire, since those of the second class are loaded with fire, which they
retain; and the fire loads itself with those of the first class, which
it carries off; whereas the matters of the third class, to which it
neither lends nor borrows, have not any affinity or attraction with it,
but are indifferent to its action, which can neither unnaturalize nor
even change them.

This division of every matter into three classes, relative to the
action of fire, does not exclude the more particular and less absolute
division of all matters into two other classes, hitherto regarded as
relative to their own nature, which is said to be always vitrifiable,
or calcareous. Our new division is only a more elevated point of view,
under which we must consider them, to endeavour to deduce therefrom
even the agent that is used by the relations fire can have with every
substance to which it is applied.

We might say, with naturalists, that all is vitrifiable in Nature,
excepting that which is calcareous: that quartz, chrystals, precious
stones, flints, granites, porphyries, agates, gypsums, clays, lava,
pumice stone, with all metals and other minerals, are vitrifiable
either by the fire of our furnaces, or that of mirrors; whereas marble,
alabaster, stones, chalk, marl, and other substances which proceed from
the residue of shells and madrepores, cannot be reduced into fusion
by these means. Nevertheless I am persuaded, that if the power of our
furnaces and mirrors were further increased, we should be enabled to
put these calcareous matters in fusion; since there are a multiplicity
of reasons to conclude, that at the bottom their substance is the same,
and that glass is the common basis of all terrestrial matter.

By my own experiments I have found, that the most powerful glass
furnaces is only a weak fire, compared with that of bellows furnaces;
and that fire produced in the focus of a good mirror, is stronger than
that of the most glowing fire of a furnace. I have kept iron ore for
thirty-six hours in the hottest part of the glass furnace of Rouelle,
in Burgundy, without its being melted, agglutinated, or even in any
manner changed; whereas, in less than twelve hours this ore runs in a
forge furnace. I have also melted, or volatilized, by a mirror many
matters which neither the fire, nor reverberatory furnace, nor the
most powerful bellows furnace could cause to run.

It is commonly supposed, that flame is the hottest part of fire, yet
nothing is more erroneous than this opinion; the contrary may be
demonstrated by the most simple and familiar experiments. Offer to a
straw fire, or even to the flame of a lighted faggot, a cloth to dry or
heat, and treble the time will be required to what would be necessary
if presented to a brasier without flame. Newton very accurately defines
flame to be a burning smoke, and this smoke, or vapour, has never the
same quantity or intensity of heat as the combustible body from which
it escapes. By being carried upwards and extending, it has the property
of communicating fire, and carrying it further than the heat of the
brasier, which alone might not be sufficient to communicate it when
even very near.

The communication of fire merits a particular attention. I found, after
repeated reflections that besides the assistance of facts which appear
to have a relation to it, that experiments were necessary to understand
the manner in which this operation of Nature is made. Let us receive
two or three thousand weight of iron in a mould at its issuing from
the furnace; this metal in a short time loses its incandescence, and
ceases from its redness, according to the thickness of the ingot. If at
the moment its redness leaves it, it is drawn from the mold, the under
parts will be still red, but this colour will fly off. Now so long as
the redness subsists, we can light combustible matters by applying them
to the ingot; but as soon as it has lost its incandescent state, there
are numbers of matters which it will not set fire to, although the heat
which it diffuses is, perhaps a hundred times stronger than that of a
straw fire, which would inflame them. This made me think that flame
being necessary to the communication of fire, there is therefore a
flame in all incandescence. The red colour seems, in fact, to indicate
it; and indeed I am convinced, that combustible, and even the most
fixed matters, such as gold and silver, when in an incandescent state,
are surrounded with a dense flame which extends only to a very short
distance, and which is attached to their surface; and I can easily
conceive, that when flame becomes dense to a certain degree, it ceases
from obeying the fluctuation of the air. This white or red body, which
issues from all bodies in incandescence, and which strikes our eyes,
is the evaporation of this dense flame which surrounds the body by
renewing itself incessantly on its surface; and even the light of the
sun, which emits such an amazing brightness, I presume to be only an
evaporation of the dense state that constantly plays on its surface;
and which we must regard as a true flame, more pure and dense than any
proceeding from our combustible matters.

It is, therefore, by light that fire communicates, and heat alone
cannot produce the same effect as when it becomes very strong to be
luminous. Even water, that destructive element to fire, by which alone
we can prevent its progress, nevertheless communicates when in a
well-closed vessel, such as Papin's digester, where it is penetrated
with a sufficient quantity of fire to render it luminous, and capable
of melting lead and tin, whereas when it is only boiling, far from
communicating fire, it extinguishes it immediately. It is true, that
heat alone is sufficient to prepare and dispose combustible bodies for
inflammation, by driving off the humid parts from bodies; and what is
very remarkable, this heat, which dilates all bodies, does not desist
from hardening them by drying. I have an hundred times discovered, by
examining the stones of my great furnaces, especially the calcareous,
they increased in hardness in proportion to the time they had undergone
the heat, and they also at the same time became specifically heavier.
From this circumstance, I think an induction may be drawn, which
would prove, and fully confirm, that heat, although in appearance
always fugitive and never stable in the bodies which it penetrates,
nevertheless deposits in a positive manner many parts which fixes there
even in greater quantities than the aqueous and other parts which it
has driven off. But what appears very difficult to be reconciled,
this same calcareous stone, which becomes specifically heavier by the
action of a moderate heat a long time continued, becomes near a half
lighter, when submitted to a fire sufficient for its calcination, and,
at the same time, not only loses all the hardness it had acquired by
the action of heat, but even the natural adherence of its constituting
parts.

Calcination generally received, is, with respect to fixed and
incombustible bodies, what combustion is to volatile and inflammable.
Calcination, like combustion, needs the assistance of air; it operates
so much the quicker, as it is furnished with a greater quantity of that
element, without which the fiercest fire cannot calcine nor inflame
any thing, except such matters as contain in themselves all the air
necessary for those purposes. This necessity for the concurrence of
air in calcination, as in combustion, indicates, that there are more
things common between them than has been suspected. The application of
fire is the principle of both; that of air is the second cause, and
almost as necessary as the first; but these two causes are equally
combined, according as they act in more or less time, and with more or
less power on different substances.

Combustion operates almost instantaneously; calcination is sometimes
so long, as to be thought impossible; for in proportion as matters
are more incombustible, the calcination is there more slowly made;
and when the constituent parts of a substance, such as gold, are not
only incombustible, but appear so fixed as not to be volatilized,
calcination produces no effect. They must both, therefore, be
considered as effects of the same cause, whose two extremes are
delineated to us by phosphorus, which is the most inflammable of all
bodies, and by gold, which is the most fixed and least combustible.
All substances comprized between these two extremes, will be more or
less subjected to the effects of combustion and calcination, according
as they approach either of them; insomuch, that in the middle points
there will be found substances that endure an almost equal degree
of both; from which we may conclude, that all calcination is always
accopmanied with a little combustion, and all combustion with a little
calcination. Cinders and other residue of the most combustible matters,
demonstrate that fire has calcined all the parts it has not burned,
and consequently, a little calcination is found here with combustion.
The small flame which rises from most matters, that are calcined,
demonstrates also that a slight combustion is made. Thus, we must not
separate these two effects, if we would find out the results of the
action of fire on the different substances to which it is applied.

But it may be said, that combustion always diminishes the volume or
mass, on account of the quantity of matter it consumes; and that, on
the contrary, calcination increases the weight of many substances.
Ought we then to consider these two effects whose results are so
contrary, as effects of the same nature? Such an objection appears
well-founded, and deserves an answer, especially as this is the most
difficult point of the question. For that purpose let us consider a
matter in which we shall suppose one half to be fixed parts, and the
other volatile or combustible. By the application of fire to this,
all the volatile or combustible parts will be raised up or burnt, and
consequently separated from the whole mass; from hence this mass or
quantity of matter will be found diminished one half, as we see it
in calcareous stones, which lose near half their weight in the fire.
But if we continue to apply the fire for a very long time to the other
half, composed of fixed parts, all combustion and volatilization
being ceased, that matter, instead of continuing to lose its mass,
must increase at the expense of the air and fire with which it is
penetrated; and those are matters already calcined, and prepared
by Nature to the degree where combustion ceases, and consequently
susceptible of increasing the weight from the first moment of the
application. We have seen, that light extinguishes on the surface of
all bodies which do not reflect; and that heat, by long residence,
fixes partly in the matters which it penetrates; we know also that
air is necessary for calcination, or combustion, and the more so for
calcination as having more fixity in the external parts of bodies, and
becomes a constituent part: hence, it is natural to imagine, that this
augmentation of weight proceeds only from the addition of the particles
of light, heat, and air, which are at length fixed and united to one
matter, against which they have made so many efforts, without being
able either to raise or burn them. This appears clearly to be the
fact, for if we afterwards present a combustible substance to them they
will quit the fixed matter, to which they were only attached through
force, retake their natural motion, elasticity, and volatility, and
all depart with it; from hence, metal, or calcinized matter, to which
these volatile parts has been rendered, retakes its pristine form,
and its weight is found diminished by the whole quantity of fiery
and airy particles which were fixed in it, and which had been just
raised by this new combustion. All this is performed by the sole law
of affinities; and there seems to be no more difficulty to conceive
how the lime of a metal is reduced, than to understand how it is
precipitated in dissolution; the cause is the same, and the effects are
similar. A metal dissolved by an acid, will precipitate when to this
acid another substance is offered with which it has more affinity than
metal, the acid then quits it and falls to the bottom. So, likewise,
this metal calcines, that is, loaded with parts of air, heat, and
fire, which being fixed, keeps it under the form of a lime, and will
precipitate, or be reduced, when presented to this fire and fixed air,
from the combustible matters with which they have more affinity than
with the metal; the latter will retake its first form as soon as it is
disembarrassed from this superfluous air and fire, at the expence of
the combustible matters offered to it, and the volatile parts it had
lost.

I think I have now demonstrated, that all the little laws of chemical
affinities, which appeared so variable and different, are no other
than the general laws of attraction, common to all matter; that this
great law, always constant and the same, appeared only to vary in
its expression, which cannot be the same when the figure of bodies
enters, like an element, into their distance. With this new key we
can unlock the most profound secrets of Nature; we can attain the
knowledge of the figure of the primitive parts of different substances;
assign the laws and degrees of their affinities; determine the forms
which they take by re-uniting, &c. I think also I have made it appear
that impulsion depends on attraction; and that, although it may be
considered as a different force, it is, notwithstanding, a particular
effect of this sole and general one. I have shewn the communication
of motion to be impossible without a spring, whence I have concluded,
that all bodies in Nature are more or less elastic, and that there
is not one perfectly hard; that is, entirely deprived of a spring,
since all are susceptible of receiving motion. I have endeavoured to
shew how this sole force may change direction, and attraction become
repulsion; and from these grand principles, which are all founded on
rational mechanics, I have sought to deduce the principal operations
of Nature, such as the production of light, heat, and fire, and their
action on different substances; this last object which interests us
the most is a vast field, but of which I can only cultivate a little
spot, yet I presume I may render some assistance, by putting into
more capable and laborious hands the instruments I made use of. These
instruments were the three modes of making use of fire, that is, by its
velocity, volume, and mass; by applying it concurrently to the three
classes of substances, which either lose, gain, or are not affected
by the application of fire. The experiments which I had made on the
refrigeration of bodies, on the real weight of fire, on the nature of
flame, on the progress of heat, or its communication, its diperdition,
its concentration, or its violent action without flame, &c. are also
so many instruments which will spare much labour to those who choose
to avail themselves of them, and will produce an ample harvest of
knowledge.




OF AIR, WATER, AND EARTH.


By our former observations it appears that air is the necessary and
first food of fire, which can neither subsist nor propagate but by what
it assimilates, consumes, or carries off, of that element, whereas
of all material substances, air is that which seems to exist the
most independently of the aid or presence of fire; for although it
habitually has nearly the same heat as other matters on the surface
of the earth, it can do without it and requires infinitely less than
any of the rest to support its fluidity, since the most excessive cold
cannot deprive it of that. The strongest condensations are not capable
of breaking its spring; the active fire, in combustible matters, is the
only agent which can alter its nature by rarefying and extending its
spring to the point of rendering it ineffectual, and thus destroying
its elasticity. In this state, and in all the links which precede, the
air is capable of re-assuming its elasticity, in proportion as the
vapours of combustible matters evaporate and separate from it. But if
the spring have been totally weakened and extended that it cannot
re-instate itself, from having lost all its elastic power, the air,
volatile as it might before have been, becomes a fixed substance which
incorporates with the other substances, and forms a constituent part of
all those to which it unites by contact. Under this new form it can no
longer forsake the fire, except to unite, like fixed matter, to other
fixed matters; and if there remain some parts inseparable from fire,
they then make a portion of that element serve it for a base, and are
deposited with it in the substance they heat and penetrate together.
This effect is manifested in all calcinations, and is the more sensible
as the heat is longer; but combustion demands only a small time to
completely effectuate the same. If we wish to hasten calcination the
use of bellows may be necessary, not so much to augment the heat of the
fire as to establish a current of air on the surface of the matters;
yet it is not requisite for the fire to be very fierce to deprive air
of its elasticity, for a very moderate heat, when constantly applied
on a small quantity, is sufficient to destroy the spring; and for this
air, without spring, to fix itself afterwards in bodies, there is only
a little more or less time required, according to the affinity it may
have under this new form, with the matters to which it unites. The
heat of the body of animals, and even vegetables, is sufficiently
powerful to produce this effect. The degrees of heat are different in
different kinds of animals: birds are the hottest, from which we pass
successively to quadrupeds, man, cetaceous animals, reptiles, fish,
insects, and, lastly, to vegetables, whose heat is so trifling as to
have made some naturalists declare they had not any, although it is
very apparent, and in winter surpasses that of the atmosphere. I have
frequently observed in trees that were cut in cold weather, that their
internal part was sensibly warm, and that this heat remained for many
minutes. This heat is only moderate while the tree is young and sound,
but as soon as it grows old the heart heats by the fermentation of the
pith, which no longer circulates there with the same freedom; and as
soon as this heat begins the centre receives a red tint, which is the
first index of the perishing state of the tree, and the disorganization
of the wood. The reason naturalists have not found there was a
difference between the temperature of the air, and the heat of
vegetables is, because they have made their observations at a bad time
of the year, and not paid attention, that in the summer the heat of the
air exceeds that of the internal part of a tree; whereas in winter it
is quite the contrary. They have not remembered that the roots have
constantly the degree of heat which surrounds them, and that this heat
of the internal part of the earth is, during all winter, considerably
greater than that of the air, and the surface of the earth. They did
not consider that the motion alone of the pith, already warm, is a
necessary cause of heat, and that this motion, increasing by the action
of the sun, or by an external heat, that of vegetables must be so much
the greater as the motion of their pith is more accelerated, &c.

Here the air contributes to the animal and vital heat, as we have
seen that it does to the action of fire in combustible and calcinable
matters. Animals, which have lungs, and which consequently respire
the air, have more heat than those deprived of them; and the more
the internal surface of the lungs is extended, and ramified in a
greater number of cells, the more it presents greater superficies
to the air which the animal draws by inspiration; the more also its
blood becomes hotter, the more it communicates heat to all parts of
the body it nourishes, and this proportion takes place in all known
animals. Birds, relatively to the volume of their body, have lungs
considerably more extended than man or quadrupeds. Reptiles, even
those with a voice, as frogs, instead of lungs have a simple bladder.
Insects which have little or no blood breathe the air only by some
pipes, &c. Thus taking the degree of the temperature of the earth for
the term of comparison, I have observed that this heat being supposed
ten degrees, that of birds was nearly thirty-three, that of some
quadrupeds more than thirty-one and a half, that of man thirty and a
half, or thirty-one, whereas that of frogs is only fifteen or sixteen,
and that of fishes and insects only eleven or twelve, which is nearly
the same as that of vegetables. Thus the degree of heat in man and
animals depends on the force and extent of the lungs; these are the
bellows of the animal machine: the only difficulty is to conceive how
they carry the air on the fire which animates us, a fire whose focus
seems to be indeterminate; a fire that has not even been qualified
with this name, because it is without flame or any apparent smoke, and
its heat is only moderate and uniform. However, if we consider that
heat and fire are effects, and even elements of the same class; that
heat rarefies air, and, by extending its spring, it may render it
without effect; we may imagine, that the air drawn by our lungs being
greatly rarefied, loses its spring in the bronchiæ and little vesicles,
where it is soon destroyed by the arterial and venous blood, for these
blood-vessels are separated from the pulmonary vesicles by such thin
divisions that the air easily passes into the blood, where it produces
the same effect as upon common fire, because the heat of this blood
is more than sufficient to destroy the elasticity of the particles
of air, and to drag them under this new form into all the roads of
circulation. The fire of the animal body differs from common fire only
in more or less; the degree of heat is less, hence there is no flame,
because the vapours, which represent the smoke, have not heat enough
to inflame; every other effect is the same: the respiration of a young
animal absorbs as much air as the light of a candle, for if inclosed in
vessels of equal capacities, the animal dies in the same time as the
candle extinguishes: nothing can more evidently demonstrate that the
fire of the animal and that of the candle are not of the same class but
of the same nature, and to which the assistance of the air is equally
necessary.

Vegetables, and most insects, instead of lungs, have only aspiratory
tubes, by which they pump up the air that is necessary for them; it
passes in very sensible balls into the pith of the vine. This air
is not only pumped up by the roots but often even by the leaves,
and forms a very essential part of the food of the vegetable which
assimilates, fixes, and preserves it. Experience fully confirms all
we have advanced on this subject, and that all combustible matters
contain a considerable quantity of fixed air, as do also all animals
and vegetables, and all their parts, and the waste which proceeds
therefrom; and that the greatest number likewise include a certain
quantity of elastic air. And, notwithstanding the chimerical ideas
of some chemists, respecting phlogiston, there does not remain the
smallest doubt but that fire or light produces, with the assistance of
air, all the effects thereof.

Minerals, which like sulphur and pyrites, contain in their substance
a quantity of the ulterior waste of animals and vegetables, contain
thence combustible matters, which, like all other, contain more or less
fixed air, but always much less than the purely animal or vegetable
substances. This fixed air can be equally removed by combustion. In
animal and vegetable matters it is disengaged by simple fermentation,
which, like combustion, has always need of air for its operation.
Sulphurs and pyrites are not the only minerals Which must be looked
upon as combustible, there are many others which I shall not here
enumerate, because it is sufficient to remark, their degree of
combustion depends commonly on the quantity of sulphur which they
contain. All combustible minerals originally derive this property
either from the mixture of animal or vegetable parts which are
incorporated with them, or from the particles of light, heat, and air,
which, by the lapse of time, are fixed in their internal part. Nothing,
according to my opinion, is combustible but that which has been formed
by a gentle heat, that is, by these same elements combined in all the
substances which the sun brightens and vivifies, or in that which the
internal heat of the earth foments and unites.

The internal heat of the globe of the earth must be regarded as the
true elementary fire; it is always subsisting and constant; it enters,
like an element, into all the combinations of the other elements, and
is more than sufficient to produce the same effects on air as actual
fire on animal heat; consequently this internal heat of the earth
will destroy the elasticity of the air, and render it fixed, which
being divided into minute parts will enter into a great number of
substances, from hence they will contain articles of fixed air and
fire, which are the first principles of combustibility; but they will
be found in different quantities, according to their degree of affinity
with the substance, and this degree will greatly depend on the quantity
these substances contain of animal and vegetable parts, which appear to
be the base of all combustible matter. Most metallic minerals, and even
metals, contain great quantities of combustible parts; zinc, antimony,
iron, copper, &c. burn and produce a very brisk flame, as long as the
combustion of these inflammable parts remains, after which, if the fire
be continued, the calcination begins, during which there enters into
them new parts of air and heat, which fixes, and cannot be disengaged
but by presenting to them combustible matters, with which they have a
greater affinity than with those of the mineral, with which they are
only united by the effort of calcination. It appears to me, that the
conversion of metallic substances into dross, and their reproduction,
might be very clearly understood without applying to secondary
principles, or arbitrary hypotheses, for their explanation.

Having considered the action of fixed air in the most secret operations
of nature, let us take a view of it when it resides in bodies under
an elastic form; its effects are then as variable as the degrees of
its elasticity, and its action, though always the same, seems to give
different products in different substances. To bring this consideration
back to a general point of view, we will compare it with water and
earth, as we have already compared it with fire; the results of this
comparison between the four elements will afterwards be easily applied
to every substance, since they are all composed merely of these four
real principles.

The greatest cold that is known, cannot destroy the spring of the air,
and the least heat is sufficient for that purpose, especially when this
fluid is divided into very small particles. But it must be observed,
that between its state of fixity, and that of perfect elasticity, there
are all the links of the intermediate states, in one of which it always
resides in earth and water, and all the substances which are composed
of them; for example, water, which appears so simple a substance,
contains a certain quantity of air, which is neither fixed nor elastic,
as is plain from its congulation, ebullition, and resistance to all
compression, &c. Experimental philosophy demonstrates, that water is
incompressible, for instead of shrinking and entering into itself when
pressed, it passes through the most solid and thickest vessels; which
could not be the case if the air it contained were in a state of full
elasticity. The air contained therefore in water, is not simply mixed
therewith, but is united in a state where its spring is not sensibly
exercised; yet the spring is not entirely destroyed, for if we expose
water to congelation, the air issues from its internal part, and unites
on its surface in elastic bubbles. This alone suffices to prove, that
air is not contained in water under its common form, since being
specifically 850 times lighter, it would be forced to issue out by the
sole necessity of the preponderance of water; neither under an affixed
form, but only in a medium state, from whence it can easily retake its
spring, and separate more easily than from every other matter.

It may, with some justice, be objected that cold and heat never operate
in the same mode, and that if one of these causes gives to air its
elasticity, the other must destroy it, and I own that in general it
is so, but in this particular they produce the same effect. It is
well known that water, frozen or boiled, reabsorbs the air it had
lost as soon as it is liquefied or cooled. The degree of affinity
of air with water, depends, therefore, in a great measure, on its
temperature, which in its liquid state; is nearly the same as that of
the general heat, to the surface of the earth: the air with which it
has much affinity penetrates it as soon as it is divided into small
parts, yet the degree of elementary and general heat, weakens their
spring so as to render them ineffectual as long as the water preserves
this temperature; but if the cold penetrate, or this degree of heat
diminish, then its spring will be re-established by the cold, and the
elastic bubbles will rise to the surface of the water ready to freeze;
if, on the contrary, the temperature of the water is increased by an
external heat, the integrant parts become too much divided, they are
rendered volatile, and the air with which they are united, rises and
escapes with them. Water and air have much greater connections between
them than opposite properties, and as I am well persuaded, that all
matter is convertible, and that the elements may be transformed, I am
inclined to believe, that water can change into air when sufficiently
rarefied to raise up in vapours, for the spring of the vapour of the
water is even more powerful than the spring of the air.

Experience has taught me that the vapours of water can increase the
fire in the same manner as common air; and this air, which we may
regard as pure, is always mixed with a very great quantity of water;
but it must be remarked, as an observation of much importance, that
the proportions of the mixtures are not nearly the same in these two
elements. It may be said in general that there is much less air in
water than water in air. In considering this proportion we must refer
to the volume and mass. If we estimate the quantity of air contained in
water by the volume it will appear nil, since the volume is not in the
least increased. Thus it is not to the volume that we must relate this
proportion, it is alone to the mass, that is, to the real quantity of
matter in one and the other of these two elements that we must compare
that of their mixture, by which we shall perceive that the air is much
more _aqueous_ than the water is _aerial_, perhaps in proportion of the
mass, that is, eight hundred and fifty times. Be this estimation either
too strong or too weak we can derive this induction from it, that water
must change more easily into air than air can transform into water.
The parts of air, although susceptible of being extremely divided,
appear to be more gross than those of water, since the latter passes
through many filtres which air cannot penetrate; since the vapours of
water are only raised to a certain height in the air; and, in short,
since air seems to imbibe water like a sponge, to contain it in a
large quantity, and that the container is certainly greater than the
contained.

In the order of the conversion of the elements it appears to me, that
water is to air what air is to fire, and that all the transformations
of nature depend on them. Air, like the food of fire, assimilates with
it, and is transformed into this first element. Water, rarefied by
heat, is transformed into a kind of air capable of feeding the fire
like common air. Thus fire has a double fund of certain subsistence;
if it consume much air it can also produce much by the rarefaction of
water, and thus repair, in the mass of atmosphere, all the quantity
it destroyed, while ulteriorly it converts itself with air into fixed
matter in the terrestrial substances which it penetrates by its heat
or by its light. And so, likewise, as water is converted into air,
or into vapours, as volatile as air, by its rarefaction, it is also
converted into a solid substance by a kind of condensation. Every fluid
is rarefied by heat and condensed by cold. Water follows this common
law, and condenses as it grows cold. Let a glass tube be filled three
parts full and it will descend in proportion as the cold increases, but
some time before congelation it will ascend above the point of three
fourths of the height of the tube, and increase still more considerably
by being frozen. But if the tube be well stopped, and perfectly at
rest, the water will continue to descend, and will not freeze, although
the degree of cold be six, eight, or ten degrees below the freezing
point; congelation, therefore, presents, in an inverted manner, the
same phenomena as inflammation. A heat, however great, shut up in a
well-closed vessel, will not produce inflammation unless touched with
an inflamed matter; so, likewise, to whatsoever degree a fluid is
cooled, it will not freeze unless it touch something already frozen,
and this is what happens when the tube is shaken or uncorked; the
particles of water, which are frozen in the external air, or in the air
contained in the tube, strike the surface of the water, and communicate
their ice to it. In inflammation, the air, at first very much rarefied
by heat, loses its volume, and fixes itself suddenly. In congelation,
water, at first condensed by the cold, takes a larger volume, and fixes
itself likewise, for ice is a solid substance, lighter than water, and
would preserve its solidity if the cold continued the same; and I am
inclined to believe that we may attain the point of fixing mercury at
a less degree of cold, by sublimating it into vapours in a very cold
air; and also that water, which only owes its liquidity to heat, would
become a substance much more solid and fusible, as it would endure a
stronger and a longer time the rigour of the cold.

But without stopping upon this subject, that is, without admitting or
excluding the possibility of the conversion of the ice into infusible
matter, or fixed and solid earth, let us pass on to more extensive
views on the modes which Nature makes use of for the transformation
of water. The most powerful of all and the most evident is the animal
filter. The body of shell-animals, by feeding on the particles of
water, labours, at the same time, on the substance to the point of
unnaturalizing it. The shell is certainly a terrestrial substance,
a true stone, from which all the stones called calcareous, and many
other matters, derive their origin. This shell appears to make the
constitutive part of the animal it covers, since it is perpetuated
by generation, for it is on the small shell-animal just come into
existence as well as on those which have arrived at their full growth;
but this is no less a terrestrial substance, formed by the secretion
or exudation of the body, for it increases and thickens by rings
and layers in proportion as the animal grows; and stony matter often
exceeds fifty or sixty times the mass of the body which produces
it. Let us, for a moment, reflect on the number of the kind of
shell-animals, or rather of those animals with a stony transudation;
they, possibly, are more numerous in the sea than the insect kind
are upon earth. Let us afterwards represent their full growth, their
prodigious multiplication, and the shortness of their lives, which
we may suppose does not exceed ten years; let us then consider that
we must multiply by fifty or sixty the almost immense number of the
individuals of this class to form an idea of all the stony matter
produced in ten years; then that this block must be augmented with as
many similar blocks as there are as many times ten in all the ages from
the beginning of the world, and by this means we shall conceive, that
all our coral, rocks of calcareous stone, marble, chalk, &c. originally
proceeded alone from the cast-off coats of those little animals.

Salts, bitumen, oil, and the grease of the sea, enter little or none
into the composition of the shell; neither does the calcareous stone
contain any of those matters; this stone is, therefore, only water
transformed, joined to some little portion of vitrifiable earth, and to
a great quantity of fixed air, which may be disengaged by calcination.
This operation produces the same effect on the shells taken in the sea
as upon those drawn out of quarries; they both form lime, with only a
little difference in their quality. Lime, made with oyster or other
shells, is weaker than that made with marble or hard stone; but the
process of Nature is the same, as are the results of its operation.
Both shells and stones, lose nearly half their weight by the action
of fire in calcination; the water issues first, after which the fixed
air is disengaged, and then the fixed water, of which these stony
substances are composed, resumes its primitive nature, is elevated into
vapours, drove off and rarefied by the fire, so that there remains
only the most fixed parts of this air and water, which, perhaps, are
so strongly united in themselves, and to the small quantity of the
fixed earth of the stone, that the fire cannot separate them; the
mass, therefore, is reduced nearly a half, and would probably be still
more if submitted to a stronger fire. And what appears to me to prove
that this matter, driven out of the stone by the fire, is nothing else
than air and water, is the avidity with which calcined stone sucks up
the water given to it, and the force with which it draws water from
the atmosphere. Lime, by exposure either in air or water, in a great
measure regains the mass it had lost by calcination; the water, with
the air it contains, replaces that which the stone contained before.
Stone then retakes its first nature, for in mixing lime with the
remains of other stones, a mortar is made which hardens, and becomes a
solid substance, like those from which it is composed.

Thus, then, we see on the one hand all the calcareous matters, the
origin of which we must refer to animals; and on the other, all the
combustible matters proceeding from animal or vegetable substances;
they occupy together a great space on the earth; yet, however great
their number may be, they only form a small part of the terrestrial
globe, the principal foundation of which, and the greatest quantity
consists in one matter of the nature of glass; a matter we must look
upon as terrestrial element, to the exclusion of all other substances,
to which it serves as a base, like earth, when it forms vegetables by
the means, or remains of animals, and by the transformation of the
other elements; and it is also the ulterior term to which we can return
or reduce them all.

It appears that the animal filter converts water into stone; the
vegetable filter can also transform it, when all the circumstances are
found to be the same. The heat of vegetables and the organs of life
being less powerful than those of shell animals, the vegetables can
produce only a small quantity of stones, which are frequently found
in its fruits; but it can and does convert a great quantify of air,
and a still greater of water into its substance. It may be asserted,
without fear of contradiction, that the fixed earth it appropriates,
and which serves as a base to these two elements, does not make the
hundredth part of its mass; hence, the vegetable is almost entirely
composed of air and water, transformed into wood, or a solid substance,
which is afterwards reduced into earth by combustion and putrefaction.
The same may be said of animals; they not only fix and transform air
and water, but fire, and in a much greater quantity than vegetables.
It appears, therefore, to me, that the functions of organized bodies
are the most powerful means made use of by Nature for the conversion
of the elements. We may regard each animal, or vegetable, as a small
particular centre of heat or fire that appropriates to itself the air
and water which surround it, assimilates them to vegetate or nourish,
and live on the productions of the earth, which are themselves only
air and water previously fixed. It also appropriates to itself a small
quantity of earth, and receiving the impressions of light, the heat of
the sun and terrestrial globe, it converts into its substance all these
different elements; works, combines, unites, and opposes them, till
they have undergone the necessary form towards its support of life, and
the growth of organization, the mold of which once given, models every
matter it admits, and from inanimate renders it organized.

Water, which so readily coalesces and enters with air into organized
bodies, unites also with some solid matters, such as salts; and it is
often by their means that it enters into the composition of minerals.
Salt at first appears to be only an earth soluble in water, and of
a sharp flavour, but chemists have perfectly discovered, that it
principally consists in the union of what they term the _earthly_ and
the _aqueous principle_. The experiment of the nitrous acid, which
after combustion leaves only a small quantity of earth and water,
has caused them to think, that salt was composed only of these two
elements; yet I think it is easily to be demonstrated, that air and
fire also enter their composition; since nitre produces a great
quantity of air in combustion, and this fixed air supposes fixed fire
which disengages at the same time: besides all the explanations given
of the dissolution cannot be supported, and it would be against all
analogy, that salt should be composed only of these two elements, while
all other substances are composed of four. Hence we must not receive
literally what those great chemists Messrs. Stahl and Macquer have
said on this subject; the experiments of Mr. Hales demonstrate, that
vitriol and marine salt contain much fixed air; that nitre contains
still more, even to the eighth of its weight; and that salt of tartar
contains still more than these. It may, therefore, be asserted that air
enters as a principle into the composition of all salts; but this does
not support the idea that salt is the mediate substance between earth
and water; these two elements enter in different proportions into the
different salts or saline substances, whose variety and number are so
great, as not to be enumerated; but which, generally presented under
the denomination of acids and alkalis, shews us, that there is in
general more earth than water in the last, and more water than earth in
the first.

Nevertheless, water, although it may be intimately mixed with salts, is
neither fixed nor united there by a sufficient force to transform it
into a solid matter like calcareous stone; it resides in salt or acid
under its primitive form, and the best concentrated acid, or the most
deprived of water, which might be looked upon as liquid earth, only
owes its liquidity to the quantity of the air and fire it contains; and
it is no less certain, that they are indebted for their savour to the
same principles. An experiment which I have frequently tried, has fully
convinced me, that alkali is produced by fire. Lime made according
to the common mode, and put upon the tongue, even before slacked by
air or water, has a savour which indicates the presence of a certain
quantity of alkali. If the fire be continued, this lime by longer
calcination, becomes more poignant; and that drawn from furnaces, where
the calcination has subsisted for five or six months together, is
still more so. Now this salt was not contained in the stone before its
calcination; it augmented in proportion to the strength and continuance
of the fire; it is therefore evident, that it is the immediate product
of the fire and air, which incorporate in the substance during its
calcination, and which, by this means, are become fixed parts of it,
and from which they have driven most of the watery molecules it before
contained. This alone appeared to me sufficient to pronounce that fire
is the principal of the formation of the mineral alkali; and we may
conclude, by analogy, that other alkalis owe their formation to the
constant heat of the animal and vegetable from which they are drawn.

With respect to acids, although the demonstration of their formation
by fire and fixed air, is not so immediate as that of alkalis, yet it
does not appear less certain. We have proved, that nitre and phosphorus
draw their origin from vegetable and animal matters: that vitriol comes
from pyrites, sulphur and other combustibles. It is likewise certain
that acids, whether vitriolic, nitrous, or phosphoric, always contain a
certain quantity of alkali; we must, therefore, refer their formation
and savour to the same principle, and by reducing the varieties of
both to one of each, bring back all salts to one common origin: those
which contain most of the active principles of air and fire, will
necessarily have the most power and taste. I understand by power the
force with which salts appear animated to dissolve other substances.
Dissolution supposes fluidity, and as it never operates between two
dry or solid matters, it also supposes the principle of fluidity in
the dissolvent, that is, fire; the power of the dissolvent will be,
therefore, so much the greater, as on one part it contains more of
this active principle; and, on the other hand, its aqueous and terrene
parts will have more affinity with those of the same kind contained
in the substances to dissolve; and, as the degrees of affinity vary,
we must not be surprized at different salts varying in their action
on different substances; their active principle is the same, their
dissolving power the same; but they remain without exercise when the
substance presented repels that of the dissolvent, or has no degree of
affinity with it; but the contrary is the case when there is sufficient
force of affinity to conquer that of the coherence; that is, when the
active principles, contained in the dissolvent, under the form of air
and fire, are found more powerfully attracted by the substance to be
dissolved, than they are by the earth and water they contain. Newton
is the first who has assigned affinities as the causes of chemical
precipitation; Stahl adopted this idea and transmitted it to all the
other chemists; and it appears to be at present universally received as
a truth. But neither Newton nor Stahl saw that all these affinities,
so different in appearance, are only particular effects of the general
force of universal attraction: and, for want of this knowledge, their
theory cannot be either luminous or complete, because they were obliged
to suppose as many trivial laws of different affinities, as there were
different phenomena; instead of which there is in fact only one law
of affinity, a law which is precisely the same as that of universal
attraction.

Salts concur in many operations of Nature by the power they have of
dissolving other substances; for, although it is commonly said, that
water dissolves salt, it is easy to be perceived, that in reality,
when there is a dissolution, both are active, and may be alike called
_dissolvents_. Regarding salt as only a dissolvent, the body to be
dissolved may be either liquid or solid; and, provided the parts of the
salt be sufficiently divided to touch immediately those of the other
substances, they will act and produce all the effects of dissolution.
By this we see how much the action of salts, and the action of the
element of water which contains them, must have influence on the
composition of mineral matters. Nature may produce by this mode, all
that our arts produce by that of fire. Time only is required for salts
and water to produce on the most compact and hard substances, the most
complete division and attenuation of their parts, so as to render them
capable of uniting with all analogous substances, and to separate from
all others; but this time, which to Nature is never wanting, is, of all
things, that which is the most deficient to us: the greatest of all our
arts, therefore, is that of abridging time, that is, to effect that
in one day, which nature takes an age to perform. However vain this
pretension may appear, we must not entirely renounce it, for has not
man discovered the mode of creating fire, of applying it to his use,
and by the means of this element to suddenly dissolve those bodies by
fusion which would require a considerable period by any other means?

We must not, however, conclude that Nature really performs by the means
of water all that we do by fire. The decomposition of every substance
is only to be made by division, and the greater this division the more
the decomposition will be complete. Fire seems to divide as much as
possible those matters which it fuses; nevertheless it may be doubted
whether those which water and acids keep in dissolution are not still
more divided, and the vapours raised by heat contain matters still
further attenuated, in the bowels of the earth, then, by the means
of the heat it includes, and the water which insinuates, there is
made an infinity of sublimations; distillations, chrystallizations,
aggregations, and disjunctions, of every kind. By time all substances
may be compounded and decompounded by these means; water may divide
and attenuate the parts more than fire when it melts them, and those
attenuated parts will join in the same manner as those of fused metal
unite by cooling. Crystallization, of which the salts have given us
an idea, is never performed but when a substance, being disengaged
from every other, is much divided and sustained by a fluid, which
having little or no affinity with it, permits it to unite and form by
virtue of its force of attraction, masses of a figure nearly similar
to its primitive parts. This operation, which supposes all the above
circumstances, may be done by the intermediate aid of fire as well as
by that of water, and is often accomplished by the concurrence of both,
because all this exacts but one division of matter sufficiently great
for its primitive parts to be able to form, by uniting figured bodies
like themselves. Now fire can bring many substances to this state much
better than any other dissolvent, as observation demonstrates to us in
asbestos, and other productions of fire, whose figures are regular, and
which must be looked upon as true crystallizations. Yet this degree of
division, necessary to crystallization, is not the greatest possible,
since in this state the small parts of matter are still sufficiently
large to constitute a mass, which like other masses, is only obedient
to the sole attractive force, and the volumes of which, only touching
in points, cannot acquire the resultive force that a much greater
division might perform by a more immediate contact, and this is what
we see happen in effervescences, where at once, heat and light are
produced by the mixture of two cold liquors.

Light, heat, fire, air, water, and salts, are steps by which we descend
from the top of Nature's ladder to its base, which is fixed earth. And
these are at the same time the only principles that we must admit and
combine for the explanation of all phenomena. These principles are
real, independently of all hypotheses and all method, as are also their
conversion and transformation, which are demonstrated by experience.
It is the same with the element of earth, it can convert itself by
volatilizing and taking the form of the other elements, as those take
that of earth in fixing; it, therefore, appears quite useless to seek
for a substance of pure earth in terrestrial matters. The transparent
lustre of the diamond dazzled the sight of our chemists, when they
considered that stone as a pure elementary fire; they might have said
with as much foundation, that it is pure water, all the parts of which
are fixed to compose a solid diaphanous substance. When we would define
Nature, the large masses should alone be considered, and those elements
have been well taken notice of by even the most ancient philosophers.
The sun, atmosphere, earth, sea, &c. are all great masses on which
they established all their conclusions; and if there ever had existed
a planet of phlogiston, an atmosphere of alkali, an ocean of acid,
or a mountain of diamonds, such might have been looked upon as the
general and real principles of all bodies, but they are only particular
substances, produced, like all the rest, by the combinations of true
elements; and ideas to the contrary would never have been started but
upon the supposition that the earth was neither more simple nor less
convertible than either of the other elements.

In the great mass of solid matter, which the earth represents, the
superficial is the least pure. All the matter deposited by the sea, in
form of sediment, all stones produced by shell-animals, all substances
composed by the combinations of the waste of the animal or vegetable
kingdom, and all those which have been changed by the fires of
volcanos, or sublimated by the internal heat of the globe, are mixed
and transformed substances; and although they compose great masses
they do not clearly represent to us the element of earth. They are
vitrifiable matters, whose mass must be considered as 100,000 times
more considerable than all those other substances, which should be
regarded as the true basis of this element. It is from this common
foundation that all other substances have derived the origin of their
solidity, for all fixed matter, however much decomposed, subsides
finally into glass by the sole action of fire: it resumes its first
nature, when disengaged from the fluid, or volatile matters, which were
united with it; and this glass, or virtreous matter, which composes
the mass of our globe, represents so much the better the element of
earth, as it has neither colour, smell, taste, liquidity, nor fluidity,
qualities which all proceed from the other elements, or belong to them.

If glass be not precisely the element of earth, it is at least the most
ancient substance of it; metals are more recent, and less dignified;
and most other minerals form within our sight. Nature produces glass
only in the particular focus of its volcanos, whereas every day she
forms other substances by the combination of glass with the other
elements. If we would form to ourselves a just idea of her formation
of the globe, we must first consider her processes, which demonstrate
that it has been melted or liquefied by fire; that from this immense
heat it successively passed to its present degree; that in the first
moments, where its surface began to take consistence, inequalities
must be formed, such as we see on the surface of melted matters grown
cold: that the highest mountains, all composed of vitrifiable matters,
existed and take their date from that moment, which is also that of
the separation of the great masses of air, water, and earth; that
afterwards, during the long space of time which the diminution of the
heat of the globe to the point of present temperature supposes, there
were made in these mountains, which were the parts most exposed to
the action of external causes, an infinity of fusions, sublimations,
aggregations, and transformations, by the fire of the sun, and all the
other causes which this great heat rendered more active than they at
present are, and that consequently we must refer back to this date the
formation of metals and minerals which we find in great masses, and in
thick and continued veins. The violent fire of inflamed earth, after
having raised up and reduced into vapours all that was volatile, after
having driven off from its internal parts the matters which compose
the atmosphere and the sea, and at the same time sublimated all the
least fixed parts of the earth, raised them up and deposited them in
every void space, in all the cavities which formed on the surface in
proportion as it cooled; this, then, is the origin and the gradation
of the situation and formation of vitrifiable matters which fire has
divided, formed and sublimated.

After this first establishment (and which still subsists) of
vitrifiable matters and minerals into a great mass, which can be
attributed to the action of fire alone, water which till then formed
with air only a vast volume of vapours, began to take its present
state; it collected and covered the greatest part of the surface of
the earth, on which, finding itself agitated by a continual flux
and reflux, by the action of winds and heat, it began to act on the
works of fire: it changed, by degrees, the superficies of vitrifiable
matters; it transported the wrecks and deposited them in the form of
sediments; it nourished shell-animals, it collected their shells,
produced calcareous stones, formed hills and mountains, which becoming
afterwards dry, received in their cavities all the mineral matters they
could dissolve or contain.

To establish a general theory on the formation of Minerals, we must
begin then by distinguishing with the greatest attention, first, those
which have been produced by the primitive fire of the earth while it
was burning with heat; secondly, those which have been formed from the
waste of the first by the means of water; and thirdly, those which
in volcanos, or other subsequent conflagrations, have a second time
undergone the proof of a violent heat. These three objects are very
distinct, and comprehend all the mineral kingdom; by not losing sight
of them, and by connecting each substance, we can scarcely be deceived
in its origin, or even in the degrees of its formation. All minerals
which are found in masses, or large veins in our high mountains,
must be referred to the sublimation of the primitive fire; all those
which are found in small ramifactions, in threads or in vegetations,
have been formed only from the waste of the first hurried away by the
stillation of waters. We are evidently convinced of this, by comparing
the matter of the iron mines of Sweden with that of our own. These
are the immediate work of water, and we see them formed before our
eyes; they are not attracted by the load stone; they do not contain
any sulphur, and are found only dispersed in the earth; the rest are
all more or less sulphureous, all attracted by the load stone, which
alone supposes that they have undergone the action of fire; they are
disposed in great, hard, and solid masses: and their substance is mixed
with a quantity of asbestos, another index of the action of fire. It is
the same with other metals: their ancient foundation comes from fire,
and all their great masses have been united by its action; but all
their crystallizations, vegetations, granulations, &c. are due to the
secondary causes, in which water is the primary agent.




EXPERIMENTS ON THE PROGRESS OF HEAT IN MINERAL SUBSTANCES.


I caused ten bullets to be made of forged and beaten iron; the first,
of half-inch diameter; the second, of an inch; and soon progressively
to five inches: and as all the bullets were made of iron of the same
forge, their weights were found nearly proportionable to their volumes.

The bullet of half an inch weighed 190 grains, Paris weight; that of
an inch, 1522 grains; that of an inch and a half, 5136 grains; that of
two inches, 12173 grains; that of two inches and an half, 23781 grains;
that of three inches, 41085 grains; that of three inches and a half,
65254 grains; that of four inches, 97388 grains; that of four inches
and an half, 138179 grains; and that of five inches, 190211 grains. All
these weights were taken with very good scales, and those bullets which
were found too heavy, were filed.

While these bullets were making, the thermometer exposed to the open
air was at the freezing point, or some degrees below; but in the pit
where the bullets were suffered to cool, the thermometer was nearly ten
degrees above that point; that is to say, to the degree of temperature
of the pits of the observatory, and it is this degree which I have here
taken for that of the actual temperature of the earth. To know the
exact moment of their cooling to this actual temperature, other bullets
of the same matters, diameters, and not heated, were made use of for
comparison, and which were felt at the same time as the others. By the
immediate touch of the hand, or two hands, on the two bullets, we could
judge of the moment when they were equally cold; and as the greater or
less smoothness or roughness of bodies makes a great difference to the
touch; (a smooth body, whether hot or cold, appearing much more so than
a rough body, even of the same matter, although they are both equally
so) I took care that the cold bullets were rough, and like those
which had been heated, whose surfaces were sprinkled over with little
eminences produced by the fire.


EXPERIMENTS.

I. The bullet of half an inch was heated white in two minutes, cooled
so as to be held in the hand in 12, and to the actual temperature in 39
minutes.

II. That of an inch, heated white in five minutes and a half, cooled
so as to be held in the hand, in 35-1/2 minutes, and to the actual
temperature in one hour and 23 minutes.

III. That of an inch and an half, heated white in nine minutes,
cooled so as to be held in the hand in 58 minutes, and to the actual
temperature in two hours and 35 minutes.

IV. That of two inches heated white in 13 minutes, cooled so as to be
held in the hand in one hour 20 minutes, and to the actual temperature
in three hours 16 minutes.

V. That bullet of two inches and an half heated white in 16 minutes,
cooled so as to be held in the hand in one hour 42 minutes, and to the
actual temperature in four hours 30 minutes.

VI. That bullet of three inches heated white in 19-1/2 minutes, cooled
so as to be held in the hand in two hours seven minutes, and to the
actual temperature in five hours eight minutes.

VII. That of three inches and a half heated white in 23-1/2 minutes,
cooled so as to be held in the hand in two hours 36 minutes, and to the
actual temperature in five hours 56 minutes.

VIII. That of four inches heated white in 27 minutes and a half, cooled
so as to be held in the hand in three hours two minutes, and to the
actual temperature in six hours 55 minutes.

IX. That of four inches and a half heated white in 31 minutes, cooled
so as to be held in the hand in three hours and 25 minutes, and to the
actual temperature in seven hours 46 minutes.

X. That of five inches heated white in 34 minutes, cooled, so as to
be held in the hand, in three hours 52 minutes, and to the actual
temperature in eight hours 42 minutes.

The most constant difference that can be taken between each of the
terms which express the time of cooling, from the instant the bullets
were drawn from the fire, to that when we can touch them unhurt, is
found to be about 24 minutes, for, by supposing each term to increase
24, we shall have 12, 36, 60, 84, 108, 132, 156, 180, 204, 228 minutes.
And the continuation of the real time of these coolings are, 12,
35-1/2, 58, 80, 102, 127, 156, 182, 205, 232 minutes, which approach
the first as nearly as experiment can approach calculation.

So, likewise, the most constant difference to be found between each of
the terms of cooling to actual temperature is found to be 54 minutes,
for by supposing each term to increase 54, we shall have 39, 93, 147,
201, 255, 309, 363, 417, 471, 525 minutes, and the continuation of
the real time of this cooling is found, by the preceding experiments,
to be 39, 93, 145, 196, 248, 308, 356, 415, 466, 522 minutes, which
approaches also nearest to the first.

I made the like experiments upon the same bullets twice or thrice,
but found I could only rely on the first, because each time the
bullets were heated they lost a considerable part of their weight,
which was occasioned not only by the falling off of the parts of the
surface reduced into scoria, but also by a kind of drying, or internal
calcination, which diminishes the weight of the constituent parts,
insomuch that it appears a strong fire renders the iron specifically
lighter each time it is heated; and I have found, by subsequent
experiments, that this diminution of weight varies much, according to
the different quality of the iron. Experience has also confirmed me
in the opinion, that the duration of heat, or the time taken up in
cooling of iron, is not in a smaller, as stated in a passage of Newton,
but in a larger ratio than that of the diameter.

Now if we would enquire how long it would require for a globe as large
as the earth to cool, we should find, after the preceding experiments,
that instead of 50,000 years, which Newton assigns for the earth to
cool to the present temperature, it would take 42,964 years, 221 days,
to cool only to the point where it would cease to burn, and 86,667
years and 132 days, to cool to the present temperature.

It might only be supposed, that the refrigeration of the earth should
be considerably increased, because we imagine that refrigeration
is performed by the contact of the air, and that there is a great
difference between the time of refrigeration in the air and in
vacuo; and supposing that the earth and air cool in the same time in
vacuo, this surplus of time should be reckoned. But, in fact, this
difference of time is very inconsiderable, for though the density of
the medium, in which a body cools, makes something on the duration of
the refrigeration, yet this effect is much less than might be imagined,
since in mercury, which is eleven thousand times denser than air, it
is only requisite to plunge bodies into it about nine times as often
as is required to produce the same refrigeration in air. The principal
cause of refrigeration is not, therefore, the contact of the ambient
medium, but the expansive force which animates the parts of heat and
fire, which drives them out of the bodies wherein they reside, and
impels them directly from the centre to the circumference.

By comparing the time employed in the preceding experiments to heat
the iron globes, with that requisite to cool them, we find that they
may be heated till they become white in one sixth part and a half of
the time they take to cool, so as to be held in the hand, and about
one fifteenth and a half of that to cool to actual temperature, so
that there is a great error in the estimate which Newton made on the
heat communicated by the sun to the comet of 1680, for that comet
having been exposed to the violent heat of the sun but a short time,
could receive it only in proportion thereto, and not only in so great
a degree as that author supposes. Indeed, in the passage alluded to,
he considers the heat of red-hot iron much less than in fact it is,
and he himself states it to be, in a Memoir, entitled, _The Scale of
Heat_, published in the Philosophical Transactions of 1701, which was
many years after the publication of his _principles_. We see in that
excellent Memoir, which includes the germ of all the ideas on which
thermometers have since been constructed; that Newton, after very exact
experiments, makes the heat of boiling water to be three times greater
than that of the sun in the height of summer; that of melted tin,
six times greater; that of melted lead, eight times; that of melted
regulus, twelve times; and that of a common culinary fire, sixteen or
seventeen times; hence we may conclude, that the heat of iron, when
heated so as to become white, is still greater, since it requires a
fire continually animated by the bellows to heat it to that degree.
Newton seems to be sensible of this, for he says, that the heat of iron
in that state seems to be seven or eight times greater than that of
boiling water. This diminishes half the heat of this comet, compared to
that of hot iron.

But this diminution, which is only relative, is nothing in itself, nor
nothing in comparison with that real and very great diminution which
results from our first consideration. For the comet to have received
this heat a thousand times greater than that of red-hot iron, it must
have remained a very long time in the vicinity of the sun, whereas it
only passed very rapidly at a small distance. It was on the 8th of
December, 1680, at 6/1000 distance from the earth to the centre of the
sun; but 24 hours before, and as many after, it was at a distance six
times greater, and where the heat was consequently 36 times less.

To know then the quantity of this heat communicated to the comet by the
sun, we here find how we should make this estimation tolerably just,
and, at the same time, make the comparison with hot iron by the means
of my experiments.

We shall suppose, as a fact, that this comet took up 666 hours to
descend from the point where it then was, and which point was at an
equal distance as the earth is from the sun, consequently it received
an equal heat to what the earth receives from that luminary, and which
I here take for unity; we shall likewise suppose that the comet took
666 hours more to ascend from the lowest point of its perihelium to
this same distance; and supposing also its motion uniform, we shall
perceive, that the comet being at the lowest point of its perihelium,
that is, to 6/1000 of the distance from the earth to the sun, the heat
it received in that motion was 27,766 times greater than that the
earth receives. By giving to this motion a duration of 80 minutes,
viz. 40 for its descent, and 40 for its ascent, we shall have, at 6
distance, 27,776 heat during 80 minutes at 7 distance 20,408 heat also
during 80 minutes, and at 8 distance 15,625 heat during 80 minutes, and
thus, successively, to the distance of 1000, where the heat is one. By
summing up the quantity of heat at each distance we shall find 363,410
to be the total of the heat the comet has received from the sun, as
much in descending as in ascending, which must be multiplied by the
time, that is, by four thirds of an hour; we shall then have 484,547,
which divided by 2,000 represents the solid heat the earth received
in this time of 1332 hours, since the distance is always 1,300, and
the heat always equals one. Thus we shall have 242,547/2000 for the
heat the comet received more than the earth during the whole time of
its perihelium instead of 28,000, as Newton supposed it, because he
took only the extreme point, and paid no attention to the very small
duration of time. And this heat must still be diminished 242,547/2000,
because the comet ran, by its acceleration, as much more way in the
same as it was nearer the sun. But by neglecting this diminution, and
admitting that the comet received a heat nearly 242 times greater than
that of our summer's sun, and, consequently 17-2/7 times greater than
that of hot iron, according to Newton's estimation, or only ten minutes
greater according to this estimation; it must be supposed, that give a
heat ten times greater than that of red hot iron, it required ten times
more time; that is to say, 1332; consequently, we may compare the comet
to a globe of iron heated by a forge fire for 13320 hours, to heat it
to a whiteness.

Now we find by calculation from my experiments, that with a forge fire,
we can heat to a whiteness a globe whose diameter is 228342-1/2 inches
in 799200 minutes, and, consequently, the whole mass of the comet to be
heated to the point of iron to a whiteness, during the short time it
was exposed to the heat of the sun, could only be 223342-1/2 inches in
diameter; and even then it must have been struck on all sides, and at
the same time, by the light of the sun. Thus comets, when they approach
the sun, do not receive an immense nor a very durable heat, as Newton
says, and as we at the first view might be inclined to believe. Their
stay is so short in the vicinity of the sun, that their masses have not
time to be heated, and besides only part of their surface is exposed
to it; this part is burnt by the extreme heat, which by calcining and
volatilizing the matter of this surface, drives it outwardly in vapours
and dust from the opposite side to the sun; and what is called the
tail of the comet, is nothing else than the light of the sun rendered
visible, as in a dark room, by those atoms which the heat lengthens as
it is more violent.

But another consideration very different and infinitely more important,
is, that to apply the result of our experiments and calculation to the
comet and earth, we must suppose them composed of matters which would
demand as much time as iron to cool: whereas, in reality, the principal
matters of which the terrestrial globe is composed, such as clay,
stones, &c. cannot possibly take so long.

To satisfy myself on this point, I caused globes of clay and marl to
be made, and having heated them at the same forge until white, I found
that the clay balls of two inches, cooled in 38 minutes so as to be
held in the hand; those of two inches and an half, in 48 minutes; and
those of three inches, in 60 minutes; which being compared with the
time of the refrigeration of iron bullets of the same diameters, give
38 to 80 for two inches, 48 to 102 for two inches and a half, and 60 to
127 for three inches; so that only half the time is required for the
refrigeration of clay, to what is necessary for iron.

I found also, that lumps of clay, or marl, of two inches, refrigerated
so as to be held in the hand in 45 minutes; those of two inches and a
half in 58; and those of three inches in 75, which being compared with
the time of refrigeration of iron bullets of the same diameters, gives
46 to 80 for two inches, 58 to 102 for two inches and a half, and 75 to
127 for three inches, which nearly form the ratio of 9 to 5; so that
for the refrigeration of clay, more than half the time is required than
for iron.

It is necessary to observe, that globes of clay heated white, lost
more of their weight than iron bullets, even to the ninth or tenth
part of their weight: whereas marl heated in the same fire, lost
scarcely any thing, although the whole surface was covered over with
scales, and reduced into glass. As this appeared singular, I repeated
the experiment several times, increasing the fire, and continuing it
longer than for iron; and although it scarcely required a third of the
time to redden marl, to what it did to redden iron, I kept them in the
fire thrice as long as was requisite, to see if they would lose more,
but I found very trifling diminutions; for the globe of two inches
heated for eight minutes, which weighed seven ounces, two drachms,
and thirty grains, before it was put in the fire, lost only forty-one
grains, which does not make a hundredth part of its weight; and that
of three inches, which weighed twenty-four ounces, five drachms, and
thirteen grains, having been heated by the fire for eighteen minutes,
that is nearly as much as iron, lost only seventy-eight grains, which
does not make the hundredth and eighty-first part of its weight. These
losses are so trifling, that it may be looked upon, in general, as
certain that pure clay loses nothing of its weight in the fire; for
those trifling diminutions were certainly occasioned by the ferruginous
parts which were found in the clay, and which were in part destroyed by
the fire. It is also worthy of observation, that the duration of heat
in different matters exposed to the same fire for an equal time, is
always in the same proportion, whether the degree of heat be greater or
smaller.

I have made similar experiments on globes of marble, stone, lead, and
tin, by a heat only strong enough to melt tin, and I found, that iron
refrigerated in eighteen minutes, so as to be able to hold it in the
hand, marble refrigerated to the same degree in twelve minutes, stone
in eleven, lead in nine, and tin in eight. It is not, therefore, in
proportion to their density, as is commonly supposed, that bodies
receive and lose more or less heat, but in an inverse ratio of their
solidity; that is, of their greater or lesser _non fluidity_; so that,
by the same heat, less time is requisite to heat or cool the most dense
fluid.

To prevent the suspicion of vainly dwelling upon assertion, I think it
necessary to remark upon what foundation I build this theory; I have
found that bodies which should heat in ratio of their diameters, could
be only those which were perfectly permeable to heat, and would heat
or cool in the same time; hence, I concluded that fluids, whose parts
are only held together by a slight connection, might approach nearer to
this perfect permeability than solids, whose parts have more cohesion.
In consequence of this, I made experiments, by which I found, that
with the same heat all fluids, however dense they might be, heat and
cool more readily than any solids, however light, so that mercury, for
example, heats much more readily than wood, although it be fifteen or
sixteen times more dense.

This made me perceive that the progress of heat in bodies cannot, in
any case, be made relatively to their density; and I have found by
experience, that this progress, as well in solids as fluids, is made
rather by reason of their fluidity, or in an inverse ratio of their
solidity. I mean by _solidity_ the quality opposite to fluidity; and I
say, that it is in an inverse ratio of this quality that the progress
of heat is made in both bodies; and that they heat or cool so much the
faster as they are the more fluid, and so much the slower as they are
more solid, every other circumstance being equal.

To prove that solidity, taken in this sense, is perfectly independent
of density, I have found, by experience, that the most or least dense
matters, heat or cool more readily than other more or less dense
matters, for example, gold or lead, which are much more dense than iron
and copper, heat and cool much quicker; while tin and marble, which are
not so dense, heat and cool much faster than iron and copper; and there
are likewise many other matters which come under the same description;
so that density is in no manner relative to the scale of the progress
of heat in solid bodies.

It is likewise the same in fluids, for I have observed, that
quicksilver, which is thirteen or fourteen times more dense than water,
nevertheless heats and cools in less time than water; and spirit of
wine, which is less dense than water, heats and cools much quicker;
so that generally the progress of heat in bodies, as well with regard
to the ingress as egress, has no affinity with their density, and is
principally made in the ratio of their fluidity, by extending the
fluidity to a solid; from hence I concluded, that we should know the
real degree of fluidity in bodies, by heating them to the same heat;
for their fluidity would be in a like ratio as that of the time during
which they would receive and lose this heat; and that it would be the
same with solid bodies. They will be so much the more solid, that
is to say, so much the more _non fluids_, as they require more time
to receive and lose this heat, and that almost generally to what I
presume; for I have already tried these experiments on a great number
of different matters, and from them I have made a table, which I have
endeavoured to render as complete and exact as possible.

I caused several globes to be made of an inch diameter with the
greatest possible precision, from the following matters, which nearly
represent the Mineral kingdom.

M. Tillet, of the Academy of Sciences, made the globe of refined gold
at my particular request, and the whole of them weighed as follows:

                                             oz. d. gr.

  Gold                                        6  2  17
  Lead                                        3  6  28
  Pure silver                                 3  3  22
  Bismuth                                     3  0   3
  Copper-red                                  2  7  56
  Iron                                        2  5  10
  Tin                                         2  3  48
  Antimony melted, and which had
    small cavities on its surface             2  1  34
  Fine                                        2  1   2
  Em                                          1  2  24-1/2
  White marble                                1  0  25
  Pure clay                                   0  7  24
  Marble common of Montbard                   0  7  20
  White gypsum, improperly called
    Alabaster                                 0  6  36
  Calcareous white stone of the quarry
    of Anieres, near Dijon                    6  6   6
  Rock chrystal: it was a little too
    small, and had many defects. I
    presume that without them it
    would have weighed                        0  6  22
  Common glass                                0  6  21
  Pure earth, very dry                        0  6  16
  Oker                                        0  5   9
  Porcelain of the Court de Lauraguais        0  5   2-1/2
  White chalk                                 0  4  49
  Cherrywood, which although lighter
    than most other woods, is that
    which takes in the least fire             0  1  59


I must here observe, that a positive conclusion must not be made of
the exact specific weight of each matter from the preceding table,
for notwithstanding the precaution that was taken to render the
globes equal, yet, as I was obliged to employ different workmen, some
were too large, and others too small. Those which were more than an
inch diameter were diminished, but those of rock chrystal, glass and
porcelain, which were rather too small, we suffered to remain, and only
rejected those of agate, jasper, and porphyry, which were sensibly so.
This precision in size was however not absolutely necessary, for it
could very little alter the result of my experiments.

Previously to ordering these globes, I exposed to a like degree
of fire, a square mass of iron, and another of lead of two inches
diameter, and found, by reiterated essays, that lead heated and
cooled in much less time than iron. I made the same experiment on red
copper, and that required more time to heat and cool than lead, and
less than iron. So that of these three matters, iron appeared the least
accessible to heat, and, at the same time, that which retained it the
longest. From which I learn that the law of the progress of heat in
bodies was not proportionable to their density, since lead, which is
more dense than iron or copper, nevertheless heats and cools in less
time than either. As this object appeared important, I was induced
to have these globes made, and to be more perfectly satisfied of the
progress of heat in a great number of different matters, I always
placed the globes at an inch distance from each other, before the same
fire, or in the same oven, 2, 3, 4, or 5, together with a globe of
tin in the midst of them. In most of my experiments I suffered them
to be exposed to the same active fire till the globe of tin began to
melt, and at that instant they were all removed, and placed on a table
in small cases. I suffered them to cool without moving, often trying
whether I could touch them, and the moment they left off burning, and
I could hold them in my hands half a second, I marked the time which
had passed since I drew them from the fire. I afterwards suffered them
to cool to the actual temperature, of which I endeavoured to judge
by means of touching other small globes of the same matters that had
not been heated. Of all the matters which I put to the trial, there
was only sulphur which melted in a less degree of heat than tin, and
notwithstanding its disagreeable smell I should have taken it for a
term of comparison, but being a brittle matter which diminishes by
friction, I preferred tin, although it required nearly double the heat
to melt.

Having heated together bullets of iron, copper, lead, tin, gres, and
Montbard marble, they cooled in the following order:

  _So as to be held in the hand     _To actual temperature._
  for half a second._
                       Min.                      Min.
    Tin in              6-1/2            In       16
    Lead in             8                In       17
    Gres in             9                In       19
    Common marble in   10                In       21
    Copper in          11-1/2            In       30
    Iron in            13                In       38

By a second experiment with a fiercer fire, sufficient to melt the tin
bullet, the five others cooled.

  _So as to be held in the hand._   _To actual temperature._
                       Min.                      Min.
    Lead in            10-1/2            In       42
    Gres in            12-1/2            In       46
    Common marble      13-1/2            In       50
    Copper             19-1/2            In       51
    Iron               23-1/2            In       54

By a third experiment, with a less degree of fire than the preceding,
the same bullets with a fresh tin bullet, cooled in the following
manner.

  _So as to be held in the hand._   _To actual temperature._
                       Min.                      Min.
    Tin in              7-1/2           In        25
    Lead in             9-1/2           In        25
    Gres in            10-1/2           In        37
    Common marble      12               In        39
    Copper             14               In        44
    Iron               17               In        50

From these experiments, which I made with as much precision as
possible, we may conclude, first, that the time of refrigeration of
iron, so as to be held in the hand, is to that of copper : : 53-1/2 :
45, and so to the point of temperature : : 142 : 125.

2dly, That the time of refrigeration of iron, so as to be held in the
hand, is to that of the first refrigeration of common marble : : 53-1/2
: 35-1/2 and their entire refrigeration : : 142 : 110.

3dly, that the time of refrigeration of iron, to that of gres, so as
to be held in the hand, is : : 53-1/2 : 32 and : : 142 : 102-1/2, for
their entire refrigeration.

4thly, That the time of refrigeration of iron to that of lead, so as
to be held in the hand, is : : 53-1/2 : 27 and 142 : 94-1/2 for their
entire refrigeration.

In an oven hot enough to melt tin, although all the coals and cinders
were drawn out, I placed, on a piece of iron wire, five bullets,
distant from one another about nine lines, after which the oven was
shut, and having drawn them out, in about 18 minutes they cooled,

  _So as to be held in the hand._   _To actual temperature._
                       Min.                      Min.
    Melted tin in       8               In        24
    Silver in          14               In        40
    Gold in            15               In        46
    Copper in          16-1/2           In        50
    Iron in            18               In        56

In the same oven, but with a slower heat, the same bullets with an
other bullet of tin, cooled,

  _So as to be held in the hand._   _To actual temperature._
                       Min.                     Min.
    Tin in              7               In       20
    Silver in          11               In       56
    Gold in            12-1/2           In       40
    Copper in          14               In       43
    Iron in            16-1/2           In       47


In the same oven, but with a still less degree of heat, the same
bullets cooled,

  _So as to be held in the hand._   _To actual temperature._
                      Min.                       Min.
    Tin in             6                In        17
    Silver in          9                In        26
    Gold in            9-1/2            In        28
    Copper in         10                In        31
    Iron in           11                In        35

Having placed in the same oven five other bullets, placed the same and
separated from each other, their refrigeration was in the following
proportions.

  _So as to be held in the hand._   _To actual temperature._
                      Min.                       Min.
    Antimony in        6-1/2            In        25
    Bismuth in         7                In        26
    Lead in            8                In        27
    Zinc in           10-1/2            In        30
    Emery in          11-1/2            In        38

In the same oven, and in the same manner, another bullet of Bismuth was
placed, with six other bullets, which cooled,

  _So as to be held in the hand._   _To actual temperature._
                      Min.                       Min.
    Antimony in        6                In        23
    Bismuth in         6                In        25
    Bismuth in         6                In        25
    Lead in            7-1/2            In        28
    Silver in          9-1/2            In        30
    Zinc in           10-1/2            In        32
    Gold in           11-1/2            In        34
    Emery in          13-1/2            In        39

There was put in the same oven a bullet of glass, another of tin, one
of copper, and one of iron, and they cooled,

_So as to be held in the hand._     _To actual temperature._
                    Min.                         Min.
    Tin in           8                  In        27
    Glass in         8-1/2              In        22
    Copper in       14                  In        42
    Iron in         16                  In        50

Bullets of gold, glass, porcelain, gypsum, and gres, were heated
together, and cooled,

  _So as to be held in the hand._   _To actual temperature._
                      Min.                       Min.
    Gypsum in          8                In        24
    Porcelain in       8-1/2            In        25
    Glass in           2                In        26
    Gres in           10                In        32
    Gold in           14-1/2            In        45

Bullets of silver, common marble, hard stone, white marble, and soft
calcareous stone of Anieres, near Dijon, were heated like the former,
and cooled,

  _So as to be held in the hand._   _To actual temperature._
                      Min.                       Min.
  Soft calcareous
    stone in           8                In        25
  Hard stone in       10                In        34
  Common marble in    11                In        35
  White marble in     12                In        36
  Silver in           13-1/2            In        40

The whole of these experiments were made with the utmost care and
attention, not only by myself but in the presence of several persons,
who also endeavoured to judge of the first degree of temperature by
holding the bullets for half a second in their hands, and the relations
of which are more exact than those of the actual temperature, because
that being variable the result must sometimes vary also.

With a view to avoid that prolixity which would necessarily attend the
continual repetition in a comparative statement of the refrigeration of
these different bodies, we have connected them in a general table, and
taking 10,000 for the standard of comparison, their differences may be
seen at one view.




                                A TABLE

                                OF THE

             _Relations of different Mineral Substances._

    IRON, with

                                 First    Entire
                                 Refrig.  Refrig.

  Emery                   10000 to 9117 -- 9020
  Copper                   ---- to 8512 -- 8702
  Gold                     ---- to 8160 -- 8148
  Zinc                     ---- to 7653 -- 6020
                                   6804
  Silver                   ---- to 7619 -- 7423
  Marble White             ---- to 6774 -- 6704
  Marble common            ---- to 6636 -- 6746
  Stone calcareous hard    ---- to 6617 -- 6274
  Gres                     ---- to 5596 -- 6926
  Glass                    ---- to 5576 -- 5805
  Lead                     ---- to 5143 -- 6482
  Tin                      ---- to 4898 -- 4921
  Stone calcareous soft    ---- to 4194 -- 4659
  Clay                     ---- to 4198 -- 4490
  Bismuth                  ---- to 3580 -- 4081
  Chalk                    ---- to 3086 -- 3878
  Gum                      ---- to 2325 -- 2817
  Wood                     ---- to 1890 -- 1594
  Pumice-stone             ---- to 1627 -- 1268


              EMERY, with

  Copper                  10000 to 8519 -- 8148
  Gold                     ---- to 8513 -- 8560
  Zinc                     ---- to 8390 -- 7693
                                   7458
  Silver                   ---- to 7778 -- 7895
  Stone calcareous hard    ---- to 7304 -- 6963
  Gres                     ---- to 6552 -- 6517
  Glass                    ---- to 5862 -- 5506
  Lead                     ---- to 5718 -- 6643
  Zinc                     ---- to 5658 -- 6000
  Clay                     ---- to 5185 -- 5185
  Bismuth                  ---- to 4949 -- 6060
  Antimony                 ---- to 4540 -- 5827
  Oker                     ---- to 4259 -- 3827
  Chalk                    ---- to 3684 -- 4105
  Gypsum                   ---- to 2368 -- 2947
  Wood                     ---- to 1552 -- 3146

              COPPER, with

  Gold                    10000 to 9136 -- 9194
  Zinc                     ---- to 8571 -- 9250
                                   7619
  Silver                   ---- to 8395 -- 7823
  Marble common            ---- to 7639 -- 8019
  Gres                     ---- to 7333 -- 8160
  Glass                    ---- to 6667 -- 6567
  Lead                     ---- to 6179 -- 7367
  Lead                     ---- to 6179 -- 7367
  Tin                     10000 to 5746 -- 6916
  Stone calcareous tender  ---- to 5168 -- 5633
  Clay                     ---- to 5652 -- 6363
  Bismuth                  ---- to 5686 -- 5959
  Antimony                 ---- to 5130 -- 5808
  Oker                     ---- to 5003 -- 4697
  Chalk                    ---- to 4068 -- 4368

              GOLD, with

  Zinc                    10000 to 2474 -- 9304
                                   8422
  Silver                   ---- to 8936 -- 8686
  Marble white             ---- to 8101 -- 7863
  Marble common            ---- to 7342 -- 7434
  Stone calcareous hard    ---- to 7383 -- 7516
  Gres                     ---- to 7368 -- 7627
  Glass                    ---- to 7103 -- 5232
  Lead                     ---- to 6526 -- 7500
  Tin                      ---- to 6324 -- 6051
  Stone calcareous soft    ---- to 6087 -- 5811
  Clay                     ---- to 5811 -- 5077
  Bismuth                  ---- to 5658 -- 7043
  Porcelain                ---- to 5526 -- 5593
  Antimony                 ---- to 5395 -- 6348
  Oker                     ---- to 5349 -- 4462
  Chalk                    ---- to 4571 -- 4452
  Gypsum                   ---- to 2989 -- 3293

              ZINC, with

  Silver                  10000 to 8904 -- 8990
                                  10015
  Marble white             ---- to 8305 -- 8424
                                   7194
  Gres                     ---- to 6242 -- 7333
                                   5838
  Lead                     ---- to 6051 -- 7947
                                   4940
  Tin                      ---- to 6777 -- 6240
                                   5666
  Stone calcareous soft    ---- to 5536 -- 7719
                                   4425
  Clay                     ---- to 5484 -- 7458
                                   4373
  Bismuth                  ---- to 5343 -- 7547
                                   4232
  Antimony                 ---- to 5246 -- 6608
                                   4135
  Chalk                    ---- to 3729 -- 5862
                                   2618
  Gypsum                   ---- to 3409 -- 4261
                                   2298

              SILVER, with

  Marble white            10000 to 8681 -- 9200
  Marble common            ---- to 7912 -- 9040
  Stone calcareous hard    ---- to 7436 -- 8580
  Gres                     ---- to 7361 -- 7767
  Glass                    ---- to 7230 -- 7212
  Lead                     ---- to 7154 -- 9184
  Tin                      ---- to 6176 -- 6289
  Stone calcareous soft    ---- to 6178 -- 6289
  Clay                     ---- to 6034 -- 6710
  Bismuth                  ---- to 6308 -- 8877
  Porcelain                ---- to 5556 -- 5242
  Antimony                 ---- to 5692 -- 7653
  Oker                     ---- to 5000 -- 5668
  Chalk                    ---- to 4310 -- 5000
  Gypsum                   ---- to 2879 -- 3366
  Wood                     ---- to 2253 -- 1864
  Pumice-stone             ---- to 2059 -- 1525


              WHITE MARBLE, with

  Marble common           10000 to 8992 -- 9405
  Stone hard               ---- to 8594 -- 9130
  Gres                     ---- to 8286 -- 8990
  Lead                     ---- to 7604 -- 5555
  Tin                      ---- to 7143 -- 6792
  Stone calcareous soft    ---- to 6792 -- 7281
  Clay                     ---- to 6400 -- 6286
  Antimony                 ---- to 6286 -- 6792
  Oker                     ---- to 5400 -- 5571
  Gypsum                   ---- to 4920 -- 5116
  Wood                     ---- to 2200 -- 2857


              COMMON MARBLE, with

  Stone hard              10000 to 9483 -- 9665
  Gres                     ---- to 8767 -- 9273
  Lead                     ---- to 7671 -- 8590
  Tin                      ---- to 7424 -- 6666
  Stone soft               ---- to 7327 -- 7959
  Clay                     ---- to 7272 -- 7213
  Antimony                 ---- to 6279 -- 8333
  Oker                     ---- to 6136 -- 6393
  Chalk                    ---- to 5581 -- 6333
  Wood                     ---- to 2500 -- 3279


              HARD CALCAREOUS STONE, with

  Gres                    10000 to 9268 -- 9355
  Glass                    ---- to 8710 -- 8352
  Lead                     ---- to 8571 -- 7931
  Tin                      ---- to 1095 -- 7931
  Stone soft               ---- to 8000 -- 8095
  Clay                     ---- to 6190 -- 6897
  Oker                     ---- to 4762 -- 5517
  Wood                     ---- to 2195 -- 4516


              GRES, with

  Glass                   10000 to 9324 -- 7939
  Lead                     ---- to 8561 -- 8950
  Tin                      ---- to 7667 -- 7633
  Stone soft               ---- to 7644 -- 7193
  Porcelain                ---- to 7364 -- 7059
  Antimony                 ---- to 7333 -- 6170
  Gypsum                   ---- to 4568 -- 5000
  Wood                     ---- to 2368 -- 4828


              GLASS, with

  Lead                    10000 to 9318 -- 8548
  Tin                      ---- to 9107 -- 8679
  Clay                     ---- to 7938 -- 7643
  Porcelain                ---- to 7692 -- 8863
  Oker                     ---- to 6289 -- 6500
  Chalk                    ---- to 6104 -- 6195
  Gypsum                   ---- to 4160 -- 6011
  Wood                     ---- to 2647 -- 5514


              LEAD, with

  Tin                     10000 to 8695 -- 8333
  Stone soft               ---- to 8437 -- 7192
  Clay                     ---- to 7878 -- 8536
  Bismuth                  ---- to 8698 -- 8750
  Antimony                 ---- to 8241 -- 8201
  Oker                     ---- to 6060 -- 7073
  Chalk                    ---- to 5714 -- 6111
  Gypsum                   ---- to 4736 -- 5714


              TIN, with

  Clay                    10000 to 8823 -- 9524
  Bismuth                  ---- to 8889 -- 9400
  Antimony                 ---- to 8710 -- 9156
  Oker                     ---- to 5882 -- 7619
  Chalk                    ---- to 6394 -- 6842
  Gypsum                   ---- to 4090 -- 4912


              STONE CALCAREOUS SOFT, with

  Antimony                10000 to 7742 -- 9542
  Chalk                    ---- to 7288 -- 7312
  Gypsum                   ---- to 4182 -- 5211


              CLAY, with

  Bismuth                 10000 to 8870 -- 9416
  Oker                     ---- to 8400 -- 8571
  Chalk                    ---- to 7701 -- 8000
  Gypsum                   ---- to 5185 -- 8055
  Wood                     ---- to 3437 -- 4545


              BISMUTH, with

  Antimony                10000 to 9349 -- 9572
  Oker                     ---- to 8846 -- 7380
  Chalk                    ---- to 8020 -- 9500


              PORCELAIN, with

  Gypsum                  10000 to 5301 -- 6500


              ANTIMONY, with

  Chalk                   10000 to 8431 -- 7391
  Gypsum                   ---- to 3833 -- 5476


              OKER, with

  Chalk                   10000 to 8954 -- 8889
  Gypsum                   ---- to 6364 -- 9062
  Wood                     ---- to 4074 -- 5128


              CHALK, with

  Gypsum                  10000 to 6667 -- 7920


              GYPSUM, with

  Wood                    10000 to 8000 -- 5260
  Pumice-stone             ---- to 7099 -- 4560


              WOOD, with

  Pumice-stone            10000 to 8750 -- 8182


Notwithstanding the assiduity I used in my experiments, and the care
I took to render the relations exact, I own there are still some
imperfections in the foregoing table; but the defects are trivial,
and do not much influence the general results; for example, it will
easily be perceived, that the relation of zinc to lead being 10,000
to 6,051, that of zinc to tin should be less than 6,000, whereas it
is found 6,777 in the table. It is the same with respect of silver
to bismuth, which ought to be less than 6,308, and also with regard
of lead to clay, which ought to be more than 8,000, but in the table
is only 7,878. This difference proceeded from the leaden and bismuth
bullets not being always the same; they melted, as well as those of tin
and antimony, and, therefore, could not fail to produce variations,
the greatest of which are the three I have just remarked. It was not
possible for me to do better; the different bullets of lead, tin,
bismuth, and antimony, which I successively made use of, were made in
the same manner, but the matter of each might be somewhat different,
according to the quantity of the alloy in the lead and tin, for I had
pure tin only for the two first bullets; besides, there remains very
often a small cavity in the melted bullet, and these little causes are
sufficient to produce the little differences which may be remarked in
the table.

On the whole, to draw from these experiments all the profit that can be
expected, the matters which compose their object must be divided into
four classes, viz. 1. Metals. 2. Semi-metals and Metallic Minerals. 3.
Vitreous and Vitrescible Substances. And 4. Calcareous and Calcinable
substances. Afterwards the matters of each class must be compared
between themselves to discover the cause, or causes, or the order which
follows the progress of heat in each, and then with each other, in
order to deduce some general results.

First. The order of the six metals, according to their _density_, is
tin, iron, copper, silver, lead, and gold; whereas the order in which
they receive and lose their heat is tin, lead, silver, gold, copper,
and iron; so that in tin alone it retains its place.

The progress and duration of heat in metals does not then follow the
order of their density, except in tin, which being the least dense,
is also that which soonest loses its heat; but the order of the five
other metals demonstrates that it is in relation to their fusibility
that they all receive and loose heat; for iron is more difficult to
melt than copper, copper more than gold, gold more than silver, silver
more than lead, lead more than tin; and therefore we may conclude that
it is only by chance if the density and fusibility of tin be found
so united as to place it in the last rank. Nevertheless, it would be
advancing too much to pretend that we must attribute all to fusibility,
and nothing to density. Nature never deprives herself of one of her
properties in favour of another in an absolute manner; that is to say,
in a mode that the first has not any influence on the second. Thus,
density may be of some weight in the progress of heat; but we may
safely affirm, that in the six metals it has very little comparatively
with fusibility.

This fact was neither known to chemists nor naturalists; they did not
even imagine that gold which is more than twice as dense as iron,
nevertheless loses its heat near a third sooner. It is the same with
lead, silver, and copper, which are all more dense than iron, and
which, like gold, heat and cool more readily; for though the object of
this, second memoir was only refrigeration, yet the experiments of the
one that preceded it demonstrate, that there is ingress and egress of
heat in bodies, and that those which receive it most quickly also lose
it the soonest.

If we reflect on the real principles of density, and the cause of
fusibility, we shall perceive, that density depends absolutely on the
quantity of matter which Nature places in a given space; that the more
she can make it enter therein, the more density there will be, and
that gold, in this respect, is of all substances, that which contains
the most matter relatively to its volume. It is for this reason that
it has been hitherto thought, that more time is required to heat or
cool gold than other metals; and it is natural enough to suppose, that
containing double or treble the matter in the same volume, double or
treble time would be required to penetrate it with heat; nay this would
be true, if in every substance the constituent parts were of the same
figure and ranged the same. But in the most dense the molecules of
matter are, probably, of a figure sufficiently regular not to leave
very void places between them; in others which are not so dense, and
their figures more irregular, more vacuities are left, and in the
lightest, the molecules being few, and most likely of a very irregular
figure, a thousand times more void is found than plenitude; for it may
be demonstrated by other experiments, that the volume of even the most
dense substance contains more void space than full matter.

Now, the principal cause of fusibility is the facility which the
particles of heat find in separating these molecules of full matter
from each other; let the sum of the vacuities be greater or less, which
causes density or lightness, it is indifferent to the separation of
the molecules which constitute the plenitude; and the greater or less
fusibility depends entirely on the power of coherence which retains
the massive parts united, and opposes itself more or less to their
separation. The dilatation of the total volume is the first degree of
the action of heat; and in different metals it is made in the same
order as the fusion of the mass, which is performed by a greater degree
of heat or fire. Tin, which melts the most readily, is also that which
dilates the quickest; and iron, which is the most difficult of all to
melt, is likewise that whose dilatation is the slowest.

After these general positions, which appear clear, precise, and founded
on experiments that nothing can contradict, it might be imagined that
ductility would follow the order of fusibility, because the greater
or less ductility seems to depend on the greater or less adhesion of
the parts in each metal; nevertheless, ductility seems to have as much
connection with the order of density, as with that of their fusibility.
I would even affirm that it is in a ratio composed of the two others,
but that would be only by estimation, and a presumption which is,
perhaps not founded; for it is not so easy to exactly determine the
different degrees of fusibility, as those of density; and as ductility
participates of both, and varies according to circumstances, we have
not as yet acquired the necessary knowledge to pronounce affirmatively
on this subject, though it is most certainly of sufficient importance
to merit particular researches. The same metal when cold gives very
different results to what it does when hot, although treated in
the same manner. Malleability is the first mark of ductility; but
that gives only an imperfect idea of the point to which ductility
may extend; nor can simple lead, the most malleable metal, be drawn
into such fine threads as gold, or even as iron, which is the least
malleable. Besides we must assist the ductility of metals with the
addition of fire, without which they become brittle: even iron,
although the most robust, is brittle like the rest. Thus the ductility
of one metal, and the extent of continuity which it can support, depend
not only on its density and fusibility, but also on the manner and
space in which it is treated, and of the addition of heat or fire which
is properly given to it.

II. By comparing those substances which we term _semi-metals_ and
_metallic minerals_, which want ductility, we shall perceive, that
the order of their density is emery, zinc, antimony and bismuth, and
that in which they receive and lose heat, is antimony, bismuth, zinc,
and emery; and which does not in any measure follow the order of
their density, but rather that of their fusibility. Emery, which is a
ferruginous mineral, although as dense again as bismuth, retains heat
longer. Zinc, which is lighter than antimony or bismuth, retains heat
longer than either. Antimony and bismuth, receive and keep it nearly
alike. There are, therefore, semi-metals, and metallic minerals, which,
like metals, receive and lose heat nearly in the same relation as their
fusibility, and partake very little of their density.

But by joining the six metals, and the four semi-metals, or metallic
minerals, which I have tried, we shall find the order of the densities
of these ten mineral substances to be emery, zinc, antimony, tin,
iron, copper, bismuth, silver, lead and gold. And that the order in
which these substances heat and cool, is antimony, bismuth, tin,
lead, silver, zinc, gold, copper, emery and iron, in which there are
two things that do not appear to perfectly agree with the order of
fusibility.

First, Antimony, which, according to Newton, should heat and cool
slower than lead, since by his experiments it requires ten degrees of
the same heat to fuse, of which eight are sufficient for lead; whereas
by my experiments antimony is found to heat and cool quicker than
lead. But it should be observed that Newton made use of the regulus of
antimony, and that I employed only melted antimony in experiments. Now
this regulus of antimony, or native antimony, is much more difficult
to fuse than antimony which has already undergone a first fusion,
therefore that does not make an exception to the rule. On the whole, I
do not know what relation native antimony, or regulus of antimony, may
have with the other matters I have heated and cooled; but I presume,
from the experiments of Newton, that it heats and cools slower than
lead.

Secondly, it is pretended, that zinc fuses more easily than silver,
consequently it should be found before silver in the order indicated
by experiments, if this order were in all cases relative to that of
fusibility; and I own that this semi-metal seems, at the first glance,
to make an exception to the law which is followed by all the others;
but it must be observed, that the difference given by my experiments
between zinc and silver is very trifling. The small globe of silver
which I made use of was of the purest silver, without the least mixture
of copper; but I had my doubts whether that of zinc were entirely
free from copper, or some other metal less fusible; and therefore,
after all my experiments, I returned the globe of zinc to M. Rouelle,
a celebrated professor of chemistry, requesting him carefully to
examine it, which having done, after several trials, he found a pretty
considerable quantity of iron, or saffron of steel in it.

I have, therefore, had the satisfaction of seeing that not only my own
supposition was well founded, but also that my experiments have been
made with sufficient precision to evince a mixture. Thus zinc exactly
follows the order of fusibility, like the other metals and semi-metals,
in the progress of heat, and does not make any exception to the rule.
It cannot therefore, in general, be said that the progress of heat in
metals, semi-metals, and metallic minerals, is in the same ratio, or
even nearly to that of their fusibility.

III. The Vitrescible and Vitreous Matters, which I tried, being ranged
according to their density, are, pumice-stone, porcelain, oker, clay,
glass, rock-chrystal, and gres, for I must observe, that although
chrystal is not set down in the table of the weight of each matter but
for six drachms 22 grains, it must be supposed one drachm heavier,
because it was sensibly too small; and it was for this reason that I
excluded it from the general table of relations; nevertheless, as the
general result agrees with the rest, I can present the following as the
order in which these different substances are cooled:

Pumice-stone, oker, porcelain, clay, glass, crystal and gres, is
according to that of their density, for the oker is here before the
porcelain only because, being a fusible matter, it diminished by the
friction it underwent in the experiments, and, besides, their density
differs so little that they may be looked upon as equal.

Thus the law of the progress of heat in vitrescible and vitreous
matters is relative to the order of their density, and has little or no
relation with their fusibility but by the heat required to fuse those
substances being in an almost equal degree, and the particular degree
of their different fusibility being so near each other that an order
of distinct terms cannot be made; thus their almost equal fusibility
making only one term, which is the extreme of this order, we must not
be astonished that the progress of heat here follows the order of
density, and that these different substances, which are all equally
difficult to fuse, heat and cool more or less quick in proportion to
the matter they contain.

It may be objected to me that glass fuses more easily than clay,
porcelain, oker, and pumice-stone, which, nevertheless, heat and cool
in less time than glass; but the objection will fail when we reflect,
that to fuse glass it is requisite to have a very fierce fire, the
heat of which is so remote from the degrees which glass receives in
our experiments on refrigeration, that it cannot have any influence
on them. Besides, by powdering clay, porcelain, and pumice-stone, and
by giving them their analogous fusers, as we give to sand to convert
it into glass, it is more than probable that we should fuse all the
matters in the same degree of fire, and that, consequently we must look
upon it as equal, or almost equal, with their resistance to fusion;
and it is for this reason that the law of the progress of heat in these
matters is found proportionable to the order of their density.

IV. Calcareous matters, ranged according to the order of their density,
are, chalk, soft stone, hard stone, common marble, and white marble,
which is the same as that of their density. The fusibility is not
here of any weight, because it requires at first a very great degree
of fire to calcine them; and although the calcination divides the
parts, we must look upon the effect only as a first degree and not
as a complete fusion. The whole power of the best burning mirrors is
scarcely sufficient to perform it. I have melted and reduced into a
kind of glass some of these calcareous matters; and I am convinced that
these matters may, like all the rest, be reduced ulteriorly into glass,
without employing for this purpose any fusing matter, and only by the
force of a fire superior to that of our furnaces; consequently the
common term of their fusibility is still more remote, and more extreme,
than that of vitreous matters, and it is for this reason that they also
follow more exactly the order of density in the progress of heat.

White gypsum, improperly called alabaster, is a matter which calcines
like all other plasters by a more moderate heat than that which is
necessary for the calcination of calcareous matters, and it follows the
order of density in the progress of heat which it receives or loses,
for although much more dense than chalk, and a little more so than
white calcareous stone, it heats and cools more readily than either of
those matters. This demonstrates that the more or less easy calcination
and fusion produces the same effects relatively to the progress of
heat. Gypsous matters do not require so much fire to calcine as
calcareous, and it is for this reason that, although more dense, they
heat and cool much quicker.

Thus it may be concluded, that, in general, the _progress of heat in
all Mineral Substances is always nearly in a ratio of their greater or
less facility to calcine, or melt_: but that when their calcination, or
their fusion, are _equally difficult_, and _that they require a degree
of extreme heat_, then the _progress of heat is made according to the
order of their density_.

I have deposited in the Royal Cabinet the globes of gold, silver, and
of all the other metallic and mineral substances which served for the
preceding experiments, that if the truth of their results, and the
general consequences which I have deduced, be doubted, there may be an
opportunity of rendering them more authentic.




OBSERVATIONS ON THE NATURE OF PLATINA.


We have already seen, that of all the Mineral substances which I
subjected to trial it was not the most dense, but the least fusible,
which required the longest time to receive and lose heat. Iron and
emery, which are the most difficult matters to fuse, are, at the same
time, those that heat and cool the slowest. There is nothing except
platina that is accessible to heat, which retains it longer than iron.
This mineral, (which has not long been publicly mentioned) appears,
however, to be more difficult to fuse; the fire of the best furnaces
is not fierce enough to produce that effect, nor even to agglutinate
the small grains, which are all angular, hard, and similar in form to
the thick scale of iron, but of a yellowish colour; and although we
can fuse them without any addition, and reduce them into a mass by a
mirror, platina seems to require more heat than the ore and scales of
iron which we easily fuse in our forge furnaces. In other respects,
the density of platina being much greater than that of iron, the
two quantities of density and non-fusibility unite here to render
this matter the least accessible to the progress of heat. I presume,
therefore, that platina would have been at the head of my table if I
had put it to the experiment; but I was not able to procure a globe
of it of an inch diameter, it being only found in grains[C]; and that
which is in the mass is not pure, it being necessary, in order to fuse
it, to mix it with other matters, which alter its nature. The Comte de
Billarderie d'Angivilliers, who often attended my experiments, led me
to examine this rare metallic substance, not yet sufficiently known.
Chemists who have employed their time in platina, have looked upon it
as a new, perfect, proper, and particular metal, different from all the
rest: they have asserted, that its specific weight was nearly equal to
that of gold; but that it essentially differed in other respects from
gold, having neither ductility nor fusibility. I own I am of a quite
contrary opinion; because a matter which has neither ductility nor
fusibility, cannot rank in the number of metals, whose essential and
common properties are to be ductile and fusible. Neither, after a very
careful examination, did platina appear to me a new metal different
from every other, but rather an alloy of iron and gold formed by
Nature, in which the quantity of gold predominated over the iron; and I
founded this opinion on the following facts:

[C] I have been assured, however, by a person of the first
respectability, that platina is sometimes found in masses, and that
he himself saw a piece that weighed twenty pounds, pure as it was
extracted from the mine.

Of 8 ounces 85 grains of platina, furnished me by Comte d'Angivilliers,
which I presented to a strong loadstone, there remained only 1 ounce,
1 dram, and 98 grains, all the rest was taken away by the loadstone;
therefore, nearly six-sevenths of the whole was attracted by the
loadstone, which is so considerable a quantity, that it is impossible
to suppose that iron is not contained in the intimate substance of
platina, but that it is even there in a very great quantity. I am
convinced it contains much more, for if I had not been weary of these
experiments, which took me up several days, I should have attracted a
great part of the remainder of the 8 ounces by my loadstone, for to the
last it continued to draw some grains one by one, and sometimes two.
There is, therefore, much iron in platina, and it is not simply mixed
with it, as with a foreign matter, but intimately united and making
part of its substance; or, if this is denied, it must be supposed,
that there exists a second matter in Nature which like iron may be
attracted by the loadstone.

All the platina I have had an opportunity of examining, has appeared
to be mixed with two different matters, the one black, and very
attractable by the loadstone; the other in larger grains, of a pale
yellow, and much less magnetic than the first. Between these two
matters, which are the two extremes, are found all the intermediate
links, whether with respect to magnetism, colour, or size of the
grains. The most magnetic, which are at the same time the blackest and
smallest, reduce easily into powder by a very slight friction, and
leave on white paper the same marks as lead. Seven leaves of paper
which were successively made use of to expose the platina to the action
of the loadstone, were blackened over the whole extent occupied by it;
the last left less than the first, in proportion as the grains which
remained were less black and magnetic; the largest grains, which are
yellow, and least magnetic, instead of crumbling into powder like
the small black grains, are very hard, and resist all trituration;
nevertheless, they are susceptible of extension in an agate mortar,
under the reiterated strokes of a pestle of the same matter, and I
flattened and extended many grains to the double or treble extent of
their surface: this part of platina, therefore, has a certain degree
of malleability, and ductility, whereas the black part appears to be
neither malleable nor ductile. The intermediate grains participate of
the qualities of the two extremes: they are brittle and hard, they
break or extend under the strokes of the pestle, and afford a little
powder not so black as the first.

Having collected this black powder and the most magnetic grains that
the loadstone at first attracted, I discovered that the whole was
iron, but in a different state from common iron. The latter reduced
into powder and filings contracts moisture, and rusts very readily;
in proportion as the rust increases, it becomes less magnetic, and
absolutely loses this magnetical quality when entirely and intimately
rusted; whereas this iron powder, or ferruginous sand found in the
platina, is inaccessible to rust, how long soever it may be exposed
to the air and humidity; it is also more infusible and much less
dissoluble than common iron; but is, nevertheless, an iron which
appears to differ only from common iron by a greater purity. This
sand is, in fact, iron divested of all the combustible matter and all
terrene parts which are found in common iron, and even in steel. It
appears endowed and covered with a vitreous varnish which defends it
from all injury. What is very remarkable, this pure iron sand does not
exclusively belong to the platina ore; for I have found it, although
always in small quantities, in many parts where the iron ore has
been dug, and which consumed in my forges. As I submitted to several
trials all the ores I had, before I used them in my experiments, I was
surprised to find in some of them, which were in grains, particles
of iron, somewhat rounded and shining, like the filings of iron,
and perfectly resembling the ferruginous sand of the platina; they
were all as magnetic, all as little fusible, and all as difficult of
solution. Such was the result of the comparison I made on the sand of
platina, and of the sand found in both my iron ores, at the depth of
three feet, in earths where water easily penetrated. I was puzzled
to conceive whence these particles of iron could proceed, how they
had been defended against rust for the ages they were exposed to the
humidity of the earth, and how this very magnetical iron had been
produced in veins of mines, which had not the smallest degree of that
quality. I called experience to my aid, and became at length satisfied
upon these points. I was well convinced that none of our iron ores in
grain were tractable by the loadstone, and well persuaded that all iron
ores, which are magnetical, have acquired that property only by the
action of fire: that the mines of the north, which are so magnetical
as to be sought after by the compass, must owe their origin to fire,
and are formed by the means, or the intermedium of water; from which I
was induced to suppose that this ferruginous and magnetic sand, that
I found in a small quantity in my iron mines, must owe its origin to
fire, and having examined the place I was confirmed in this idea. This
magnetical sand is found in a wood, where, from time immemorial, they
have made, and still continue to make, coal furnaces. It is likewise
more than probable that there were formerly considerable fires here.
Coal and burnt wood produce iron dross, which includes the most fixed
parts of iron that vegetables contain; it is this fixed iron which
forms the sand here spoken of, when the dross is decomposed by the
action of the air, sun, and rain, for then these pure iron particles,
which are not subject to rust, nor to any other kind of alteration,
suffer themselves to be carried away by the water, and penetrate with
it some feet deep into the earth. What I here advance may be verified
by grinding the dross well burnt, and there will be found a small
quantity of this pure iron, which, having resisted the action of the
fire, equally resists that of the solvents, and does not rust at all.

Being satisfied on this head, and having sufficiently compared the
sand and dross taken from the iron ores with that of the platina,
so as to have no doubt of their identity, it was not long before I
was led to conclude, considering the specific gravity of platina,
that if this pure iron sand, (proceeding from the decomposition of
dross) instead of being in an iron mine, was found near to a gold
one, it might, by uniting with that metal, form an alloy which would
be absolutely of the same nature as platina. Gold and iron have a
great affinity; and it is well-known that most iron mines contain a
small quantity of gold; it is also known how to give to gold the tint,
colour, and even the brittleness of iron, by fusing them together.
This iron-coloured gold is used on different golden jewels to vary
the colours; and this gold mixed with iron is more or less grey, and
more or less tempered, according to the quantity of iron which enters
the mixture. I have seen it of a tint absolutely like the colour of
platina; and having enquired of a goldsmith the proportion of gold
and iron therein, he informed me, that in a piece of 24 carats, there
were no more than 18 gold, consequently a fourth part was iron, which
is nearly the proportion found in the natural platina, if we judge of
it by the specific weight; and this gold made with iron is harder and
specifically less weighty than pure gold. All these agreements and
common qualities with platina, have persuaded me, that this pretended
metal is, in fact, only an alloy of gold and iron, and not a particular
substance, a new and perfect metal different from every other, as
chemists have supposed.

It is well known that alloy makes all metals brittle, and that when
there is a penetration, that is, an augmentation in the specific
gravity, the alloy is so much the more tempered as the penetration is
the greater, and the mixture becomes the more intimate, as is perceived
in the alloy called _bell-metal_, although it be composed of two very
ductile metals. Now nothing is more tempered, nor heavier than platina,
which alone ought to make us conclude that it is only an alloy made by
Nature, a mixture of iron and gold, owing in part its specific gravity
to this last, and, perhaps, also, in a great part, to the penetration
of the two matters of which it is composed.

As this matter, heated alone and without any addition, is very
difficult to reduce into a mass, as by the fire of a burning mirror we
can obtain only very small masses, and as the hydrostatical experiments
made on small volumes are so defective, that we cannot conclude any
thing therefrom, it appears to me that the chemists have been deceived
in their estimation of the specific gravity of this mineral. I put some
powder of gold in a little quill, which I weighed very exactly; I put
in the same quill an equal volume of platina, and it weighed nearly a
tenth less; but this gold powder was much too fine in comparison of
the platina. M. Tillet, who besides a profound knowledge of metals,
possessed the talent of making experiments with the greatest precision,
repeated, at my request, this experiment upon the specific weight of
the platina, compared to pure gold; for this purpose, he, like me,
made use of a quill, and cut gold of 24 carats, reduced as much as
possible to the size of the grains of platina, and he found, by eight
experiments, that the weight of platina differed from that of pure
gold very near a fifteenth? but we both observed that the grains of
gold had much sharper angles than the platina: all the angles of the
latter were blunt, and even soft, whereas the grains of this gold had
sharp and cutting angles, so that they could not adjust themselves,
nor heap one on the other as easily as those of platina. The gold
powder I had before made use of was such as is found in river sand,
whose grains adjust themselves much better one against the other, and I
found a about a tenth difference between the specific weight of those
and platina; nevertheless, those are not pure gold, more than two or
three carats being often wanting, which must diminish the specific
weight in the same relation. Thus we have thought we might maintain,
from the result of my experiments, that platina in grains, and such as
Nature produces it, is, at least, an eleventh, or twelfth, lighter than
gold. There is every reason to presume that the error on the density
of platina, proceeded from its not having been weighed in its natural
state, but only after it had been reduced into a mass; and as this
fusion cannot be made but by the addition of other matters, and a very
fierce fire, it is no longer pure platina, but a composition in which
fusing matters are entered, and from which fire has taken the lightest
parts.

Platina, therefore, instead of being of a density almost equal to that
of pure gold, as has been asserted, is only a density between that of
gold and iron, and only nearer this first metal than the last. For
supposing that the cube foot of gold weighed 1326 lb and that of iron
280, that of platina in grains will be found to weigh about 1194 lb.
which supposes more than 3/4 of gold to 1/4 of iron in this alloy, if
there is no penetration; but as we extract 6/7 by the loadstone, it
might be thought, that there is more than 1/4 iron therein: especially
as by continuing this experiment, I am persuaded, we should be able,
with a strong loadstone to bring away all the platina even to the
last grain. Nevertheless, we must not conclude that iron is contained
therein in so great a quantity; for when it is mixed by the fusion with
gold, the mass which results from this alloy is attractable by the
loadstone, although the iron is in no great quantity therein. M. Baume
had a piece of this alloy weighing 66 grains, in which was only entered
6 grains, that is, 1/11 of iron, and this button was easily taken up by
the loadstone. Hence the platina might possibly contain only 1/11 iron,
or 16/11 gold, and yet be attracted entirely by the loadstone; and this
perfectly agrees with the specific weight which is 1/12 less than gold.

But what makes me presume, that platina contains more than 1/11 of
iron, or 16/11 of gold, is, that the alloy from this proportion is
still of the gold colour, and much yellower than the highest coloured
platina, and that 1/4 iron, or 3/4 gold is requisite for the alloy to
be precisely of the natural colour of platina. I am, therefore, greatly
inclined to think that there might possibly be this quantity of 1/4
iron in platina. We were assured by many experiments, that the sand of
this pure iron which contained platina, is heavier than the filings
of common iron. Thus, this cause, added to the effect of penetration,
is sufficient for the reason of this great quantity of iron contained
under the small volume indicated by the specific weight of platina.

On the whole, it is very possible that I may be deceived in some of the
consequences which I have drawn from my observations on this metallic
substance: for I have not been able to make so profound an examination
as I could wish; and what I say is only what I have observed, which may
perhaps serve as a stimulus to other and better researches.

Chance led me to tell my ideas to Conte de Milly, who declared himself
nearly of my opinion. I gave him the preceding remarks to inspect, and
two days after he favoured me with the following observations, and
which he has permitted me to publish.

"I weighed exactly thirty-six grains of platina; I laid them on a
sheet of white paper that I might observe them the better with a
magnifying glass: I perceived three different substances; the first had
the metallic lustre, and was the most abundant; the second, drawing
a little on the black, very nearly resembled a ferruginous metallic
matter, which could undergo a considerable degree of fire, such as the
scoria of iron, vulgarly called _machefer_: the third less abundant
than the two first, i. e. sand, where the yellow, or topaz colour, is
the most predominant. Each grain of sand, considered separate, offered
to the sight regular chrystals of different colours. I remarked some in
an hexagon form, terminating in pyramids like rock chrystal; and this
sand seems to be no other than a _detritus_ of chrystal, or quartz of
different colours.

"I resolved on separating, as exactly as possible, these different
substances, by means of the loadstone, and to put aside the parts most
attractable by the loadstone, from those which were less, and both
from those which were not so at all; then to examine each substance
particularly, and to submit them to different chemical and mechanical
heats.

"I separated these parts of the platina which were briskly attracted at
the distance of two or three lines; that is to say, without the contact
of the loadstone; and for this experiment I made use of a good fictious
magnet; I afterwards touched the metal with this magnet, and carried
off all that would yield to the magnetical force. Being scarcely any
longer attractable, I weighed what remained, and which I shall call No.
4; it was twenty-four grains; No. 1, which was the most sensible to the
magnet, weighed four grains; No. 2 weighed the same; and No. 3, five
grains

"No. 1, examined by the magnifying glass, presented only a mixture of
metallic parts, a white sand bordering on the greyish, flat and round,
or black vitriform sand, resembling pounded scoria, in which very rusty
parts are perceptible: in short, such as the scoria of iron presents
after having been exposed to moisture.

"No. 2 presented nearly the same, excepting that the metallic parts
predominated, and that there were very few rusty particles.

"No. 3 was the same, but the metallic parts were more voluminous;
they resembled melted metal which had been thrown into water to be
granulated; they were flat, and of all sorts of figures, rounded on the
corners.

"No. 4, which had not been carried off by the magnet (but some parts
of which still afforded marks of sensibility to magnetism, when the
magnet was moved under the paper where they were in), was a mixture of
sand, metallic parts, and real scoria, friable between the fingers, and
which blackened in the same manner as common scoria. The sand seemed
to be composed of small rock, topaz, and cornelian chrystals. I broke
some on a steel, and the powder was like varnish, reduced into powder;
I did the same to the scoria; it broke with the greatest facility, and
presented a black powder which blackened the paper like the common.

"The metallic parts of this last (No. 4) appeared more ductile under
the hammer than those of No. 1, which made me imagine they contained
less iron than the first: from whence it follows, that platina may
possibly be no more than a mixture of iron and gold made by Nature, or
perhaps by the hands of men.

"I endeavoured to examine, by every possible means, the nature of
platina: to assure myself of the presence of iron of platina by
chemical means, I took No. 1, which was very attractable by the magnet,
and No. 4, which was not; I sprinkled them with fuming spirit of
nitre; I immediately observed it with the microscope, but perceived no
effervescence: I added distilled water thereon, and it still made no
motion, but the metallic parts acquired new brilliancy, like silver:
I let this mixture rest for five or six minutes, and having still
added water, I threw some drops of alkaline liquor saturated with the
colouring matter of Prussian blue, and very fine Prussian blue was
afforded me on the first.

"No. 4, treated in the same manner, gave the same result. There are
two things very singular to remark in these experiments; first, that
it passes current among chemists who have treated on the platina,
that aquafortis, or spirit of nitre, has no action on it. Yet, as
I have just observed, it dissolves it sufficiently, though without
effervescence, to afford Prussian blue, when we add the alkaline liquor
phlogisticated and saturated with the colouring matter, which, as is
known, participates iron into Prussian blue.

"Secondly, Platina, which is not sensible to the magnet, does not
contain less iron, since spirits of nitre dissolves it enough, and
without effervescence, to make Prussian blue. Whence it follows, that
this substance, which modern chemists, perhaps too greedy of the
marvellous, and too willing to give something novel, have considered as
a ninth metal, may possibly be only a mixture of gold and iron.

"Without doubt there still require many experiments to determine how
this mixture has taken place, if it be the work of Nature or the
effects of some volcano, or simply the produce of the Spaniards'
labours in the New World to acquire gold in the mines of Peru.

"If we rub platina on white linen it blackens it like common scoria,
which made me suspect that it was the parts of iron reduced into scoria
which are found in this platina, and give it this colour, and which
seem, in this state, only to have undergone the action of a violent
fire. Besides, having a second time examined platina with my lens, I
perceived therein different globules of liquid mercury, which made
me suppose that platina might be the produce of the hands of man, in
the following manner:--Platina, as I have been told, is taken out
of the oldest mines in Peru, which the Spaniards explored after the
conquest of the New World. In those dark times only two methods were
known of extracting gold from the sands which contained it; first, by
an amalgama with mercury; secondly, by drying it. The golden sand was
triturated with quicksilver, and when that was judged to be loaded with
the greatest part of the gold, the sand was thrown away, which was
named _crasse_, as useless and of no value.

"The other method was adopted with as little judgment; to extract it
they began by mineralising auriferous metals by means of sulphur, which
has no action on gold, the specific weight being greater than that of
other metals: but to facilitate its precipitation iron was added, which
loaded itself with the superabundant sulphur, and this method is still
followed. The force of fire vitrifies one part of the iron, the other
combines itself with a small portion of the gold, or even silver, which
mixes with the scoria, from whence it cannot be drawn but by strong
fusions, and being well instructed in the suitable intermediums which
are made use of. Chemistry, which is now arrived to great perfection,
affords, in fact, means to extract the greatest part of this gold and
silver: but at the time when the Spaniards explored the mines of Peru,
they were, doubtless, ignorant of the art of mining with the greatest
profit; besides, they had such great riches at their disposal that
they, probably, neglected the means which would have cost them trouble,
care, and time; there is much reason therefore to conclude that they
contented themselves with a first fusion, and threw away the scoria
as useless, as well as the sand which had escaped the quicksilver,
and perhaps they made a mere heap of these two mixtures, which they
regarded as of no value.

"These scoria contained gold and silver, iron under different states,
and that in different proportions unknown to us, but which, perhaps,
are those that gave origin to the platina. The globules of quicksilver
which I observed, and those of gold which I distinctly saw, with the
assistance of a good lens, in the platina I had in my hands, have
given birth to the ideas which I have written on the origin of this
mineral; but I only give them as hazardous conjectures. To acquire
some certainty we must know precisely where the platina mines are
situated, and examine if they have been anciently explored, whether it
be extracted from a new soil, or if the mines be only rubbish, and to
what depth they are found; and, lastly, if they have any appearance of
being placed by the hands of man there or not, which alone can verify
or destroy the conjectures I have advanced."[D]

[D] Baron Siekengen, minister of the elector Palatine, told M. de
Milly, that he had then in his possession two memoirs which had been
given to him by M. Kellner, chemist and metallurgist in the service of
the Prince of Birckenfeld, at Manheim, and which offered to the court
of Spain to return nearly as much gold as they would send him platina.

These observations of Comte de Milly confirm mine in almost every
point. Nature is the same, and presents herself always the same to
those who know how to observe her: thus we must not be surprized that,
without any communication, we observed the same things, and deduced the
same consequence therefrom; that platina is not a new metal, different
from every other, but a mixture of iron and gold. To reconcile his
observations still more with mine, and to enlighten, at the same time,
the doubts which remain on the origin and formation of platina, I have
thought it necessary to add the following remarks:

1. The Comte de Milly distinguishes three kinds of matters in platina,
namely, two, metallic, and the third, non-metallic, of a chrystalline
form and substance. He observed, as well as I, that one of the metallic
matters is very attractable by the magnet, and the other but little,
or not at all. I mentioned these two matters as well as he, but I did
not speak of the third, which is not metallic, because there was none,
or very little, on the platina on which I made my observations. It is
possible that the platina which the Comte made use of was not so pure
as mine, which, I observed with the greatest care, and in which I saw
only some small transparent globules, like white melted glass, which
were united to the particles of platina, or ferruginous sand, and which
were carried any where by the magnet. These transparent globules were
very few, and in eight ounces of platina which I narrowly inspected
with a very strong lens, I never perceived regular crystals. It rather
appeared to me that all the transparent particles were globulous,
like melted glass, and all attached to metallic parts; nevertheless,
as I did not in the least doubt the veracity of the Comte de Milly's
observation, who observed chrystalline particles of a regular form,
and in a great number, in his platina, I thought I ought not to
confine myself solely to the examination of that platina of which I
have spoken; and finding some in the king's cabinet, M. Daubenton and
I examined it together: this appeared to be much less pure than that
we had before made our experiments on; and in it we remarked a great
number of small prismatic and transparent crystals, some of a ruby
colour, others of a topaz, and others perfectly white, which convinced
us of the correctness of the Comte de Milly in his observations; but
this only proves that there are some mines of platina much more pure
than others, and that in those which are the most so, none of these
foreign bodies are found. M. Daubenton also remarked some grains flat
at bottom and rough at top, like melted metal cooled on a plain, and
I very distinctly saw one of these hemispherical grains, which might
indicate that platina is a matter that has been melted by the fire;
but it is very singular, that in this matter, if melted by fire, small
crystals, topaz, and rubies, are found; and I know not whether we
ought not to suspect fraud in those who supplied this platina, who, to
increase the quantity, mixed it with these crystalline sands, for I
never met with these crystals but in one half pound of platina given me
by the Comte de Angilliviers.

2. I, as well as Comte de Milly, found gold sand in platina; it is
readily discovered by its colour, and because it is not magnetical; but
I own that I never perceived the globules of mercury which he states to
have done; yet I do not mean therefore to deny their existence, only
that it appears to me that the sand of gold meeting with the globules
of mercury, in the same matter, they might be soon amalgamated, and not
retain the colour of gold, which I have remarked in all the gold sand
that I could find in half a pound of platina; besides, the transparent
globules, which I have just spoken of, resemble greatly the globules of
live and shining mercury, insomuch that at the first glance it is easy
to be deceived in them.

3. There were by no means so many tarnished and rusty parts in my
first platina as in that of Comte de Milly's, nor was it properly a
rust which covered the surface of those ferruginous particles, but a
black substance produced by fire, and perfectly similar to that which
covers the surface of burnt iron. But my second platina, that which I
had from the royal cabinet, had a mixture of some ferruginous parts,
which under the hammer were reduced into a yellow powder, and had all
the characters of rust. This platina therefore of the royal cabinet,
and that of Comte de Milly, resembling in every respect, it is probable
that they proceeded from the same part, and by the same road. I even
suspect that both had been sophisticated and mixed nearly one half with
foreign crystalline and ferruginous rusty matters, which are not to be
met with in the natural platina.

4. The production of Prussian blue by platina appears evidently to
prove the presence of iron in those parts even of this mineral which
are the least attractable to the magnet, and at the same time confirms
what I have advanced on the intimate mixture of iron in its substance.
The flowing of platina by spirits of nitre, also proves that although
it has no sensible effervescence, this acid attracts the platina in an
evident manner; and the authors who have asserted the contrary, have
followed their common track, which consists in looking on all actions
as null which do not produce an effervescence. These second experiments
of the Comte de Milly would appear to me very important, if they
succeeded always alike.

5. We must however admit that many essential points of information
are wanting to pronounce affirmatively on the origin of platina. We
know nothing of the natural history of his mineral, and we cannot
too greatly exhort those who are able to examine it on the spot, to
make known their observations; and until that is done we must confine
ourselves to conjectures, some of which appear only more probable
than others. For example, I do not imagine platina to be the work of
man. The Mexicans and Peruvians knew how to cast and work gold before
the arrival of the Spaniards, and they were not acquainted with iron,
which nevertheless they must have employed in a great quantity. The
Spaniards themselves did not establish furnaces in this country when
they first inhabited it to fuse iron. There is, therefore, every reason
to conclude, that they did not make use of the filings of iron for
the separation of gold, at least in the beginning of their labours,
which does not go above two centuries and a half back; a time much too
short for so plentiful a production as platina, which is found in large
quantities in many places.

Besides, when gold is mixed with iron, by fusing them together, we may
always, by a chemical process, separate them, and extract the gold:
whereas, hitherto, chemists have not been able to make this separation
in platina, nor determine the quantity of gold contained in this
mineral. This seems to prove, that gold is united with it in a more
intimate manner than the common alloy, and that iron is also in it, in
a different state from that of common iron. Platina, therefore, appears
to me to be the production of nature, and I am greatly inclined to
think, that it owes its first origin to the fire of volcanos. Burnt
iron, intimately united with gold by sublimation, or fusion, may have
produced this mineral, which having been at first formed by the action
of the fiercest fire, will afterwards have felt the impression of
water, and reiterated frictions, which have given it the form of blunt
angles. But water alone might have produced platina; for supposing
gold and iron divided as much as possible by the humid mode, their
molecules, by uniting, will have formed the grains which compose it,
and which from the heaviest to the lightest contain gold and iron; the
proposition of the chemist who offers to render _nearly_ as much gold
as they shall furnish him with platina, seems to indicate, that there
is, in fact, only 1/11 of iron to 10/11 of gold in this mineral, or
possibly less. But the _nearly_ of this chemist is perhaps a fifth, or
fourth, and indeed, if he could realize his promise to a fourth, it
would be doing a great deal, and no vain boast.

Being at Dijon the summer of 1773, the Academy of Sciences and Belles
Letters, of which I have the honour to be a member, expressed a desire
of hearing my observations on platina; and having complied, M. de
Morveau resolved to make some experiments on this mineral; for which
purpose I gave him a portion of that which I had attracted by the
loadstone, and also some which I had found insensible to magnetism,
requesting him to expose it to the strongest fire he could possibly
make. Some time after, he sent me the following experiments, which he
was pleased to subjoin to mine.

"Monsieur the Comte de Buffon, in a journey to Dijon, in the summer
of 1773, having caused me to remark in half a drachm of platina,
which M. de Baume had sent him in 1768, grains in form of buttons,
others flatter, and some black and scaly; and having separated by the
loadstone those which are attractable from those which appeared not so,
I tried to form Prussian blue with both. I sprinkled the fuming nitrous
acid on the non-attractable parts, which weighed 2-1/2 grains. Six
hours after I put distilled water on the acid, and sprinkled alkaline
liquor, saturated with a colouring matter; however there was not a
single atom of blue, the platina had only a little more brightness.
I alike sprinkled the fuming acid on the remaining platina, part of
which was attractable, the same Prussian alkali precipitated a blue
feculency, which covered the bottom of a pretty large bason. The
platina, after this operation, shewed like the first. I washed and
dried it, and found it had not lost 1/4 of a grain, or 1/138 part;
having examined it in this state I perceived a grain of beautiful
yellow, which was pure gold.

"M. de Fourcy had lately told the world, that the dissolution of gold
was thrown down in a blue precipitate by the Prussian alkali, and
had placed this circumstance in a table of affinity; I was tempted
to repeat this experiment, and sprinkled, in consequence, the
phlogisticated alkaline liquor in the dissolution of gold, but the
colour of this dissolution did not change, which made me suspect that
the dissolution of gold made use of by M. de Fourcy might possibly not
have been so pure.

"At the same time the Comte de Buffon having given me a sufficient
quantity of platina to make further assays, I undertook to separate it
from all foreign bodies by a good front; and I have here subjoined the
processes and their results.


EXPERIMENTS.

"I. Having put a drachm of platina, in a cupel, into a furnace, I
kept up the fire two hours, when the covers sunk down, the supporters
having run, nevertheless the platina was only agglutinated; it stuck to
the cupel, and had left spots of a rusty colour. The platina was then
tarnished, even a little black, and had only augmented a quarter of a
grain in weight; a quantity very small in comparison with that which
other chemists have observed. What surprised me still more was, that
this drachm of platina, as well as that I used for other experiments,
had been successively carried away by the loadstone, and made a
portion of 6/7 of eight ounces, of which the Comte de Buffon has before
spoken.

"II. Half a drachm of the same platina, exposed to the same fire in a
cupel, was also agglutinated; I adhered to the cupel, on which it had
left spots of a rusty colour; the augmentation of weight was found to
be nearly in the same proportion, and the surface as black.

"III. I put this half drachm into a new cupel, but instead of a cover I
placed over it a leaden crucible. This I kept in the most extreme heat
for four hours; when it was cooled I found the crucible soldered to the
support, and having broken it I perceived that nothing had penetrated
into the internal part of the crucible, which appeared to be only more
glossy than before. The cupel had preserved its form and position; it
was a little cracked, but not enough to admit of any penetration; the
platina was also not adherent to it, though agglutinated, but in a much
more intimate manner than in the first experiments; the grains were
less angular, the colour more clear, and the brilliancy more metallic.
But what was the most remarkable during the operation, there issued
from its surface, probably in the first moments of its refrigeration,
three drops of water, one of which, that arose perfectly spherical,
was carried up on a small pedicle of the vitreous and transparent
matter. It was of an uniform colour, with a slight tint of red, which
did not deprive it of any transparency; the smallest of the other two
drops had likewise a pedicle, and the other none, but was only attached
to the platina by its external surface.

"IV. I endeavoured to assay the platina, and for that intent put a
drachm of the grains taken up by the loadstone into a cupel, with two
drachms of lead. After having kept up a very strong fire for two hours,
I found an adherent button, covered with a yellowish and spungeous
crust of two drachms twelve grains weight, which announces that the
platina had retained one drachm twelve grains of lead. I put this
button into another cupel in the same furnace, observing to turn it, by
which it only lost twelve grains in two hours; its colour and form were
very little changed. The same piece of platina was put into Macquer's
furnace, and a fire kept up for three hours, when I was obliged to take
it out, because the bricks began to run. The platina was become more
metallic, but it, nevertheless, adhered to the cupel, and this time
it lost 34 grains. I threw it into the fuming nitrous acid to assay
it, and there arising a little effervescence, I added distilled water
thereon. The platina lost two grains, and I remarked some small holes,
like those which its flying off might occasion.

"There then remained only 22 grains of lead in the platina. I began to
form a hope of vitrifying this remaining portion of lead, for which
purpose I put the same piece of platina into a new cupel, and by the
care I took for the admission of air, and other precautions, the
activity of the fire was so greatly augmented that it required a supply
every eleven minutes; to this degree of heat we kept for four hours,
and then permitted it to cool.

"I perceived the next morning that the leaden crucible had resisted,
and that the supporters were only glazed by the cinders. I found a
piece in the cupel, not adhering, of a uniform colour, approaching more
the colour of tin than any other metal, but only a little ragged. It
weighed exactly one drachm. All, therefore, announced that this platina
had endured an absolute fusion, and that it was perfectly pure, for if
we suppose it still contained lead, we must then admit that it had lost
exactly as much of its substance as it had gained of foreign matter;
and such a precision cannot be the effect of pure chance.

"I passed several days with M. Buffon, whose company has the same
charms as his style, and whose conversation is as complete as his
books: I took a pleasure in presenting him with the production of our
essays; we examined them together, and observed, First, that the drachm
of platina, agglutinated by these experiments, was not attractable by
the loadstone; that, nevertheless, the magnetical bar had an action on
the grains that were loosened from it.

"2. The half drachm of the third experiment was not only attractable in
the mass, but the grains of gold separated therefrom did not themselves
give any signs of magnetism.

"3. The platina of the fourth experiment was absolutely insensible to
the loadstone.

"4. The specific weight of this piece was determined by a good
hydrostatical balance, and being, for the greater certainty, compared
to coined and to other very pure gold, used by M. Buffon in his
experiments, their density was found, with water, in which they were
plunged,

  Pure gold  -  19-87/1
  Coin gold  -  17-1/2
  Platina  -    14-2/5

"5. This piece of platina was put upon steel to try its ductability;
it supported the hammer very well for a few strokes; its surface
became flat and even, a little smooth in the parts which were struck,
but it split soon after, and nearly a sixth part separated. The
fracture presented many cavities, some of which had the whiteness and
brilliancy of silver, and in others we remarked several points like
chrystalization; the tops of these points examined with the lens, was
a globule absolutely similar to that of the third experiment. All the
other parts of this piece of platina were compact, the grain finer and
closer than the best brass, which it resembled in colour. We offered
several of these pieces to the loadstone, but not one was attracted
thereby. We powdered them again in an agate mortar, and then remarked
that the magnetical bar raised up some of the smallest every time they
are placed under it.

"This new appearance of magnetism was so much the more surprising,
as the grains were detached from the agglutinated mass of the second
experiment, which seemed to have lost all sensibility at the approach
and contact of the loadstone. In consequence we again took some of
these grains, which were alike powdered, and soon perceived the
smallest parts sensibly attach themselves to the magnetic bar. It is
impossible to attribute this effect to the smoothness of the bar,
or to any other cause foreign to magnetism. A piece of smooth iron,
applied in the same manner on the parts of this platina did not raise
up a single grain.

"By these experiments, and the observations which have arisen
therefrom, we may judge of the difficulty of determining the nature
of platina. It is very certain that it contains some parts which are
verifiable even without the addition of a fierce fire; it is also
certain that all platina contains iron and attractable parts; but if
the Prussian alkali never affords blue but with the grains which the
loadstone attracts, we should conclude, that those which resist it are
pure platina, which of itself has no magnetical virtue, and of which
iron does not make an essential part. We must suppose that a sufficient
fusion, or perfect cupellation, might decide the question; at least,
these operations appear to have, in fact, deprived it of every magnetic
virtue, by separating it from all foreign bodies; but the last
observation proves, in an incontrovertible manner, that this magnetic
property was, in reality, only weakened, and perhaps masked or buried,
since it reappeared when it was ground."

From these experiments of M. de Morveau there results, 1. That we may
expect to meet platina without addition, by applying the fire of it
several times successively, because the best crucibles might not resist
the action of so fierce a fire during the whole time that the complete
operation would require.

2. That by melting it with lead, and assaying them several times, we
should in the end vitrify all the lead and the platina; and that this
experiment would be able to purge it from a part of the foreign matters
it contains.

3. That by melting without any addition, it seems to purge itself
partly into the vitrescible matters it includes, since it emits to its
surface small drops of glass, which form pretty considerable masses,
and which we can easily separate after refrigeration.

4. That by making experiments on Prussian blue with the grains of
platina, which appeared to be most insensible to the loadstone, we were
not always certain of obtaining it; a circumstance which never fails
with grains that have more or less sensibility to magnetism.

5. It appears that neither fusion nor cupellation can destroy all the
iron with which platina is intimately penetrated; the pieces melted or
assayed, appeared, in reality, equally insensible to the action of the
loadstone; but having pounded them in a mortar, we found magnetical
parts; so much the more abundant as the platina was reduced to a fine
powder. The first piece, whose grains were only agglutinated, being
ground, rendered many more magnetical parts than the second and third,
the grains of which had undergone a stronger fusion; but, nevertheless,
being both ground, they furnished magnetical parts; insomuch that it
cannot be doubted that there is iron in platina, after it has undergone
the fiercest efforts of fire, and the devouring actions of the heat in
the cupel. This demonstrates, that this mineral is really an intimate
mixture of gold and iron, which hitherto has not been able to separate.

6. I made another observation with M. Morveau on melted, and afterwards
on ground platina; namely, that it takes in grinding precisely the same
form as it had before it had been melted; all the grains of this melted
and ground platina are similar to those of the natural, as well in form
as variety of size; and they appear to differ only because the smallest
alone suffer themselves to be raised by the loadstone, and in so much
the less quantity as the platina has endured the fire. This seems also
to prove, that, although the fire has been strong enough not only to
burn and vitrify, but even to drive off a part of the iron with other
vitrescible matter which it contains; the fusion, nevertheless, is not
so complete as that of other perfect metals, since, in grinding, it
retakes the same figure as it had before fusion.




EXPERIMENTS ON LIGHT, AND ON THE HEAT IT MAY PRODUCE.




INVENTION OF MIRRORS TO BURN AT GREAT DISTANCES.


The story of the burning glasses of Archimedes is famous; he is said
to have invented them for the defence of his country; and he threw,
say the ancients, the fire of the sun with such force on the enemy's
fleet, as to reduce it into ashes as it approached the ramparts of
Syracuse. But this story, which, for fifteen or sixteen centuries,
was never doubted, has been contradicted, and treated as fabulous in
these latter ages. Descartes, with the authority of a master, has
attacked this talent attributed to Archimedes; he has denied the
possibility of the invention, and his opinion has prevailed over the
testimonies and credit of the ancients. Modern naturalists, either
through a respect for their philosopher, or through complaisance for
their contemporaries, have adopted the same opinion. Nothing is allowed
to the ancients but what cannot be avoided. Determined, perhaps, by
these motives, of which self-love too often is the abettor, have
we not naturally too much inclination to refuse what is due to our
predecessors? and if, in our time, more is refused than was in any
other, is it not that, by being more enlightened, we think we have more
right to fame, and more pretensions to superiority?

Be that as it may, this invention was the cause of many other
discoveries of antiquity which are at present unknown, because the
facility of denying them has been preferred to the trouble of finding
them out; and the burning glasses of Archimedes have been so decried,
that it does not appear possible to re-establish their reputation;
for, to call the judgment of Descartes in question, something more is
required than assertions, and there only remained one sure decisive
mode, but at the same time difficult and bold, which was to undertake
to discover glasses that might produce the like effects.

Though I had conceived the idea, I was for a long time deterred from
making the experiment, from the dread of the difficulty which might
attend it; at length, however, I determined to search after the mode of
making mirrors to burn at a great distance, as from 100 to 300 feet. I
knew, in general, that the power of reflecting mirrors, never extended
farther than 15 or 20 feet, and with refringent, the distance was
still shorter: and I perceived it was impossible in practice to form a
metal, or glass mirror, with such exactness as to burn at these great
distances. To have sufficient power for that, the sphere, for example,
must be 800 feet diameter; therefore, we could hope for nothing of that
kind in the common mode of working glasses; and I perceived also that
if we could even find a new method to give to large pieces of glass, or
metal, a curve sufficiently slight, there would still result but a very
inconsiderable advantage.

But to proceed regularly, it was necessary first to see how much light
the sun loses by reflection at different distances, and what are the
matters which reflect it the strongest; I first found, that glasses
when they are polished with care, reflect the light more powerfully
than the best polished metals, and even better than the compounded
metal with which telescope mirrors are made; and that although there
are two reflectors in the glasses, they yet give a brighter and more
clear light than metal. Secondly, by receiving the light of the sun in
a dark place, and by comparing it with this light of the sun reflected
by a glass, I found, that at small distances, as four or five feet, it
only lost about half by reflection, which I judged by letting a second
reflected light fall on the first; for the briskness of these two
reflected lights appeared to be equal to that of direct light. Thirdly,
having received at the distances of 100, 200, and 300 feet, this light
reflected by great glasses, I perceived that it did not lose any of its
strength by the thickness of the air it had to pass through.

I afterwards tried the same experiments on the light of candles; and to
assure myself more exactly of the quantity of weakness that reflection
causes to this light, I made the following experiments:

I seated myself opposite a glass mirror with a book in my hand, in a
room where the darkness of the night would not permit me to distinguish
a single object. In an adjoining room I had a lighted candle placed at
about 40 feet distance; this I approached nearer and nearer, till I
could read the book, when the distance was about 24 feet. Afterwards
turning the book, I endeavoured to read by the reflected light, having
by a parchment intercepted the part of the light which did not fall
on the mirror, in order to have only the reflected light on my book.
To do so I was obliged to approach the candle nearer, which I did by
degrees, till I could read the same characters clearly by the same
light, and then the distance from the candle, comprehending that of the
book to the mirror, which was only half a foot, I found to be in all
15 feet. I repeated this several times, and had always nearly the same
results; from whence I concluded, that the strength, or quantity, of
direct light is to that of reflected light, as 576 to 225; therefore,
the light of five candles reflected by a flat glass, is nearly equal to
that of the direct light of two.

The light of a candle, therefore, loses more by reflection than by the
light of the sun; and this difference proceeds from the rays of the
former falling more obliquely on the mirror than the rays of the sun,
which come almost parallel. This experiment confirmed what I had at
first found, and I hold it certain, that the light of the sun loses
only half by its reflection on a glass mirror.

This first information being acquired, I afterwards sought what
became of the images of the sun when received at great distances. To
be perfectly understood we must not, as is generally done, consider
the rays of the sun as parallel; and it must also be remembered, that
the body of the sun occupies an extent of about 32 minutes; that
consequently the rays which issue from the upper edge of the disk,
falling on a point of a reflecting surface, the rays which issue
from the lower edge falling also on the same point of this surface,
they form between them an angle of 32 minutes in the incidence, and
afterwards in the reflection, and that, consequently, the image must
increase in size in proportion as it is farther distant. Attention
must likewise be paid to the figure of those images; for example, a
plain square glass of half a foot, exposed to the rays of the sun, will
form a square image of six inches, when this image is received at the
distance of a few feet; by removing farther and farther off, the image
is seen to increase, afterwards to become deformed, then round, in
which state it remains still increasing in size, in proportion as we
are more distant from the mirror. This image is composed of as many of
the sun's disks as there are physical points in the reflecting surface;
the middle point forms an image of the disk, the adjoining points form
the like, and of the same size, which exceed a little the middle disk:
it is the same with the other points, and the image is composed of
an infinity of disks, which surmounting regularly, and anticipating
circularly one over the other, form the reflected image, of which the
middle point of the glass is the centre.

If the image composed of all these disks is received at a small
distance, then their extent being somewhat larger than that of the
glass, this image is of the same figure and nearly of the same extent
as the glass; but when the image is received at a great distance from
the glass, where the extent of the disks is much greater than that
of the glass, the image no longer retains the same figure as the
glass, but becomes necessarily circular. To find the point of distance
where the image loses its square figure, we have only to seek for the
distance where the glass appears under an angle equal to that the sun
forms to our sight, i. e. an angle of 32 minutes, and this distance
will be that where the image will lose its square figure, and become
round, for the disks having always an equal line to the semi-circle,
which measures an angle of 32 minutes for a diameter, we shall find by
this rule that a square glass of six inches loses its square figure at
the distance of about 60 feet, and that a glass of a foot square loses
it at 120 feet, and so on of the rest.

By reflecting a little on this theory we shall no longer be astonished
to find, that at very great distances a large and small glass afford an
image of nearly the same size, and which only differs by the intensity
of the light; we shall no longer be surprised that a round, square,
long, or triangular glass, or any other figure, always yields round
images[E]; and we shall evidently see that images do not increase and
lessen by the dispersion of light, or by any loss in passing through
the air, as some naturalists have imagined; but that, on the contrary,
it is occasioned by the augmentation of the disks, which always occupy
a space of 32 minutes to whatever distance they are removed.

[E] This is the reason that the small images which pass betwixt the
leaves of high and full trees, and which falling on the walks are all
oval or round.

So, likewise, we shall be convinced, by the simple exposition of this
theory, that curves, of any kind, cannot be used with advantage to
burn at a great distance, because the diameter of the focus can never
be smaller than the chord, which measures an angle of 32 minutes, and
that, consequently, the most perfect concave mirror, whose diameter is
equal to this chord, will never produce double the effect of a plane
mirror of the same surface; and if the diameter of a curved mirror were
less than the chord, it would scarcely have more effect than a plane
mirror of the same surface.

When I had well considered the above I had no longer a doubt that
Archimedes could not burn at a distance but with plane mirrors, for,
independently of the impossibility they then felt, and which we feel at
pleasure, of making concave mirrors with so large a focus, I was well
aware that the reflection I have just made could not have escaped this
great mathematician. Besides, there is every reason to suppose that the
ancients did not know how to make large masses of glass; that they were
ignorant of the art of burning it to make large glasses, possessing
only the method of blowing it, and making bottles and vases; from which
consideration I was led to conclude, that it was with plane mirrors of
polished metals, and by the reflections of the sun, that Archimedes
had been enabled to burn at a distance. But as I perceived that glass
mirrors reflected the light more powerfully than the most polished
mirrors, I thought to construct a machine to coincide in the same point
the reflected images by a great number of these plane glasses, being
well convinced that this was the sole mode of succeeding.

Nevertheless, I had still some doubts remaining, which appeared to me
well founded, for thus I reasoned. Supposing the burning distance to
be 240 feet, I perceived clearly that the focus of my mirror could not
have a less than two feet diameter; in which case what would be the
extent I should be obliged to give to my assemblage of plane mirrors to
produce a fire in so great a focus? It might be so great that the thing
would be impracticable in the execution, for, by comparing the diameter
of the focus to the diameter of the mirror, in the best reflecting
mirrors, I observed that the diameter of the Academy's mirror, which
is three feet, was 108 times bigger than its focus, which was no more
than four lines; and I concluded, that to burn as strong at 240 feet it
was necessary that my assemblage of mirrors should be 216 feet diameter
to have a focus of two feet; now a mirror of 216 feet diameter was
certainly an impossible thing.

This mirror of three feet diameter burnt strong enough to melt gold,
and I was desirous to see how much I should gain by reducing its action
to the burning of wood. For this purpose I used circular zones of paper
on the mirrors to diminish the diameter, and I found that there was no
longer power enough to inflame dry wood when its diameter was reduced
to little more than four inches; therefore, taking five inches, or
sixty lines, for the diameter necessary to burn with a focus of four
lines, it appeared, that to burn equally at 210 feet, where the focus
should necessarily have two feet diameter, I should require a mirror
of 30 feet diameter, which appeared still as impossible, or at least
impracticable.

To such positive conclusions, and which others would have regarded
as demonstrations of the impossibility of the mirror, I had only a
supposition to oppose; but an old supposition, on which the more I
reflected the more I was persuaded that it was not without foundation;
namely, that the effects of heat might possibly not be in proportion to
the quantity of light, or, what amounts to the same, that at an equal
intensity of light large focuses must burn brisker than the small.

By estimating heat mathematically, it is not to be doubted but that
the power of a focus of the same length is in proportion to the surface
of the mirror. A mirror whose surface is double that of another, must
have the same sized focus, and this focus must contain double the
quantity of light which the first contained; and in the supposition,
that effects are always in proportion to their causes, it might be
presumed that the heat of this second focus should be double that of
the first.

So likewise, and by the same mathematical estimation, it has always
been thought, that at an equal intensity of light, a small focus ought
to burn as much as a large one, and that the effect of the heat ought
to be in proportion to this intensity of light: _insomuch_ (says
Descartes) _that glasses, or extremely small mirrors, may be made,
which will burn with as much violence as the large_. I at first thought
that this conclusion, drawn from mathematical theory, might be found
false in practice, because heat being a physical quality, of the action
and propagation of which we know not the laws, it seemed to me, that
there was some kind of temerity in thus estimating its effects by a
simple speculation.

I had, therefore, once more, recourse to experiments. I took metal
mirrors of different focuses and different degrees of polish, and by
comparing the different actions on the same fusible or combustible
matters, I found, that at an equal intensity of light, large focuses
constantly have more effect than small, and I discovered the same to be
the case with refracting mirrors.

It is easy to assign the reason of this difference, if we consider that
heat communicates nearer and nearer, and disperses, if I may so speak,
when it is even applied on the same point: for example, if we let the
focus of a burning glass fall on the centre of a crown piece, and that
this focus was only a line in diameter, the heat produced on the centre
disperses and extends over and throughout the whole piece: thus all the
heat, although used at first to the centre of the crown, does not stop
there, and consequently cannot produce so great an effect as if it did.
But if, instead of a focus of a line which falls upon the centre of the
crown, we let fall a focus of equal intensity on the whole crown, every
part being alike heated, then instead of experiencing the less heat, it
acquires an augmentation; for the middle profiting of the heat with the
other points which surround it, the crown piece will be melted in this
latter case, while in the first, it will only be slightly heated.

After these experiments and reflections, I began to entertain sanguine
hopes of making mirrors to burn at a great distance; for I no longer
dreaded as before, the great extent of the focus; I was persuaded, on
the contrary, that a focus of a considerable breadth, as two feet, and
which in the intensity of the light would not be near so great as in a
small focus of four lines, might, nevertheless, produce inflammation,
and with more power; and that, consequently, this mirror, which, by
mathematical theory, ought to have at least thirty feet diameter, would
be reduced to one of eight or ten feet at most, which was not only a
possible, but even a very practicable thing.

I then thought seriously of executing my project: I had at first a
design of trying to burn at 200 or 300 feet distance with circular or
hexagonal glasses of a square foot in surface, and I was desirous of
having four iron carriages for them, with screws to each to move them,
and a spring to adjust them; but the considerable expense that this
required made me quit that idea, and I took two common glasses of six
inches by eight, and a wooden adjustment, which, in fact, was less
solid and precise, but the expence was more consistent with a mere
experiment: the mechanism of which was executed by M. Passement.

It is sufficient to say, that it was at first composed of 168 glasses
of six inches by eight each, about four lines distant from each other;
these glasses moved in all directions, and the four lines of space
between them not only served for the freedom of this motion, but also
to let the operator see the place where he was to conduct his images.
By means of this construction, 168 images could be thrown on one point,
and, consequently, burn at several distances, as at 20, 30, and to 150
feet. By increasing the size of the mirror, or by making other mirrors
like the first, we are certain of throwing fire to still greater
distances, or to increase as much as we please the force or activity of
those first distances.

It is only to be observed, that the motion here spoken of is not very
easy to be executed, and that also there is a very great choice to
be made in the glasses; for they are not all equally good, though
they appear so at the first inspection. I was obliged to pick out of
more than 500 the 168 I made use of. The method of trying them is to
receive at 150 feet distance the reflected image of the sun, as a
vertical plane; we must select those which give a round and terminated
image, and reject those, whose thicknesses being unequal in different
parts, or the surface a little concave or convex, have images badly
terminated, double, treble, oblong, &c. according to the different
defects found in the glasses.

By the first experiment which I made the 23d of March, 1747, at noon, I
set fire to a plank of fir at 66 feet distance, with 40 glasses only,
about a quarter of the mirror. It must be observed that not being yet
mounted, it was very disadvantageously placed, forming an angle with
the sun of twenty degrees declination, and another of more than ten
degrees inclination.

The same day I set fire to a pitchy and sulphureous plank at 126 feet
distance, with eighty-eight glasses, the mirror being still placed
disadvantageously. It is well known, that to burn with the greatest
advantage the mirror should be directly opposed to the sun, as well as
the matters to be inflamed; so that, by supposing a perpendicular plane
on the plane of the mirror, it must pass by the sun, and, at the same
time, through the midst of combustible matters.

The 3d of April, at four o'clock in the afternoon, the mirror being
mounted, produced a slight inflammation on a plank covered with
pitch at 138 feet distance, although the sun was weak and the light
pale. Great care must be taken, when we approach the spot where
the combustible matters are, not to look on the mirror; for if,
unfortunately, the eyes should meet the focus, inevitable blindness
will ensue.

The 4th of April, at eleven in the morning, although the sun appeared
watery, and the sky cloudy, yet it produced, with 154 glasses, so
considerable a heat at 158 feet, that in less than two minutes it made
a deal plank smoke, and which would certainly have flamed, if the sun
had not suddenly disappeared.

The ensuing day, the 5th of April, at three o'clock in the afternoon,
we set fire, in a minute and a half, at 150 feet distance, to a plank
sulphured and mixed with coals, with 154 glasses. When the sun is
powerful, only a few seconds is required to produce inflammation.

The 10th of April in the afternoon, the sun being bright, we set
fire to a fir plank at 150 feet distance, with only 128 glasses: the
inflammation was very sudden, and made in all the extent of the focus,
which was about sixteen inches diameter at this distance.

The same day, at half past two o'clock, we threw the fire on another
plank, partly pitched and covered with sulphur in some places: the
inflammation was made very suddenly; it began by the parts of the wood
which were uncovered, and the fire was so violent, that the plank was
obliged to be dipt in water to extinguish it: there were 148 glasses at
150 feet distance.

The eleventh of April, the focus being only 20 feet distant from the
mirror, it only required 12 glasses to inflame small combustible
matters; with 21 glasses we set fire to another plank which had already
been partly burnt; with 45 glasses we melted a block of tin of 6lb.
weight; and with 117 glasses we melted thin pieces of silver, and
reddened an iron plate; and I am also persuaded, that by using all the
glasses of the mirror we should have been enabled to have melted metals
at 50 feet distance; and as the focus at this distance was six or seven
inches broad, we should be able to make trials on all metals, which
it was not possible to do with common mirrors, whose focus is either
very weak or 100 times smaller than that of mine. I have remarked, that
metals, and especially silver, smoke much before they melt; the smoke
was so striking that it shaded the ground, and it was there I looked on
it attentively, for it is not possible to look a moment on the focus
when it falls on the metal, the lustre being much more dazzling than
that of the sun.

The experiments which I have here related, and which were made
immediately after the invention of the mirrors, have been followed by
a great number of others, which confirm them. I have set fire to wood
at 210 feet distance with this mirror, by the sun in summer; and I am
certain, that with four similar mirrors I could burn at 400 feet, and,
perhaps, at a greater distance. I have likewise, melted all metals,
and metallic minerals, at 25, 30, and 40 feet. We shall find, in the
course of this article, the uses to which these mirrors can be applied,
and the limits that must be assigned to their power for calcination,
combustion, fusion, &c.[F]

[F] It requires about half an hour to mount the mirror and to make all
the images fall on the same point; but when this is once adjusted, it
may be used at all times by simply drawing a curtain.

This mirror burns according to the different inclination given it, and
what gave it this advantage over the common reflecting mirrors was that
its focus was very distant, and had so little curvature, that it was
almost imperceptible: it was seven feet broad by eight feet high, which
makes about the 150th part of the circumference of the sphere, when we
burn at 150 feet distance.

The reason that determined me to prefer glasses of six inches broad
by eight inches high to square glasses of six or eight inches, was,
that it is much more commodious to make experiments upon a horizontal
and level ground than otherwise, and that with this figure, the height
of which exceeded the breadth, the images were rounder; whereas with
square glasses they would be shortened, especially at small distances,
in a horizontal situation.

This discovery furnishes us with many useful hints for physic, and
perhaps for the arts. We know that what renders common reflecting
mirrors most useless for experiments is, that they burn almost always
upwards, and that we are greatly embarrassed to find means to suspend
or support to their focus matters to be melted or calcined. By means
of my mirror we burn concave mirrors downwards, and with so great an
advantage that we have what degree of heat we please; for example, by
opposing to my mirror a concave one of a foot square in the surface,
the heat produced to this last mirror, by using 154 glasses only, will
be upwards of 12 times greater than that generally produced, and the
effect will be the same as if 12 suns existed instead of one, or rather
as if the sun had 12 times more heat.

Secondly, By means of my mirror we shall have the true scale of the
augmentation of heat, and make a real thermometer, whose divisions will
be no longer arbitrary, from the temperature of the air to what degree
of heat we chuse, by letting fall, successively, the images of the sun
one on the other, and by graduating the intervals, whether by means of
an expansive liquor, or a machine of dilatation, and from that we shall
know, in fact, what a double, treble, quadruple, &c. augmentation of
heat is, and shall find out matters whose expansion, or other effects,
will be the most suitable to measure the augmentations of heat.

Thirdly, We shall exactly know how many times is required for the
heat of the sun to burn, melt, or calcine different matters, which
was hitherto only known in a vague and very indefinite manner; and
shall be in a state to make precise comparisons of the activity of
our fires with that of the sun, and have exact relations and fixed
and invariable measures. In short, those who examine my theory, and
shall have seen the effect of my mirror, I think will be convinced the
mode I have used was the only one possible to succeed to burn far off,
for, independant of the physical difficulty of making large concave,
spherical, parybolical mirrors, or of any other curvature whatsoever,
regular enough to burn at 150 feet distance, we shall easily be
convinced that they would not produce but nearly as much effect as
mine, because the focus would be almost as broad; that besides, these
curved mirrors, if even it should be possible to make them, would have
the very great disadvantage to burn only at a nigh distance, whereas
mine burns at all distances; and, consequently, we shall abandon the
scheme of making mirrors to burn at a great distance by means of
curves, which has uselessly employed a great number of mathematicians
and artists, who were always deceived, because they considered the rays
of the sun as parallel, whereas they should be considered as they are,
namely, as forming angles of all sizes, from 0 to 32 minutes, which
makes it impossible, whatsoever curve is given to a mirror, to render
the diameter of the focus smaller than the chord, which measures 32
minutes. Thus, even if we could make a concave mirror to burn at a
great distance; for example, at 150 feet, by employing all its points
on a sphere of 600 feet diameter, and by employing an uncommon mass
of glass or metal, it is evident that we shall have a little more
advantage than by using, as I have done, only small plane mirrors.

On the whole, although this mirror is susceptible of a very great
perfection, both for the adjustment, and many other particulars, and
though I think I shall be able to make another, whose effects will be
superior, yet, as every thing has its limits, it must not be expected
that every one can be formed to burn at extreme distances; to burn,
for example, at the distance of half a mile, a mirror 200 times larger
would be required; and I am of opinion that more will never be effected
than to burn at the distance of 8 or 900 feet. The focus, whose motion
is always correspondent to that of the sun, moves so much the quicker
as it is farther distant from the mirror; and at 90 feet it would move
about six feet a minute.

However, as I have given an account of my discovery, and the success of
my experiments, I should render to Archimedes, and the ancients, the
glory that is their due. It is certain that Archimedes could perform
with metal mirrors what I have done with glass, and that, consequently,
I cannot refuse him the title of the first inventor of these mirrors,
and the opportunity he had of using them rendered him, without doubt,
more celebrated than the merit of the thing itself.

Many advantages may be derived from the use of these mirrors; by an
assemblage of small mirrors, with hexagonal planes, and polished steel,
which will have more solidity than glasses, and which would not be
subject to the alterations which the light of the sun may cause, we may
produce very useful effects, and which would amply repay the expences
of the construction of the mirror.

"For all evaporations of salt waters, where great quantities of
wood and coal are consumed, or structures raised for the purpose of
carrying the waters off, which cost more than the construction of many
mirrors, such as I mention; for the evaporation of salt waters, only an
assemblage of twelve plane mirrors of a square foot each is necessary.
The heat reflected by their focuses, although directed below their
level, and at fifteen or sixteen feet distance, will be still great
enough to boil water, and consequently produce a quick evaporation:
for the heat of boiling water is only treble the heat of the sun in
summer; and as the reflection of a well polished plane surface only
diminishes the heat one half, only six mirrors are required to produce
at the focus a heat equal to boiling water; but I shall double the
number to make the heat communicate quicker; and likewise by reason of
the loss occasioned by the obliquity, under which the light falls on
the surface of the water to be evaporated, and because salt water heats
slower than fresh. This mirror, whose assemblage would form only a
square four feet broad by three high, would be easy to be managed; and
if it were required to double or treble the effects in the same time,
it would be better to make so many similar mirrors, than to augment the
scale of them; for water can only receive a certain quantity of heat,
and we should not gain any thing by increasing this degree; whereas, by
making two focuses with two equal mirrors, we should double the effect
of the evaporation, and treble it by three mirrors, whose focuses would
fall separately one from the other on the surface of the water to be
evaporated. We cannot avoid the loss caused by the obliquity; nor can
it be remedied but by suffering a still greater, that is, by receiving
the rays of the sun on a large glass, which would reflect them broken
on the mirror; for then it would burn at bottom instead of the top,
but it would lose half the heat by the first reflection, and half of
the remainder by the second; so that instead of six small mirrors, it
would require a dozen to obtain a heat equal to boiling water. For the
evaporation to be made with more success, we ought to diminish the
thickness of the water as much as possible; a mass of water a foot deep
will not evaporate nearly so quick as the same mass reduced to six
inches, and increased to double the superfices. Besides, the bottom
being nearer the surface, it heats quicker, and this heat, which the
bottom of the vessel receives, contributes still more to the celerity
of the evaporation.

2. These mirrors may be used with advantage to calcine plaisters, and
even calcareous stones, but they would require to be larger, and the
matters placed in an elevated situation, that nothing might be lost by
the obliquity of the light. It has already been observed that gypsum
heats as soon again as soft calcareous stone, and nearly twice as quick
as marble, or hard calcareous stone; their calcination, therefore,
must be in a respective ratio. I have found by an experiment repeated
three times, that very little more heat is required to calcine white
gypsum, called alabaster, than to melt lead. Now the heat necessary
to melt lead is, according to the experiments of Newton, eight times
stronger than the heat of the summer sun; it therefore would require
at least sixteen small mirrors to calcine gypsum; and because of the
losses thereby occasioned, as well by the obliquity of the light as by
the inequality of the focus, which is not removed above fifteen feet,
I presume it would require twenty, and perhaps twenty-four mirrors of
a foot square each, to calcine gypsum in a short time, consequently it
would require an assemblage of forty-eight small mirrors to calcine the
softest calcareous stone, and seventy-two of a foot square to calcine
hard calcareous stones. Now a mirror twelve feet broad by six feet
high, would be a large and cumbersome machine; yet we might conquer
these difficulties if the product of the calcination were considerable
enough to surpass the expense of the consumption of wood. To ascertain
this, we ought to begin by calcining plaister with a mirror of
twenty-four pieces, and if that succeeded, to make two other similar
mirrors, instead of making a large one of seventy-two pieces; for by
coinciding the focuses of these three mirrors of twenty-four pieces, we
should produce an equal heat, strong enough to calcine marble or hard
stone.

But a very essential matter remains doubtful, that is, to know how much
time would be requisite, for example, to calcine a cubical foot of
matter, especially if that foot were struck with the heat only in one
part. Some time would pass before the heat penetrated its thickness;
during this time, a great part of the heat would be lost, and which
would issue from this piece of matter after it had entered it. I fear,
therefore, much that the stone not being touched by the heat on every
side at once, the calcination would be slower, and the produce less.
Experience alone can decide this, but it would be at least necessary to
attempt it on gypsous matters, whose calcination is as quick again as
calcareous stone.

By concentrating this heat of the sun in a kiln, which has no other
opening than what admits the light, a great part of the heat would
be prevented from flying off, and by mixing with calcareous stone a
small quantity of coal dust, which is the cheapest of all combustible
matters, this slight supply of food would suffice to feed and augment
the quantity of heat, which would produce a more ample and quick
calcination, and at very little expense.

3. These mirrors of Archimedes might be, in fact, used to set fire to
the sails of vessels, and even to pitched wood at more than 150 feet
distance; they might also be used against the enemy, by burning the
grain and other productions of the earth; this effect would be no less
sudden than destructive; but we will not dwell on the means of doing
mischief, conceiving it to be more our duty to think on those which may
do some real service to mankind.

4. These mirrors furnish the sole means of exactly measuring heat.
It is evident that two mirrors, whose luminous images unite, produce
double heat in all the points of their surfaces, that three, four,
five, or more mirrors, will also give a treble, quadruple, quintuple,
&c. heat, and that, consequently, by this mode we can make a
thermometer whose divisions will not be too arbitrary, and the scales
different, like those of the present thermometers. The only arbitrary
thing which would enter into the composition of the thermometer, would
be the supposition of the total number of the parts of the quicksilver
by quitting the degree of absolute cold; but by taking it to 10000
below the congelation of water, instead of 1000, as in our common
thermometers, we should approach greatly towards reality, especially
by choosing the coldest day in winter to mark the thermometers, for
then every image of the sun would give it a degree of heat above the
temperature of ice. The point to which the mercury rises by the first
image of the sun, would be marked 1, and so on to the highest, which
might be extended to 36 degrees. At this degree we should have an
augmentation of heat, thirty-six times greater than that of the first,
eighteen times greater than that of the second, twelve times greater
than that of the third, nine times greater than that of the fourth,
and so on; this augmentation of thirty-six of heat above that of ice
would be sufficient to melt lead; and there is every appearance to
think that mercury, which volatilizes by a much less heat, would by
its vapour break the thermometer. We cannot therefore, at most, extend
the division farther than twelve, and perhaps not farther than nine
degrees, if mercury be used for these thermometers, and by these means
we shall have only nine degrees of the augmentation of heat. This is
one of the reasons which induced Newton to make use of linseed oil
instead of quicksilver; and, in fact, by making use of this liquor,
we can extend the division not only to twelve degrees, but as far
as to make this oil boil. I do not propose spirits of wine, because
that liquor decomposes in a very short time, and cannot be used for
experiments of a strong heat.[G]

[G] Many travellers have told and written to me, that Reaumur's
thermometers of spirit of wine, became quite useless to them, because
this liquid lost its colour, and became charged with a sort of mud in a
very short time.

When on the scale of these thermometers filled with oil or mercury,
the first divisions 1, 2, 3, 4, &c. are marked to indicate the double,
treble, quadruple, &c. augmentations of heat, we must search after the
aliquot parts of each division; for example, of the point 1-1/4, 2-1/4,
3-1/4, &c. or 1-1/2, 2-1/2, 3-1/2, &c. and 1-3/4, 2-3/4, 3-3/4, and
which will be obtained in an easy manner, by covering the 1/4, 1/2,
or 3/4, of the superfices of one of those small mirrors; for then the
image which it reflects, will contain only the 1/4, 1/2, or 3/4, of
the heat which the whole image will contain, and, consequently, the
division of the aliquot parts will be as exact as those of the whole
numbers.

If once we succeed in this real thermometer, which I call real,
because it actually marks the proportion of the heat, every other
thermometer whose scale is arbitrary and different, will become not
only superfluous, but even inimical, in many cases, to the precision of
natural truths sought after by these means.

5. By means of three mirrors we may easily collect in their entire
purity, the volatile parts of gold, silver, and other metals and
minerals; for, by exposing to the large focus of those mirrors a large
piece of metal, as a dish, or silver plate, we shall see smoke issue
from it in great abundance, and for a considerable time, till the
metal is in fusion; and by giving only a smaller heat than what fusion
requires, we shall evaporate the metal so as to diminish the weight
considerably.

I am certain of this circumstance, which also elucidates the intimate
composition of metals. I was desirous of collecting this plentiful
vapour, which the pure fire of the sun causes to issue from metal,
but I had not the necessary instruments, and I can only recommend to
chemists and naturalists to follow this important experiment, the
results of which would be as much less equivocal as the metallic vapour
is pure; whereas, in all like operations made with common fire, the
metallic vapour is necessarily mixed with other vapours proceeding from
combustible matters, which serve for food to this fire.

Besides, this means is the only one we have to volatilize fixed metals,
such as gold and silver; for I presume that this vapour, which I have
seen rise in such great quantities from these fixed metals, heated in
the large focus of my mirror, is neither of water, nor of any other
liquor, but of the parts even of the metal which the heat detaches by
volatilizing them. By receiving these vapours of different metals, and
thus mixing them together, more intimate and pure alloys would be made
than can be by fusion, and the mixture of these metals when melted,
which never perfectly unites on account of the inequality of their
specific weight, and many other circumstances which are opposed to the
intimate and perfect equality of the mixture. As the constituent parts
of the metallic vapours are in a much greater state of division than
fusion, they would join and unite closer and more readily. In short,
we should attain the knowledge of a general fact by this mode, and
which, for many reasons, I have a long time suspected, that there is
penetration in all alloys made in this manner, and that their specific
weight would be always greater than the sum of the specific weights
of the matters of which they are composed: for penetration is only a
greater degree of intimacy; every thing equal in other respects will
be so much the greater as matters will be in a more perfect state of
division.

By reflecting on the vessels used to receive and collect these metallic
vapours, I was struck with an idea, which appeared to me to be of too
great utility not to publish; it is also easy enough to be realized by
good able chemists; I have even communicated it to some of them, who
appeared to be quite satisfied with it. This idea is to freeze mercury
in this climate, and with a much less degree of cold than that of the
experiments of Petersburgh or Siberia. For this purpose the vapour
of mercury is only required to be received, and which is the mercury
itself volatilized by a very moderate heat in a crucible, or vessel,
to which we give a certain degree of artificial cold. This vapour, or
this mercury, minutely divided, will offer, to the action of the cold,
surfaces so large, and masses so small, that instead of 187 degrees of
cold requisite to freeze mercury, possibly 18 or 20 will be sufficient,
and perhaps even less to freeze it when in vapour. I recommend this
important experiment to all those who endeavour earnestly for the
advancement of the sciences.

To these principal uses of the mirror of Archimedes, I could add
many other particular ones; but I have confined myself to those only
which appeared the most useful, and the least difficult to be put in
practice; nevertheless I have subjoined some experiments that I made
on the transmission of light through transparent bodies, to give some
new ideas on the means of seeing objects at a distance with the naked
eye, or with a mirror, like that spoken of by the ancients, and by the
effect of which vessels could be perceived from the port of Alexander,
as far as the curvature of the earth would permit.

Naturalists at present know, that there are three causes which prevent
the light from uniting in a point, when its rays have passed the
objective glass of a common mirror. The first is the spherical curve of
this glass, which disperses a part of the rays in a space terminated
by a curve. The second is the angle under which the object appears to
the naked eye: for the breadth of the focus of the objective glass has
a diameter nearly equal to the chord of which this angle measures.
The third is the different refrangibility of the light; for the most
refrangible rays do not collect in the same place with the lesser.

The first cause may be remedied by substituting, as Descartes has
proposed, elliptical, or hyperbolical, glasses to the spherical. The
second is to be remedied by a second glass, placed to the focus of the
objective, whose diameter is nearly equal the breadth of this focus,
and whose surface is worked on a sphere of a very short ray. The third
has been found to be remedied, by making telescopes, called Acromatics,
which are composed of two sorts of glasses, which disperse the coloured
rays differently; so that the dispersion of the one is corrected
by the other, without the general refraction, which constitutes the
mirror, being destroyed. A telescope 3-1/2 feet long, made on this
principle, is in effect equivalent to the old telescopes of 25 feet.

But the remedy of the first cause is perfectly useless at this time,
because the effect of the last being much more considerable, has such
great influence on the whole effect, that nothing can be gained by
substituting hyperbolical, or elliptical glasses to spherical, and
this substitution could not become advantageous, but in the case where
the means of correcting the effect of the different refrangibility of
the rays of light might be found; it seems, therefore, that we should
do well to combine the two means, and to substitute, in acromatic
telescopes, elliptical glasses.

To render this more obvious, let us suppose the object observed to be a
luminous point without extent, as a fixed star is to us. It is certain,
that with an objective glass, for example, of 30 feet focus, all the
images of this luminous point will extend in the form of a curve to
this focus, if it be worked on a sphere; and, on the contrary, they
will unite in one point if this glass be hyperbolical; but if the
object observed have a certain extent, as the moon, which occupies
half a degree of space to our eyes, then the image of this object will
occupy a space of three inches diameter in the focus of the objective
glass of thirty feet; and the aberration caused by the sphericity
producing a confusion in any luminous point, it produces the same on
every luminous point of the moon's disk, and, consequently, wholly
disfigures it. There would be, then, much disadvantage in making use of
elliptical glasses or long telescopes, since the means have been found,
in a great measure, to correct the effect produced by the different
refrangibility of the rays of light.

From this it follows, that if we would make a telescope of 30 feet,
to observe the moon, and see it completely, the ocular glass must be
at least three inches diameter, to collect the whole image which the
objective glass produces to its focus; and if we would observe this
planet with a telescope of 60 feet, the ocular glass must be at least
six inches diameter, because the chord which the angle measures under
which the moon appears to us, is, in this case, nearly six inches;
therefore astronomers never make use of telescopes that include the
whole disk of the moon, because they would magnify but very little. But
if we would observe the planet Venus with a telescope of 60 feet, as
the angle under which it appears to us is only 60 seconds, the ocular
glass can only have four lines diameter; and if we make use of an
objective of 120 feet, an ocular glass of eight lines diameter would
suffice to unite the whole image which the objective forms to its focus.

Hence we see, that even if the rays of light were equally refrangible
we could not make such strong telescopes to see the moon with as to see
the other planets, and that the smaller a planet appears to our sight
the more we can augment the length of the telescope, with which we can
see it wholly. Hence it may be well conceived, that in this supposition
of the rays, equally refrangible, there must be a certain length more
advantageously determined than any other for each different planet, and
that this length of the telescope depends not only on the angle under
which the planet appears to our sight, but also on the quantity of
light with which it is brightened.

In common telescopes the rays of light being differently refrangible,
all that could be done in this mode to give them perfection would be of
very little advantage, because, that under whatever angle the object,
or planet, appears to our sight, and whatever intensity of light it
may have, the rays will never collect in the same part; the longer the
telescope the more interval it will have between the focus of the red
and violet rays, and consequently the more confused the image of the
object observed.

Refracting telescopes, therefore, can be rendered perfect only by
seeking for the means of correcting this effect of the different
refrangibility, either by composing telescopes of different densities,
or by other particular means, which would be different according to
different objects and circumstances. Suppose, for example, a short
telescope, composed of two glasses, one convex and the other concave;
it is certain that this telescope might be reduced to another whose
two glasses would be plain on one side, and on the other bordering on
spheres, whose rays would be shorter than that on the spheres on which
the glasses of the first telescopes have been constructed. However,
to avoid a great part of the effect of the different refrangibility
of the rays, the second telescope may be made with one single piece
of massive glass, as I had it done with two pieces of white glass,
one of two inches and a half in length, and the other one inch and a
half; but then the loss of transparency is a greater inconvenience
than the different refrangibility which it corrects, for these two
small massive telescopes of glass are more obscure than a small common
telescope of the same glass and dimensions; they indeed give less
iris, but are not better; for in massive glass the light, after having
crossed this thickness of glass, would no longer have a sufficient
force to take in the image of the object to our eye. So to make
telescopes 10 or 20 feet long, I find nothing but water that has
sufficient transparency to suffer the light to pass through this great
thickness. By using, therefore, water to fill up the intervals between
the objective and the ocular glass, we should in part diminish the
effect of the different refrangibility, because water approaches nearer
to glass than air, and if we could, by loading the water with different
salts, give it the same refringent degree of power as glass, it is not
to be doubted, that we should correct still more, by this means, the
different refrangibility of the rays. A transparent liquor should,
therefore, be used, which would have nearly the same refrangible power
as glass, for then it would be certain that the two glasses, with their
liquor between them, would in part correct the effect of the different
refrangibility of the rays, in the same mode as it is corrected in the
small massive telescope which I speak of.

According to the experiments of M. Bouguer, the thickness of a line of
glass destroys 2/7 of light, and consequently the diminution would be
made in the following proportion:

Thickness, 1, 2, 3, 4, 5, 6 lines

Diminution, 2/7, 10/49, 50/343, 250/2401, 1250/16807, 6250/117649

So that by the sum of these six terms we should find, that the light
which passes through six lines of glass would lose 102024/117649, that
is about 10/11 of its quantity. But it must be considered, that M.
Bouguer makes use of glasses which are but little transparent, since he
has observed, that the thickness of a line of these glasses destroys
2/7 of the light. By the experiments which I have made on different
kinds of white glass, it has appeared to me that the light diminishes
much less. These experiments are easy to be made, and are what all the
world may repeat.

In a dark chamber, whose walls were blackened, and which I made use of
for optical experiments, I had a candle lighted of five to the pound;
the room was very large and the candle the only light in it; I then
tried at what distance I could read by this light, and found that I
read very easily at 24 feet four inches from the candle. Afterwards,
having placed a piece of glass, about a line thick, before it, at two
inches distance, I found that I still read very plainly at 22 feet nine
inches; and substituting to this glass another piece of two lines in
thickness and of the same glass, I read at 21 feet distance from the
candle. Two of the same glasses joined one to the other, and placed
before the candle diminished the light so much that I could only read
at 17-1/2 feet distance; and at length, with three glasses, I could
only read at 15 feet. Now the light of a candle diminishing as the
square of the distance augments, its diminution should have been in the
following progression, if glasses had not been interposed: 2--24-1/3.
2--22-3/4. 2--21. 2--17-1/2. 2--15, or 592-1/9. 517-9/15. 441. 306-1/4.
225. Therefore the loss of the light, by the interposition of the
glasses, is in the following progression: 84-79/144. 151. 285-7/9.
367-1/4.

From hence it may be concluded, that the thickness of a line of this
glass diminishes only 84/592 of light, or about 1/7; that two lines
diminishes 157/592, not quite 1/4 and three glasses of two lines
397/592, i. e. less than 2/3.

As this result is very different from that of M. Bouguer, and as I was
cautious of suspecting the truth of his experiments, I repeated mine
with common glass. For long telescopes water alone can be used; and
it is still to be feared that an inconveniency will subsist, from the
opacity resulting from the quantity of liquor which fills the interval
between the two glasses.

The longer the telescope the greater loss of light will ensue; so that
it appears at first sight that this mode cannot be used, especially
for long telescopes; for following what M. Bouguer says in his Optical
Essay, on the gradation of light, nine feet seven inches sea-water
diminishes the light in a relation of 14 to 5; therefore these long
telescopes, filled with water, cannot be used for observing the sun,
and the stars would not have light enough to be perceived across a
thickness of 20 or 30 feet of intermediate liquor.

Nevertheless, if we consider, that by allowing only an inch, or an
inch and a half, for the bore of an objective of 30 feet, we shall
very distinctly perceive the planets in the common telescopes of this
length; we may suppose that by allowing a greater diameter to the
objective we should augment the quantity of light in the ratio of the
square of this diameter, and, consequently, if an inch before suffices
to see a star distinctly, in a common telescope, three inches bore
would be sufficient to see it distinctly through a thickness of 10 feet
water, and that with a glass of three inches diameter we should easily
see it through a thickness of 20 feet water, and so on. It appears,
therefore, that we might hope to meet with success in constructing
a telescope on these principles; for, by increasing the diameter of
the objective, we partly regain the light lost by the defect of the
transparency of the liquor.

But it appears to me certain that a telescope constructed on this mode
would be very useful for observing the sun; for supposing it even
the length of 100 feet, the light of that luminary would not be too
strong after having traversed this thickness of water, and we should
be enabled to observe its surface easily, and at leisure, without
the need of making use of smoked glasses, or of receiving the image
on pasteboard; an advantage we cannot possibly derive from any other
telescope.

There would require only some trifling difference in the construction
of this solar telescope, if we wanted the whole face of the sun
presented; for supposing it the length of 100 feet, in this case, the
ocular glass must be ten inches diameter; because the sun, taking up
more than half a celestial degree, the image formed by the objective
to its focus at 100 feet, will at least have this length of ten
inches; and to unite it wholly, it will require an ocular glass of this
breadth, to which only twenty inches of focus should be given to render
it as strong as possible. It is necessary that the objective, as well
as the ocular glass, should be ten inches in diameter, in order that
the image of the sun, and the image of the bore of the telescope, be of
an equal size with the focus.

If this telescope, which I propose, should only serve to observe the
sun exactly, it would be of great service; for example, it would be
very curious to be able to discover whether there be any luminous parts
larger than others in the sun; if there be inequalities on its surface;
and of what kind; if the spots float on its surface; or whether they be
fixed there, &c. The brightness of its light prevents us from observing
this luminary with the naked eye, and the different refrangibility of
its rays, renders its image confused when received in the focus of
an objective glass, or on pasteboard, so that the surface of the sun
is less known to us than that of any of the planets. The different
refrangibility of its rays would be but little corrected in this long
telescope filled with water; but if the liquor could, by the addition
of salts, be rendered as dense as glass, it would then be the same
as if there were only one glass to pass through; and it appears to me
that infinitely more advantage would result from making use of these
telescopes filled with water, than from the common telescopes with
smoked glasses.

Whether that would or would not be the fact, this however is certain,
that to observe the sun, a telescope quite different is required from
those that we make use of for the different planets; and it is also
certain, that a particular telescope is necessary for each planet,
proportionate to their intensity of light, that is, to the real
quantity of light with which they appear to be enlightened. In all
telescopes the objectives are required as large, and the ocular glass
as strong, as possible, and, at the same time, the distance of the
focus proportioned to the intensify of the light of each planet. To
do this with the greatest advantage, it is requisite to use only an
objective glass so much the larger, and a focus so much the shorter,
according to the light of the planet. Why has there not hitherto been
made objective glasses of 243 feet diameter? The aberration of the
rays, occasioned by the sphericity of the glasses, is the sole cause
of the confusion, which is as the square of the diameter of the
tube; and it is for this reason that spherical glasses, with a small
bore, are of no value when enlarged; we have more light, but less
distinction and clearness. Nevertheless, broad, spherical glasses are
very good for night telescopes. The English have constructed telescopes
of this nature, and they make use of them very advantageously to see
vessels at a great distance in dark nights But at present, that we
know, in a great measure, how to correct the effects of the different
refrangibility of the rays, it seems, that we should make elliptical
or hyperbolical glasses, which would not produce the alteration caused
by sphericity, and which, consequently, would be three or four times
broader than spherical glasses. There is only this mode of augmenting
to our sight the quantity of light sent to us from the planets, for
we cannot put an additional light on them, as we do on objects which
we observe with the microscope, but must at least employ to the
greatest possible advantage, the quantity of light with which they are
illumined, by receiving it on as great a surface as possible. This
hyperbolical telescope, which would be composed only of one single
large objective glass, and of an ocular one proportionate, would
require matter of the greatest transparency; and we should unite by
this means all the advantages possible, that is, those of the acromatic
to that of the elliptical or hyperbolical telescopes, and we should
profit by all the quantity of light each planet reflects to our sight.
I may be deceived; but what I propose appears to be sufficiently
founded to recommend its execution to persons zealously attached to the
advancement of the sciences.

Employing myself thus on these reveries, some of which may one day
be realized, and in which hope I publish them, I thought of the
Alexandrian mirror, spoken of by some ancient authors, and by means
of which vessels were seen at a great distance on the sea. The most
positive passage which I have met with is the following.

"Alexandria ... in Pharo vero erat speculum e ferro sinico. Per quod
a longe videbantur naves Græcorum advenientes; sed paulo postquam
Islamismus invaluit, scilicet tempore califatus Walidfil: Abdi-I-melec,
Christiani, fraude adhibita illud deleverunt. Abu-l-feda, &c.
Descriptio Ægypti."

Having dwelt for some time on this, I have thought, 1. That such a
mirror was possible to be made. 2. That even without a mirror or
telescope, we might by certain dispositions obtain the same effect,
and see vessels from land, as far, perhaps, as the curvature of the
earth would permit. We have already observed that persons whose sight
was very good, have perceived objects illumined by the sun at more
than 3400 times their diameter, and at the same time we have remarked,
that the intermediate light was of such great hurt to that of distant
objects, that by night a luminous object is perceived at ten, twenty,
and perhaps a hundred times greater distance than during the day. We
know that at the bottom of very deep pits, stars may be seen in the
daytime[H]; why therefore should we not see vessels illumined by the
rays of the sun, by placing one's self at the end of a very long dark
gallery, situated on the seashore, in such a manner as to receive no
other than that of the distant sea, and the vessels which might be on
it? This gallery would be only a horizontal pit, which would have the
same effect with respect to ships as the vertical pit has with respect
to the stars; and it appears to me so simple, that I am astonished it
has never before been thought of and tried. It seems to me, that by
taking the time of the day for our observations when the sun should
be behind the gallery, we might see them from the dark end of it ten
times at least better than in the open light. Now a man on horseback is
easily distinguished at a mile distance, when the rays of the sun shine
on him, and by suppressing the intermediate light which surrounds us,
and darkening our sight, we should see him at least ten times farther;
that is to say, ten miles. Ships, therefore, being much larger, would
be seen as far as the curvature of the earth would permit, without any
other instrument than the naked eye.

[H] Aristotle is, I believe, the first that ever mentioned this
observation.

But a concave mirror, of a great diameter, and of any focus, placed at
the end of a long black tube, would have nearly the same effect as our
great objective glasses of the same diameter and form would have during
the night, and it was probably one of these concave mirrors of polished
steel that was established at the port of Alexandria[I]. If this steel
mirror did really exist, we cannot refuse to the ancients the glory
of the first invention, for this mirror can only be effective by as
much as the light reflected by its surface was collected by another
concave mirror placed at its focus, and in this consists the essence
of the telescope and the merit of its construction. Nevertheless this
does not deprive the great Newton of any glory, who first renewed the
almost-forgotten invention. As the rays of light are by their nature
differently refrangible, he was inclined to think there were no means
of correcting this effect, or, if he had perceived those means, he
judged them so difficult that he chose rather to turn his views another
way, and produce, by means of the reflection of the rays, the great
effects which he could not obtain by their refraction; he, therefore,
constructed his telescope, the reflection of which is infinitely
superior to those that were in common use. The best telescopes are
always dark in comparison of the acromatic, and this obscurity does not
proceed only from the defect of the polish, or the colour of the metal
of mirrors, but from the nature even of light, the rays of which being
differently refrangible are also differently reflexible, although in
much less unequal degrees.

[I] From time immemorial the Chinese, and particularly the Japanese,
have possessed the art of working in steel both in large and small
bodies; and hence I have thought that the words _e ferro sinico_ in the
preceding quotation should be understood as applying to polished steel.

It still remains, therefore, to bring the telescope to perfection, and
to find the manner of compensating this different reflexibility, as we
have discovered that of compensating the different refrangibility.

After all, I imagine that it will be well perceived that a very good
day-glass may be made, without using either glasses or mirrors, and
simply by suppressing the surrounding light, by means of a tube 150
or 250 feet long, and by placing ourselves in an obscure place. The
brighter the day is, the greater will be the effect. I am persuaded
that we should be able to see at 15, and perhaps 20 miles distance. The
only difference between this long tube, and the dark gallery, which
I have spoken of, is, that the field, or the space seen, would be
smaller, and precisely in the ratio of the square of the bore of the
tube to that of the gallery.




OBSERVATIONS AND EXPERIMENTS ON TREES AND OTHER VEGETABLES.


The physical study of Vegetables is one of those sciences which
require a multiplicity of observations and experiments beyond the
capacity of one man, and must consequently be a work of time; even the
observations themselves are seldom of much value till they have been
repeatedly made, and compared in different places and seasons, and by
different persons of similar ideas. It was for this purpose that Buffon
united with M. Du Hamel, to labour, in concert for the illustration
of a number of phenomena, which appeared difficult to explain, in
the vegetable kingdom, and from the knowledge of which may result an
infinity of useful matters in the practice of agriculture.

The frost is sometimes so intense during winter, that it destroys
almost all vegetables, and the scarcity in the year 1709 was a
melancholy proof of its cruel effects. Seeds, and some kinds of
trees, entirely perished, while others, as olives, and almost all
fruit-trees, shared a milder fate, shooting forth their leaves, their
roots not having been hurt; and many large trees, which were more
vigorous, shot forth every branch in spring, and did not appear to have
suffered any material injury. We shall, nevertheless, remark on the
real and irreparable damage this winter occasioned them.

Frost, which can deprive us of the most necessary articles of life,
destroys many kinds of useful trees, and which scarcely ever leaves
one insensible of its rigour, is certainly one of the most formidable
misfortunes of human nature; we have therefore every reason to dread
intense frosts, which might reduce us to the last extremities if their
severities were frequent; but fortunately we can quote only two or
three winters which have produced so great and general a calamity as
that in 1709.

The greatest spring frosts, although they damage the grain, and
principally barley, when it is but just eared, never occasion great
scarcities. They do not affect the trunks or branches of trees, but
they totally destroy their productions, deprive us of the harvest of
the vines and orchards, and by the suppression of new buds cause a
considerable damage to forests.

Although there are some examples of winter frosts having reduced us to
a scarcity of bread, and deprived us of vegetables, the damage which
spring frosts occasion becomes still more important, because they
afflict us more frequently, and their effects are felt almost every
year.

To consider frost even very superficially, we must perceive that the
effects produced by the sharp frosts of winter are very different from
what are occasioned by those in spring, since the one attacks the body
and most solid parts of trees, whereas the other simply destroys their
productions, and opposes their growth; at the same time they act under
quite different circumstances; and it is not always the ground in which
the winter frosts produce the greatest disorders, as that generally
suffers most from those in the spring frosts.

It was from a great number of observations that we have been able to
make this distinction on the effects of frost, and which we hope will
not be simply curious, but prove of utility, and be profitable to
agriculture; and should they not wholly enable us to escape from the
evils occasioned by frost, they will afford us a means to guard against
them. We shall, therefore, enter upon the detail, beginning with that
which regards the sharp frosts of winter: of these, however, we cannot
reason with so great a certainty as on those of spring, because, as
we have already observed, we are seldom subjected to their tragical
effects.

Most trees during winter being deprived of blossoms, fruits, and
leaves, have generally their buds hardened so as to be capable of
supporting very sharp frosts, unless the preceding summer was cool, in
which case the buds not being arrived to that degree of maturity, which
gardeners call _aoutes_[J], they are not in a state of resisting the
moderate frosts of winter; but this seldom happens, the buds commonly
ripening before winter, and the trees endure the rigour of that season
without being damaged, unless excessive cold weather ensue, joined to
the circumstances hereafter mentioned.

[J] Ripened or filled with sap.

We have, nevertheless, met with many trees in forests with considerable
defects, which have certainly been produced by the sharp frosts, and
which will never be effaced.

These defects are, 1st, chaps or chinks, which follow the direction
of the fibres. 2. A portion of dead wood included in the good; and
lastly, the double sap, which is an entire crown of imperfect wood. We
must dwell a little on these defects to trace the causes whence they
proceed.

The sappy part of trees is, as is well known, a crown or circle of
white or imperfect wood of a greater or less thickness, and which in
almost all trees is easily distinguished from the sound wood, called
the _heart_, by the difference of its colour and hardness; it is found
immediately under the bark, and surrounds the perfect wood, which in
sound trees is nearly of the same colour, from the circumference to the
centre. But in those we now speak of, the perfect wood was separated by
another circle of white wood, so that on cutting the trunks of them we
saw alternately circles of sap and perfect wood, and afterwards a clump
of the latter, which was more or less considerable, according to the
different soils and situations; in strong and forest earth it is more
scarce than in glades and light earth.

By the mere inspection of these cinctures of white wood, which we
in future shall term _false sap_, we could perceive it to be of bad
quality; nevertheless, to be certain of it, we had several planks sawed
two feet in length, by nine to ten inches square, and having the like
made from the true sap, we had both loaded in the middle, and those of
the false sap always broke under a less weight than those of the true,
though the strength of the true sap is very trivial in comparison with
that of formed wood.

We afterwards took several pieces of these two kinds of sap, and
weighed them both in the air and water, by which we discovered that
the specific weight of the natural sap was always greater than that of
the false. We then made a like experiment with the wood of the centre
of the same trees, to compare it with that of the cincture which is
found between these two saps, and we discovered that the difference
was nearly the same as is usual between the weight of the wood of the
centre of all trees and that of the circumference; thus all that is
become perfect wood in these defective trees is found nearly in the
common order. But it is not the same with respect to the false sap,
for, as these experiments prove, it is weaker, softer, and lighter
than the true sap, although formed 20, nay 25 years before, which we
discovered to be the fact, by counting the annual circles, as well of
the sap as of the wood which covered it; and this observation, which
we have repeated on a number of trees, incontestibly proves that these
defects had been caused by the hard frost of 1709, notwithstanding
that the number of some of their coats was less than the years which
had passed since that period; and at which we must not be surprised,
not only because we can never, by the number of ligneous coats, find
the age of trees within three or four years, but also because the first
ligneous coats, formed after that frost, were so thin and confined,
that we cannot very exactly distinguish them.

It is also certain, that it was the portion of the trees that were in
sap in the hard frost of 1709, which instead of coming to perfection,
and converting itself into wood, became more faulty. Besides, it is
more natural to suppose, that the faulty part must suffer more from
sharp frosts than sound wood: because it is not only at the external
part of the tree, and therefore more exposed to the weather, but also
because the fibres are more tender and delicate than the wood. All this
at first appears to wear but little difficulty, yet the objections
related in the history of the Academy of Sciences, 1710, might be here
adduced; by these objections it appears that in 1709, the young trees
endured the hard frost much better than old. But as these facts are
certain, there must be some difference between the organic parts, the
vessels, the fibres, &c. of the sappy part of the old trees and that
of the young; they perhaps will be more supple, so that a power which
will be capable of causing the one to break, will only dilate the other.

But as these are conjectures with which the mind remains but little
satisfied, we shall pass slightly over them, and content ourselves with
the particulars we have well observed. That this sappy part suffered
greatly from the frost is an incontestible fact, but has it been
entirely disorganized? This might happen without the death of the tree
ensuing, provided the bark remained sound; and even vegetation might
continue. Willows and limes frequently subsist only by their bark,
and the same thing has been seen at the nursery of Roule in an orange
tree. But we do not think that the false sap is dead, because it always
appeared to us in quite a different state from the sap found in trees,
which had a portion of dead wood included in the sound; besides, if it
had been disorganized, as it extends over the whole circumference, it
would have interrupted the lateral motion of the sap, and the wood of
the centre, not being able to vegetate, would have also perished and
altered, which was not the case, and which I could confirm by a number
of experiments; however, it is not easily conceivable how this sappy
part of wood has been changed so far as not to become wood, and that
far from being dead, it was even in a state of supplying the ligneous
coats with sap, which are formed from above in a state of perfection,
and which may be compared to the wood of trees that have suffered no
accident. This must nevertheless have been done by the hard winter,
which caused an incurable malady to this part of the tree; for if it
were dead, as well as the bark which cloathed it, there can be no
doubt that the tree would have entirely perished, which happened in
1709 to many trees whose bark was detached from them, and which by the
remaining sap in their trunk, shot forth their buds in spring, but
died through weakness before autumn, for want of receiving sufficient
nutriment to subsist on.

We have met with some of these false sappy part of trees which are
thicker on one side than the other, and which surprisingly agrees with
the most general state of the sap. We have also seen others very thin,
so that apparently there were only the outer coats injured. These were
not all of the same colour, had not undergone an equal alteration, nor
were equally affected, which agrees with what we have before advanced.
At length, we dug at the foot of some of these trees, to see if the
defect existed also in the roots, but we found them sound: therefore,
it is probable that the earth which covered them had repaired the
injury done by the frost.

Here then we see one of the most dreadful effects of winter frosts,
which though locked up within the tree, is not less to be feared, since
it renders the trees attacked by them almost useless; but besides this,
it is very difficult to meet with trees totally exempt from these
injuries; and indeed all those whose wood is not of a deeper colour at
the centre, growing somewhat lighter towards the sap, may be suspected
of having some defects, and ought not to be made use of in any matter
of consequence.

By horizontally sawing the bottom of trees, we sometimes perceive a
piece of dead sap or dried bark, entirely covered by the live wood:
this dead sap occupies nearly half of the circumference in the parts
of the trunk where it is found: it is sometimes browner than good
wood, and at others almost white. From the depth also where this sap
is found in the trunk, it appears to have been occasioned by the sharp
frost in winter, by which a portion of the sap and bark perished, and
was afterwards covered by the new wood; for this sap is almost always
found exposed to the south, where the sun melting the ice, a humidity
results, which again freezes soon after the sun disappears, and that
forms a true ice, which is well known to cause a considerable prejudice
to trees. This defect does not always appear throughout the whole
length of the trunk, for we have seen many square pieces which seemed
perfectly exempt from all defects, nor were the injuries of the frost
discovered until they were slit into planks. It is, nevertheless easily
to be conceived, how such a disorder, in their internal parts, must
diminish their strength, and assist their perishing.

In forests, or woods, we meet with trees which strong winter frosts
have split according to the direction of their fibres; these are marked
with a ridge formed by the cicatrice that covers the cracks, but which
remain within the trees without uniting again, because a re-union is
never formed in the ligneous fibres when they have been divided or
broken; nor can it be doubted, that the sap, which increases in volume
when it freezes, as all liquors do, may produce many of these cracks.
But we also suppose that there are some which are independent of the
frost, and which have been occasioned by a too great abundance of sap.

Be this as it may, the fact is, we have found defects of this kind in
all soils, and in all expositions, but most frequently in wet ground
and in northern and western expositions; the latter may perhaps proceed
in cases when the cold is more intense, in such expositions; and in the
other, from the trees which are in marshy grounds, having the tissue of
their ligneous fibres weaker, and because their sap is more abundant
and aqueous than in dry land; which may be the cause that the effect
of the rarefaction of liquors by the pores is more perceptible, and
more in a state of diminishing the ligneous fibres, as they bring less
resistance thereto.

This reasoning seems to be confirmed by another observation; namely,
that resinous trees, as the fir, are seldom injured by the sharp frosts
of winter, evidently from their sap being more resinous: for we know
that oils do not perfectly freeze, and that instead of augmenting in
volume, like water, in frosty weather, they diminish when they congeal.

Dr. Hales says in his _Vegetable Statics_, _p._ 16, that the plants
which transpire the least, are those which best resist the winter;
because they have need of only a small quantity of nutriment to
preserve themselves. He says, likewise in the same part, that the
plants, which preserve their leaves during winter, are those which
transpire the least; nevertheless, we know that the orange tree, the
myrtle, and still more the jessamine of Arabia, &c. are very sensible
to frost, although these trees preserve their leaves during winter; we
must, therefore, have recourse to another cause to explain why certain
trees which do not shed their leaves in winter, so well support the
sharpest frosts.

We have sawed many trees which were attacked with this malady, and
have almost always found, under the prominent cicatrice, a deposit of
sap or rotten wood, and they are easily distinguished from what are
called in the forest terms, sinks or gutters, because the defects which
proceed from an alteration of the ligneous fibres, which is internally
produced, occasion no cicatrice to change the external form of the
trees, whereas the chinks produced by frosts, which proceed from a
cleft afterwards covered by a cicatrice, make a ridge or eminence in
the form of a cord, which announces the internal defect.

The sharp winter frosts produce, without doubt, many other injuries
to trees, and we have remarked many defects, which we might attribute
to them with great probability; but, as we have not been able to
verify the fact, we shall pass on to the effects of the advantages
and disadvantages of different expositions with respect to frost; for
this question is too interesting to agriculture not to attempt its
elucidation, especially as various authors have supported an opposition
of sentiment more capable of breeding doubts than increasing our
knowledge. Some have insisted that the frost is felt more strongly
at the northern exposition, while others assert it is more sensible
to the south or west, and all these opinions are founded on a single
observation. We nevertheless perceive what has caused this diversity of
opinion, and we are therefore enabled to reconcile them. But, before we
relate the observations and experiments which have led us thereto, it
is but just we should give a more exact idea of the question.

It is not doubted that the greatest cold proceeds from the north, for
that is in the shade of the sun, which alone, in sharp frosts, tempers
the rigour of the cold; besides, a situation to the north, is exposed
to the north-east, and north-west winds, which are clearly the most
intense, whether we judge from the effects which those winds produce,
or from the liquor of the thermometers, whose decision is much more
certain. It may also be observed along the espaliers, that the earth is
often frozen and hardened all the day towards the north, while it may
be worked upon towards the south. Moreover when a strong frost succeeds
in the night, it is evident, that it must be much colder in the part
where it is already formed, than in that where the earth is warmed
by the sun; this is also the reason why, even in hot countries, we
find snow in the northern exposition, on the back of lofty mountains:
besides, the liquor of the thermometer is always lower at the northern
exposition, than in that of the south; therefore, it is incontestible,
that it is colder there, and freezes stronger.

It is therefore certain, that all the accidents which depend solely on
the power of the frost, will be found more frequently at the northern
exposition than elsewhere. But yet it is not always the great power
of the frost which injures trees, for there are particular accidents,
which cause a moderate frost to do them more prejudice than the much
sharper, when they happen in favourable circumstances. Of this we
have already given an example in speaking of that part of dead wood
included in the good, which is produced by the hoar frost, and is found
most frequently in the expositions to the south; and it is also to be
observed, that great part of the disorders produced in the winter of
1709, are to be attributed to a false thaw, which was followed by
a frost still sharper than what had preceded; but the observations
which we have made on the effects of spring frosts supply us with
many similar examples, which incontestibly prove it is not in the
expositions where it freezes the strongest, that the frost commits the
greatest injuries to vegetables. Not to dwell upon assertions, we shall
proceed to a detail of facts, which will render these general positions
clear and apparent.

In the winter 1734 we caused a coppice in my wood, near Montbard in
Burgundy, to be cut, which measured one hundred and fifty-four feet,
situated in a dry place, on a flat ground, surrounded on all sides
with cultivated land. In this wood we left many small square pieces
without felling them, and in a manner that each equally faced east,
west, north and south. After having well cleared the part that was
cut, we observed carefully in spring the growth of the young buds; the
renewed tops on the 20th of April, had sensibly shot out in the parts
exposed to the south, and which consequently were sheltered from the
north by the tufted tops; these were the first buds that appeared, and
were the most vigorous; those exposed to the east appeared next; then
those of the west, and lastly those of the northern exposition. On
the 28th of April the frost was very sharp in the morning accompanied
by a north wind; the sky was clear, and the air very dry, and in which
manner it continued for three days. At the end of which I went to see
in what state the buds were about the clumps, and found them absolutely
blackened in all the parts exposed to the south and sheltered from the
north wind, whereas those which were exposed to the cold north wind,
which still blowed, were only slightly injured; and with respect to
the eastern and western expositions, they were that day nearly alike
injured.

The 14th, 15th, and 22d of May, it froze pretty sharply, accompanied
by the north and north-west winds, and I then likewise observed that
all those sheltered from the wind were very much injured, but that
all those which were exposed thereto had suffered but very little.
This experiment appeared decisive, and showed that although it froze
most strong in parts exposed to the north wind, yet the frost in that
situation did the least injury to vegetables.

This circumstance is certainly opposed to common prejudice; but it is
not less the fact, and is even easy to be explained; for this purpose,
it is sufficient to pay attention to circumstances in which frost
acts, and we shall discover that humidity is the principal cause of
its effects, so that all which occasions humidify renders, at the
same time, the frost dangerous to vegetables, and all that dissipates
humidity, even if it should be done by increasing the cold (for every
thing that dries diminishes the disasters of a frost) acts towards
their preservation.

We have often remarked, that in low places, where mists and fogs
reign, frost is felt more sharply, and oftener than elsewhere. For
instance, in autumn and spring we have seen delicate plants frozen
in a kitchen-garden, in a low situation, while the like plants were
preserved sound in another kitchen-garden situated on an eminence.
So, likewise, in vallies and low forests the wood is never of a
beautiful vein, nor of good quality, although the vallies are often
by much the best soil. The coppice wood is never good in low places,
although it shoots forth there later than upon high places, and which
is occasioned by a freshness that is always concentered therein. When
I walked at night in the wood I felt almost as much heat on eminences
as in the open plains, but in the vallies I experienced a sharp and
uncomfortable cold. Though the trees shoot out the latest in those
parts, yet the shoots are still injured by the frost, which spoiling
the principal buds obliges the trees to shoot forth lateral branches,
and thus prevents their ever becoming straight and handsome trees
fit for service. What we have just advanced must not be understood
only of deep vallies, which are liable to those inconveniencies from
northern expositions, or those inclosed on the southern side in the
form of an alley, in which it often freezes the whole year, but also
of the smallest vallies, so that by a little custom we can discover
the bad figure of the shoots from the inclination of the earth; this
I particularly observed on the 28th of April, 1734; on that day the
buds of all the trees, from one year up to six or seven, were frozen in
all the lower places; whereas in the high and uncovered places there
were only the shoots near the earth which were so; the earth was then
very dry, and the humidity of the air did not appear to have greatly
contributed to this injury. Neither vines, nor the trees of the plain,
are subject to frost, which might lead us to suppose they are less
delicate than the oak; but we think this must be attributed to the
humidity, which is always greater in the woods than in the rest of the
plains, for we have observed that oaks are often very much injured
from frosts in forests, while those which are in the plains are not
hurt in the least.

Large timbers, even on eminences, may cause the young trees near them
to be in the same state as if at the bottom of a valley. We have also
remarked, that the young wood near large trees is often more injured
by the frost than in parts remote from them, as in the midst of such
woods, where a great number of branches are left, it is felt with more
force than in those which are open. Now all these disorders are most
considerable in such places, for as the wind and sun cannot dissipate
the transpiration of the earth and plants, there remains a considerable
humidity, which causes a very great prejudice to plants.

We have also remarked, that the frost is never more to be dreaded, with
respect to the vine flowers, buds of trees, &c. than when it succeeds
mists, or even rain, however slight, for they are all capable of
enduring a very considerable degree of cold without being damaged, when
it has not rained for some time, and the earth is dry.

Frosts likewise act more powerfully in places newly cultivated than
in others, because the vapours, which continually rise from the
earth, transpire more freely and abundantly from that which is newly
cultivated. To this reason we must, however, subjoin the fact, that
plants, newly set, shoot forth more vigorously than others, which
renders them more sensible and liable to the effects of frost. So also
in light and sandy soil the frost does more injury than in strong land,
even though of equal dryness, because more exhalations escape from the
first kind of earths than from the latter; and if a vine newly dunged
is most subject to the frost, it arises from the humidity which escapes
from it. A furrow of vine which lies along a field of sainfoin, peas,
&c. is often all destroyed by the frost, while the rest of the vine
is quite healthy, and this is undoubtedly, to be attributed to the
transpiration of the sainfoin, or other plants, which bring a humidity
on the shoots of the vine. In the vine also, the branches that are
strong and cut are always less injured than the stock; especially when
not attached to the props, as they are then agitated by the wind which
dries them.

The same thing is remarked of timber, and I have seen in copses all the
buds entirely destroyed by the frost, while the upper shoots had not
received the least damage; indeed it always appeared that the frost did
most injury nearest to the earth, commonly within one or two feet,
insomuch that it must be very violent to destroy the buds higher than
four.

All these observations, which may be regarded as very constant, agree
to prove that in general it is not the sharpest frosts which do the
greatest injury to plants, but that they are affected in proportion as
they are loaded with humidity, which perfectly explains why the frost
causes so many disorders in the southern exposition, although it should
be less cold than that of the north, and likewise why the frost causes
more injury to the northern exposition, when after a rain proceeding
from a westerly wind the wind veers to the north towards sun-set, as
often happens in spring, or when, by an easterly wind, a cold moist air
arises before sun-rise, which, however, is not so common.

There are likewise circumstances where the frost does most injury
to the eastern exposition; but as we have many observations on that
subject, we shall first relate those which we made in the spring frost
in 1736, which occasioned so much damage. It having been very dry
previously, it froze for a long time before it injured the vines; but
it was not so in the forests, apparently because they contained more
humidity. In Burgundy it was the same as in the forest of Orleans,
the underwood was injured very early. At last the frost increased so
greatly that all the vines were destroyed, notwithstanding the dryness
still continued; but instead of this frost doing much damage under the
shelter of the wind, those parts which were sheltered were the only
ones preserved, insomuch, that in many closes surrounded by walls the
stocks along the southern exposition were very green, while all the
rest remained dry; and in two quarters the vines were saved, the one by
being sheltered from the north by a nursery of ash-trees, and the other
because the vineyard was stocked with a number of fruit-trees.

But this effect is very rare, and this happened only because the season
had been dry, and because the vines had resisted the weather till the
plants had became so strong, from the time of the year, that the frost
could not injure them, independently of the external humidity and other
particular circumstances.

But there are other causes to be assigned why frost produces injury
more frequently to the east than to the west, and which are drawn from
the following observations:

A sharp frost causes no prejudice to plants when it goes off before the
sun comes upon them: let it freeze at night, if the morning be cloudy,
or a slight rain fall, or, in a word, if by any cause whatever the ice
melt gently, and independently of the action of the sun, it seldom does
any injury; and we have very often saved very delicate plants, which
had by chance remained exposed to the frosts, by returning them into
the green-house before sun-rise, or by simply covering them before the
sun had shone upon them.

One time in particular a very sharp frost happened in autumn while our
orange-trees were out of the green-house, and as it rained part of
the night they were all covered with icicles: but this accident was
prevented from doing any injury by covering them with cloths before the
sun rose, so that there was only the young fruit and the most tender
shoots injured, and we are persuaded they would all have been saved if
the covering had been thicker.

Another time our _geraniums_, and many other plants which cannot bear
the frost, were out, when suddenly the wind, which was south-west,
veered to the north, and became so cold that the rain, which fell
abundantly, was frozen, and in almost a moment all that were exposed
to the air were covered with ice; we thought, therefore, that all our
plants were irrecoverably destroyed; nevertheless we had them carried
to the furthermost part of the green-house, shut up the windows, and by
that means they sustained but little damage.

This kind of precaution is always observed with regard to animals; when
they are stricken with cold, or have a limb frozen, great care is taken
not to expose them hastily to heat, but they are rubbed with snow,
dipped in water, or burned in dung; in one word, the greatest attention
is paid that they shall gradually be brought to warmth. It is almost
certain, with respect to fruit which may be frozen, that if thawed with
precipitation it invariably perishes, whereas it suffers but little if
thawed gradually.

In order to explain how the sun produces so many disorders in frozen
plants, some have imagined that the ice, by melting, is reduced into
small spherical drops of water, which form so many small burning
mirrors when the sun shines upon them. But however small the form of
a mirror may be, it can only produce heat at a distance, and can have
no effect on a body it touches; besides, the side of the drop of water
which is on the leaf of a plant is flat, which removes its focus to a
greater distance. In short, if these drops of water could produce this
effect why should not the dew-drops, which are also spherical, produce
the same? Perhaps, it may be thought that the most spirituous and
volatile parts of the sap melting the first, they evaporate before the
rest are in a state of moving in the vessels of the plant, which might
decompose the sap.

But in general it may be said, that the frost increasing the volume
of fluids, dilates the vessels of plants, and that the thaw cannot be
performed without the parts which compose the frozen fluid enter into
motion. This change may be made with sufficient gentleness not to break
the most delicate vessels of plants, which will by degrees return to
their natural tone, and then the plants will not suffer any injury;
but, if it be done with precipitation, these vessels will not be able
to resume their natural tone so soon after having suffered a violent
extension, the liquors will evaporate and the plant remain dry.

Although we might conclude with these conjectures, with which I am not
myself perfectly satisfied, yet the following data are irrevocably
constant.

1. That it seldom happens with regard to fruit, either in spring or
winter, that the plants are injured simply by the force of the frost
and independently of any particular circumstances, and when it does,
it is at the northern exposition that plants meet with the greatest
injury.

2. In frosty weather, which lasts several days, the heat of the sun
melts the ice in some places for a few hours; for it often freezes
again before sun-set, which forms an ice very prejudicial to plants,
and it is observable that the southern exposition is more subject to
this inconvenience than all the rest.

3. It has been observed, that spring frosts principally disorder those
plants where there is humidity, the soils which transpire much, the
bottoms of vallies, and in general all places which cannot be dried by
the wind and sun are the most injured.

In short, if, in spring, the sun which shines on frozen plants occasion
a more considerable damage to them, it is clear that it will be the
eastern exposition, and those next the south which will suffer most.

But it may be said, if this be the case, we must no longer plant to
the southern exposition _en a-dos_ (which are slopes, or borders of
earth, thrown up in kitchen gardens or along espaliers) gilliflowers,
cabbages, winter lettuces, green peas, and such other delicate plants
as we would have stand the winter, and preserve for an early crop in
spring; and that it is to the northern exposition alone that we must
in future plant peach and other delicate trees. It is proper to destroy
these objections, and shew that they are false consequences of what we
have advanced.

Different objects are proposed when we set plants to pass through
the winter in shelters exposed to the south, and sometimes it is to
expedite vegetation: it is, for example, with this intention, that
along espaliers we plant ranges of lettuces, which for that reason are
termed _winter-lettuces_; these will tolerably well resist the frost
in whatever part we plant them, but are always most forward in this
exposition; at other times, it is to preserve them from the rigour of
this season, with an intention of replanting them early in the spring.
This practice is also followed in winter cabbages, which are sown in
this season along an espalier border. These kind of cabbages, like
brocoli, are tender and cannot endure the frost, and would often perish
in these shelters, if care were not taken to cover them during the
sharp frosts with straw or dung supported on frames.

To forward the vegetation of some plants which will not bear the frost,
as green peas, &c. it is usual for that purpose to plant them on
borders exposed to the south, besides which, they are defended from
sharp frosts when the weather requires it.

It is well known, without being compelled to dwell any longer on this
point, that the southern exposition is more proper than all the rest
to accelerate vegetation, and we have shewn that this is also what is
principally proposed when some plants are set in that exposition to
pass through the winter, since, in addition, we are also obliged to
make use of coverings to guard those plants which are very delicate
from the frost. But we must add, that if there be some circumstances
wherein the frost causes more disorders to the southern than to other
expositions, there are also many cases which are favourable to this
exposition: for example, in winter, when there is any thing to fear
from the ice, it frequently happens that the heat of the sun, increased
by the reflection of the wall, has sufficient force to dissipate all
the humidity, and then the plants are almost perfectly secure against
the cold. Besides, dry frosts often happen, which unceasingly act
towards the north, and which are scarcely ever felt towards the south.
In spring, likewise, we perceive that after a rain which proceeds from
the south-west, or south-east, if the wind change to the north, the
southern espalier being under the shelter of the wind, will suffer
more than the rest; but these cases are very rare, and most often it is
after rains, which come from the north-east or north-west that the wind
changes to the north, and then the southern espalier having been under
shelter from the rain by the wall, the plants there will have less
to suffer than the rest, not only because it will have received less
rain, but also because there is always less cold here, than in other
expositions. It is likewise to be observed that as the sun dries much
earth along the espaliers which are to the south, the earth transpires
there less than elsewhere.

It is well known that what we have just advanced must be considered as
applying also to peach and apricot trees, which it is customary to put
in this exposition and in that of the east. We shall only add, that
it is not unusual to see peach trees frozen in the east and southern
expositions, while those are not so which stand in the west or north;
but notwithstanding this we can never rely on having many, nor good
peaches in this last exposition, for great quantities of blossoms fall
off entirely without setting; others, after having set fall from the
trees, and those which remain with difficulty arrive to maturity. I
have an espalier of peach-trees in a western exposition, a little
declining to the north, which scarcely ever produce any fruit, although
the trees are handsomer than those to the southern and northern. We
cannot, therefore, avoid the inconveniences of the frost with respect
to the southern exposition without feeling others that are worse.

All delicate trees, as fig, laurel, &c. must be set to the south, and
great care taken to cover them; it is only requisite to remark that dry
dung is preferable for this purpose to straw, because the latter not
only does not so exactly cover them, but also from its always retaining
some grain which attracts moles and rats, who sometimes eat the bark of
trees to quench their thirst in frosty weather, when they can meet with
no water to drink, nor herb to feed upon; and however singular this may
appear, it is a circumstance which has happened to us several times;
but when dung is made use of it must be dry, without which it will heat
and make the young branches grow mouldy.

All these precautions are, nevertheless, very inferior to the espaliers
in niches, as in that manner plants are sheltered from all winds,
except the south, which cannot hurt them; the sun, which warms these
places during the day, prevents the cold from being so violent during
the night; and over these defended places we may put a slight covering
with great facility, which will hold the plants there in a state of
dryness, infinitely proper to prevent all the accidents which the
spring frosts and ice might produce; and most plants will not suffer
from being deprived of their external humidity, because they scarcely
transpire in the winter, or in the beginning of spring, so that the
humidity of the air is sufficient for their supply.

But since the dew renders plants so susceptible of the spring frost,
might we not hope, that from the researches of Messrs. Musschenbroeck
and Fay, some inferences may be deduced which may turn to the advantage
of agriculture? for since there are some bodies which seem to attract
dew, while others evidently repel it, if we could paint, plaster, or
wash the walls with some matter which would have the latter effect,
it is certain we should have room to expect a more fortunate success
than from the precaution taken to place a plank in form of a roof
over the espaliers, which cannot prevent the abundance of dew from
resting on trees, since Fay has proved that it very often does not
fall perpendicularly like rain, but floats in the air, and attaches
itself to those bodies it encounters; so that frequently as much dew
is amassed under a roof as in places entirely open. It would be easy
for us to recapitulate all our observations, and continue to deduce
useful consequences, but what we have said must be sufficient to shew
the necessity of rooting up all trees which prevent the wind from
dissipating mists.

Since by cultivating the earth we cause more exhalations to issue,
great attention should be paid not to cultivate them in critical times.

We must expressly declare against sowing kitchen-plants on
vine-furrows, as by their transpiration they hurt the vine.

Props should be put to the vines as late as possible. The hedges, which
border them on the north side, should be kept lower than the rest. It
is preferable to improve vines with mould rather than dung. And in
choosing a soil we should avoid those which are in bottoms and grounds
which transpire much.

A part of these precautions may be also usefully employed for
fruit-trees; with respect, for example, to plants which gardeners are
forward to put at the feet of their bushes and along their espaliers.

If there are some parts high and others low in a garden, we should pay
attention to sow spring and delicate plants on elevated parts, at least
if we do not design to cover them with glasses, &c. but in cases where
humidity cannot hurt them it might be often advantageous to choose low
places, where they might be sheltered from the north and north-west
winds.

We may also profit from what has been said to the advantage of forests,
for if we mean to make a reserve of any of the trees, it should never
be in parts where the frost is severe; and in planting we should pay
attention to put in vallies those trees which can endure the frost
better than the oak.

When any considerable fall of timber is made we should make them in
roads, beginning always on the north side, in order that the wind,
which generally blows in frosty weather, may dissipate that humidity
which is so prejudicial to the underwood.

There might be also many other useful consequences drawn from our
observations; but we shall content ourselves with having briefly
adverted to some, because the ingenious man may supply what we have
omitted by paying a little attention to the observations we have
mentioned. We are well convinced there are a great number of further
experiments to be made on this matter; and perhaps even those which we
have related will engage some persons to work on the same subject, and
from our hints general and useful advantages may be derived.




ON THE TEMPERATURE OF THE PLANETS.


Man newly created, and even the ignorant man at this day beholds the
extent and nature of the universe only by the simple organ of light: to
him the earth is but a solid body, whose volume is unbounded, and whose
extent is without limits, of which he can only survey small superficial
spaces: while the sun and planets seem to be luminous points, of
which the sun and moon appear to be the only objects worthy regard
in the immensity of the heavens. To this false idea on the extent of
nature and the proportions of the universe is joined the still more
disproportionate sentiment of superiority. Man, by comparing himself
with other terrestrial beings, feels that he ranks the first, and hence
he presumes that all was made for him; that the earth was created only
to serve for his habitation, and the heavens for a spectacle; and
in short the whole universe ought to yield to his necessities, and
even his pleasures. But in proportion as he makes use of that divine
light, which alone ennobles his being; in proportion as he obtains
instruction, he is forced to abate his pretensions; he finds himself
lessened in proportion as the universe increases in his ideas, and
it becomes demonstrable to him, that the earth, which forms all his
domain, and on which unfortunately he cannot subsist without trouble
and sorrow, is as small with respect to the universe, as he is with
respect to the Creator. In short, from study and application, he finds
that there does not remain a possible doubt, that this earth, large
and extensive as it may seem to him, is but a moderate sized planet, a
small mass of matter, which, with others, has a regular course round
the sun: for as it appears our globe is at the distance of at least 33
millions of leagues, and the planet Saturn at 313 millions, the natural
conclusion is, that the extent of the sun's empire is a sphere, whose
diameter is 627 millions of leagues, and that the earth, relative to
this space, is not more than a grain of sand to the volume of the globe.

However, the planet Saturn, although the furthest from the sun, is not
by any means near the confines of his empire: his limits extend much
further, since comets pass over spaces beyond that distance, as may be
estimated by the time of their revolutions: a comet which like that
of the year 1680 revolves round the sun in 575 years must be 15 times
more remote from him than Saturn; for the great axis of its orbit is
138 times greater than the distance from the earth to the sun. Hence we
must still augment the extent of the solar power 15 times the distance
from the sun to Saturn, so that all the space in which the planets are
included is only a small province of his domain, whose bounds should be
placed at least 138 times his distance from the earth.

What immensity of space! What quantity of matter! For independently
of the planets, there is a probability of the existence of 400 or 500
comets, perhaps larger than the earth, which run over the different
regions of this vast sphere of which the terrestrial globe only
constituting a part, a unity on 191,201,612,985,514,272,000, a quantity
represented by numbers, which imagination cannot attain or comprehend.

Nevertheless, this enormous extent, this vast sphere, is yet only a
very small space in the immensity of the heavens; each fixed star is
a sun, a center of a sphere equally as extensive; and as we reckon
more than 2000 of these fixed stars perceived by the naked eye, and as
with telescopes we can discover so much the greater number as these
instruments are more powerful; the extent of the universe appears to
be without bounds and the solar system forms only a province of the
universal empire of the Creator; an infinite empire like himself.

Sirius, the most brilliant fixed star, and which for that reason may
be regarded as the nearest sun to our's, affords to our sight only a
second of annual parrallax on the whole diameter of the earth's orbit,
and is therefore at the distance of 6,771,770, millions of leagues
distant from us, that is, 6,767,216 millions of leagues from the limits
of the solar system, such as we have assigned it after the depth to
which the comets immerse. Supposing then, there is an equal space from
Sirius to that which belongs to our sun, we shall perceive that we must
extend the limits of our solar system 742 times more than it is at
present, as far as the aphelion of the comet, whose enormous distance
from the sun is nevertheless only a unit on 742 of the total diameter
of the solar system.

                                                           Leagues.
  Distance from the earth to the Sun                           33,000,000
  Distance from Saturn to the Sun                             313,000,000
  Distance from the aphelion of the Comet to the Sun        4,554,000,000
  Distance from Sirius to the Sun                       6,771,770,000,000
  Distance of Sirius to the point
    of the aphelion of the Comet,
    supposing that in ascending
    from the sun the comet pointed
    directly towards Sirius (a supposition
    which diminishes the distance as much as
    possible)                                           6,767,216,000,000
  One half the distance from Sirius to the
    Sun, or the depth of the solar and sircin
    system                                              3,385,885,000,000
  Extent beyond the limits of the comet's
    aphelion                                            3,331,331,000,000
  Which being divided by the distance of the
    comet's aphelion, gives about                       742-1/2

We can form another idea of our immense distance from Sirius, by
recollecting that the sun's disk forms to our sight an angle of 32
minutes, whereas that of Sirius forms only that of a second; and Sirius
being a sun like ours, which we shall suppose of equal magnitude, since
there is no reason to conceive it larger or smaller, it would appear
to us as large as the sun, if it were but a like distance. Taking
therefore two numbers proportional to the square of 32 minutes, and to
the square of a second, we shall have 3,686,400 for the distance of the
earth to Sirius, and one for its distance to the sun; and as this unit
is equal to 33 millions of leagues, we see how many millions of leagues
Sirius is distant from us, since we must multiply these 33 millions by
3,686,400; and if we divide the space between these two neighbouring
suns, although at so great a distance, we shall see that the comets
might be removed to a distance 1,800,000 times greater than that of
the earth to the sun without quitting the limits of the solar universe,
and without being subjected to other laws than that of our sun, and
hence it may be concluded that the solar system for its diameter has
an extent, which, although prodigious, nevertheless, forms only a very
small portion of the heavens; and we must infer a truth therefrom but
little known, namely, that from the sun, the earth and all the other
planets, the sky must appear the same.

When in a serene and clear night we contemplate all those stars with
which the celestial vault is illuminated, it might be imagined that
by being conveyed into another planet more remote from the sun, we
should see these glittering stars larger, and emitting a brighter
light, since we should be so much nearer to them. Nevertheless, the
calculation we have just made demonstrates that if we were placed in
Saturn, which is 300 millions of leagues nearer Sirius, it would appear
only an 194,021st part bigger, an augmentation absolutely insensible;
from which it must be concluded, that the heaven, with respect to all
the planets, has the same aspect as it has to the earth. Therefore if
even there should exist comets whose periods of revolution might be
double, or treble the period of 575 years, the longest known to us; if
even the comets in consequence thereof, immerse at a depth ten times
greater, there would still be a space 74 or 75 times deeper, to reach
the last confines, as well of the solar system, as of the sirian; so
that by allowing Sirius as much magnitude as our sun has, and supposing
in his system as many or more cometary bodies than there are comets
existing in the solar, Sirius will govern them as the sun governs his,
and there will remain an immense interval between the confines of the
two empires; an interval which appears to be no more than a desart in
the vast space, and which must give a suspicion that cometary bodies
do exist, whose periods are longer, and which are to a much greater
distance than we can determine by our actual knowledge. Sirius may
also be a sun much larger and more powerful than ours; and if that is
the case, it must throw the borders of his domain so much the further
back by approaching them to us, and at the same time retrench the
circumference of the sun.

I cannot avoid presuming, that in this great number of fixed stars,
which are all so many suns, there are some greater and others smaller
than ours; others more or less luminous, some nearer, which are
represented to us by those stars called by astronomers, _stars of the
first magnitude_, and many others more remote, which for that reason
appear to us smaller. The stars called _nebulous_ seem to want light
and fire, and to be only half lighted; those which appear and disappear
alternately are, perhaps, of a form flattened by the violence of the
centrifugal force in their motion of rotation, and are perceiveable
only when they are in the full, disappearing when they are sideways.
In this grand order of things, and in the nature of the stars, there
are the same varieties, and the same differences, in number, size,
space, motion, form, and duration; the same relation, the same degrees,
and the same connection, as are found in all the other orders of the
creation.

Each of the suns being endowed like ours, and like all matter, with
an attractive power, which extends to an indefinite distance, and
decreases, as the space increases, analogy leads us to imagine that
within each of their spheres there exists a great number of opaque
bodies, planets, or comets, which circulate round them, but which being
much smaller than the suns which serve them for heat, they are beyond
the reach of our sight.

It might be imagined that comets pass from one system to the other,
and that if they happened to approach the confines of the two empires
they would be attracted by the preponderating power, and forced to
obey the laws of a new master. But, by the immensity of space which
is beyond the aphelion of our comets, it appears that the Sovereign
Ruler has separated each system by immense desarts, a thousand and
a thousand times larger than all the extent of known spaces. These
desarts, which numbers cannot fathom the depth of, are external and
invincible barriers, that all the powers of created nature cannot
surmount. To form a communication from one system to the other, and for
the subjects of one to pass into the other, it would be requisite that
the centre was not immoveable, for the sun, the head of the system,
changing place, would draw with it in its course all the bodies which
depend thereon, and hence might approach and invade another demesne.
If its route were directed towards a weaker star, it would commence by
carrying off the subjects of its most distant provinces, afterwards
those more interior, and would oblige them all to increase its train by
revolving round it; and its neighbour thus deprived of its subjects, no
longer having planets nor comets, would lose both its light and fire,
which their motion alone can excite and support; hence this detached
star, being no longer maintained in its place by the equilibrium of its
forces, would be obliged to change nutrition, by changing nature, and
becoming an obscure body, would, like the rest, obey the power of the
conqueror, whose fire would increase in proportion to the number of its
conquests.

For what can be said on the nature of the sun but that it is a body of
prodigious volume, an enormous mass of matter penetrated by fire, which
appears to subsist without aliment, and which resembles a metal or a
solid body in incandescence? And from whence can this constant state
of incandescence, this continually renewed production of fire proceed,
whose consumption does not appear to be supported by any aliment, and
whose deperdition is at least insensible, although constant for such
a great number of years? Is there, or can there be, any other cause
of the production of this permanent fire, but the rapid motion from
the strong pressure of all bodies, which revolve round this common
heat, and which heats and sets fire to it, like a wheel rapidly
turned round its axis? The pressure, which they exercise by virtue of
their weight is equivalent to the friction, and even more powerful,
because this pressure is a penetrating power, which not only rubs the
external surface but all the internal parts of the mass: the rapidity
of their motion is so great that the friction acquires a force almost
infinite, and consequently sets the whole mass of the axis in a state
of incandescence, of light, of heat, and of fire, which hence has no
need of aliment to be supported, and which, in spite of the deperdition
each day made by the emission of light, may remain for ever without any
sensible alteration, other suns rendering as much light to ours as it
sends to them, and no part of the smallest atom of fire, or any other
matter, being lost in a system where all is attracted.

If from this sketch of the great table of the heavens, and in which
I have only attempted to represent to myself the proportion of the
spaces, and that of the motion of bodies which travel over them;
if from this point of view, to which I only raised myself to see
how greatly nature must be multiplied in the different regions of
the universe, we descend to that proportion of space which we are
better acquainted with, and in which the sun exercises its power,
we shall discover, that although it governs all bodies therein, it,
nevertheless, has not the power of vivifying them, nor even that of
supporting life and vegetation.

Mercury, which is the nearest to the sun, nevertheless receives only
a heat 400 times stronger than that of the earth, and this heat, so
far from being burning, as it has always been supposed, would not be
strong enough of itself to support animated nature, for the actual
heat of the sun on the earth being only 1/50 part of the heat of the
terrestrial globe, that of the sun on Mercury consequently is only 1/8
part of the actual heat of the earth. Now if 7/8 parts were subtracted
from the heat which is at present the temperature of the earth, it is
certain animated nature would be checked, if not entirely extinguished.
Since the sun alone cannot maintain organised nature in the nearest
planet, how much more aid must it require to animate those at a greater
distance? To Venus it only sends a heat 2/50 times stronger than that
it sends to the earth, which instead of being strong enough to support
animated nature, would not certainly suffice to maintain the liquidity
of water, nor perhaps even the fluidity of air, since our actual
temperature would be refrigerated to 2/49, which is very near the
term 1/25 we have given as the external limit of the slightest heat,
relative to living nature. And with respect to Mars, Jupiter, Saturn,
and all their satellites, the quantity of heat which the sun sends to
them, in comparison with that which is necessary for the support of
nature, which may be looked upon as of little effect, especially in the
two larger planets, which, nevertheless, appear to be the essential
objects of the solar system.

All the planets, therefore, have always been volumes (as large as
useless) of matter more than dead, profoundly frozen, and consequently
places uninhabited and uninhabitable for ever, if they do not include
within themselves treasures of heat much superior to what they receive
from the sun. The heat which our globe possesses of itself, and which
is 50 times greater than that which comes to it from the sun, is, in
fact, the treasure of nature, the true fund which animates us as well
as every being: it is this internal heat of the earth which causes
all things to germinate and to develope; it is that which constitutes
the element of fire, properly called an element, which alone gives
motion to other elements, and which if it was reduced to 1/20 could
not conquer their resistance, but would itself fall into an inertia.
Now this element, this sole active power, which may render the air
fluid, the water liquid, and the earth penetrable, might it not have
been given to the terrestrial globe alone? Does analogy permit us to
doubt that the other planets do not likewise contain a quantity of
heat, which belongs to them alone, and which must render them capable
of receiving and supporting living nature? Is it not greater and more
worthy the idea we ought to have of the Creator, to suppose that there
every where exists beings who acknowledge his power and celebrate his
glory, than to depopulate all the universe, excepting the earth, and
to despoil it of all beings, by reducing it to a profound solitude,
in which we should only find a desart space, and frightful masses of
inanimate matter.

Since the heat of the sun is so small on the earth, and other planets,
it is necessary that they should possess a heat belonging solely to
themselves, and our enquiry must be to see whence this heat proceeds
which alone can constitute in them this element of fire. Now where
shall we be able to discover this great quantity of heat if it be
not in the source itself, in the sun alone? for the matter of which
the planets have been formed and projected by a like impulsion will
have preserved their motion in the same direction, and their heat
in proportion to their magnitude and density. Whoever weighs these
analogies, and conceives the power of their relations, will not
doubt that the planets have issued from the sun by the stroke of a
comet, because in the solar system comets only could have power and
sufficient motion, to communicate a similar impulsion to the masses
of matter which compose the planets. If to all these circumstances we
unite that of the innate heat of the earth, and of the insufficiency
of the sun to support nature, we must rest persuaded, that in the
time of their formation the planets and earth were in a state of
liquefaction, afterwards in a state of incandescence, and at last in
a successive state of heat, always decreasing from incandescence to
actual temperature, for there is no other mode of conceiving the origin
and duration of this heat peculiar to the earth. It is difficult to
imagine that the fire, termed central, can subsist at the bottom of the
globe without air (that is, without its first aliment, and from whence
this fire should proceed, which is supposed to be shut up in the centre
of the globe), because what origin, what source shall we then find
for it? Descartes has imagined the earth and planets were only small
incrusted suns; in other words, suns entirely extinguished. Leibnitz
has not hesitated to pronounce that the terrestrial globe owes its
source, and the consistence of its matters, to the element of fire; yet
these two great philosophers had not the assistance of these numerous
circumstances and observations which have been acquired and collected
in our days, and which are so well established that it appears more
than probable that the earth, as well as the planets, were projected
out of the sun, and being consequently of a like matter, which was
at first in a state of liquefaction they obeyed the centrifugal
power, at the same time that it collected itself together by that of
attraction, which has given a round form to all the planets under the
equator, and flattened under the poles, on account of the variety of
their rotation; that afterwards this fire being gradually dissipated,
the benign temperature, suitable to organized nature, succeeded in
different planets according to the difference of their thickness or
density. If there should be other particular causes of heat assigned
for the earth and planets, which might combine with those whose effects
we have calculated, our results are not less curious, nor less useful
to the advancement of science; and we shall here only observe, that
those particular causes may prolong the time of the refrigeration of
the globe, and the duration of living nature, beyond the terms we have
indicated.

But I may be asked is this Theory equally as well founded in every
point which serves for its basis; is it certain, according to your
experiments, that a globe, as large as the earth, and composed of
the same matters, cannot refrigerate from incandescence to actual
temperature in less than 74,000 years, and that in order to become
heated to the point of incandescence a 15th of this time, that is
5000 years, would be required: and also that it should be surrounded
all that time by the most violent fire; if so, there are as you say
strong presumptions that this great heat of the earth could not have
been communicated to it from a distance, and that consequently the
terrestrial matter formerly made a part of the mass of the sun; but it
does not appear equally proved that the heat of this body on the earth
is at present but 1/50 part of the heat of the globe. The testimony
of our senses seems to refute this opinion, which you lay down as a
certain truth, for although we cannot doubt that the earth has an
innate heat, which is demonstrated by its always equal temperature, in
all deep places where the coldness of the air cannot communicate; yet
does it result that this heat, which appears of moderate temperature,
is greater than that of the sun which seems to burn us?

To all these objections I can give full satisfaction, but let us first
reflect on the nature of our sensations. A very slight, and often
imperceptible, difference in the causes which affect us, produces
considerable ones in their effects. Is there any thing which comes
nearer to extreme pleasure than grief? and who can assign the distance
between the lively irritation by which we are moved with delight, and
the friction which gives us pain? between the fire which warms and that
which burns? between the light which is agreeable to our sight and that
which blinds us? between the savour which pleases our taste and that
which is disagreeable? between the smell of which a small quantity
will at first be agreeable and yet soon after create nausea? We must
therefore cease from being astonished that a small augmentation of
heat, such as 1/50 should appear so striking.

I do not pretend positively to assert that the innate heat of the
earth is really 49 times greater than that which comes to it from the
sun: for as the heat of the globe belongs to all terrestrial matter,
we have no means of separating it, nor consequently any sensible and
real limits to which we might relate it. But even if the solar heat be
greater or smaller than we have supposed, relative to the terrestrial
heat, our theory would only alter the proportion of the results.

For example, if we include the whole extent of our sensations of the
greatest heat to the greatest cold, within the limits given by the
observations of M. Amontons, that is, between seven and eight, and at
the same time suppose that the heat of the sun can alone produce this
difference of our sensations, we shall from thence have the proportion
of 8 to 1 of the innate heat of the terrestrial globe to that which
proceeds from the sun; and consequently the compensation which this
heat of the sun actually makes on the earth, would be 1/8 and the
compensation which it made in the time of incandescence will have
been 1/260: adding together these two terms, we have 26/900, which
multiplied by 12-1/2, the half of the sum of all the terms of the
diminution of heat, gives 325/400 or 5/8 for the total compensation
made by the sun's heat during the the period of 74047 years of the
refrigeration of the earth to actual temperature. And as the total
loss of the innate heat is to the total compensation in the same ratio
as the time of the period of refrigeration, we shall have 25 : 1-5/8
:; 74047 : 4813-1/25, so that the refrigeration of the globe of the
earth instead of having been prolonged only 770 years, would have been
4813-1/25 years; which joined to the longest prolongation, the heat of
the moon would also produce in this supposition, would give more than
5000 years.

If we adopt the limits laid down by M. de Marian, which are from 31 to
32, and suppose that the solar heat is no more than 1/32 of that of the
earth, we shall have only 1/4 of this prolongation, about 1250 years,
instead of 770, which gives the supposition of 1/50 which we have
adopted.

But if we suppose that the sun's heat is only 1/250 of that of the
earth, as appears to result from the observations made at Paris, we
should have for the compensation of the incandescence 1/6250 and 1/250
for the compensation to the end of the period of 7407 years of the
refrigeration of the terrestrial globe to actual temperature, and we
should find 17/250 for the total compensation made by the heat of the
sun during this period, which would give only 154 years, or the 5th
part of 770 years for the time of the prolongation of refrigeration.
And likewise, if in the place of 1/50 we suppose that the solar
heat was 1/50 of the terrestrial, we should find that the time of
prolongation would be five times longer, that is 3850 years; so that
the more we endeavour to increase the heat which comes to us from the
sun relative to that which emanates from the earth, the more we shall
extend the duration of nature, and date the antiquity of the earth
further back; for by supposing the heat of the sun was equal to the
innate of the globe, we should find that the time of prolongation would
be 38504 years, which consequently gives the earth a greater antiquity
of 38 or 39000 years.

If we cast our eye on the table which M. de Mairan has calculated with
great exactness, and in which he gives the proportion of the heat which
comes to us from the sun, to that which emanates from the earth in all
climates, we shall discover a well attested fact, which is, that in
all climates where observations have been made, the summers are equal,
whereas the winters are prodigiously unequal; this learned naturalist,
attributes this constant equality of the intensity of heat in summer in
all climates to the reciprocal compensation of the solar heat, and from
the heat of the emanations of the central fire.

All naturalists who have employed themselves on this subject agree
with me that the terrestrial globe possesses of itself a heat
independently of that which comes from the sun. Is it not evident that
this innate heat should be equal at every place on the surface of the
globe, and that there is no other difference in this respect than that
which results from the swelling of the earth at the equator, and of its
flatness under the poles? A difference, which being in the same ratio
nearly as the two diameters, does not exceed 1/230, so that the innate
heat of the terrestrial spheriod must be 1/230 times greater under
the equator than under the poles. The deperdition which is made, and
the time of refrigeration must, therefore, have been quicker, or more
sudden, in the northern climates, where the thickness of the globe is
not so great as in the southern climates, but this difference of 1/230
cannot produce that of the inequality of the central emanations, whose
relation to the heat of the sun in winter being equal 50 to 1 in the
adjacent climates to the equator, is found double to the 27th degree,
triple to the 35th, quadruple to the 40th, tenfold to the 49th, and
35 times greater to the 60th degree of latitude. This cause, which
presents itself, contributes to the cold of the northern climates, but
it is insufficient for the effect of the inequality of the winters,
since this effect would be 35 times greater than its cause to the 60th
degree, and even excessive in climates nearer the poles; at the same
time it would in no part be proportional to this same cause.

On the other hand there is not any foundation for supposing that in
a globe which has received, or which possesses a certain degree of
heat, there might be some parts of it much colder than others. We are
sufficiently acquainted with the progress of heat and the phenomena of
its communication, to be convinced that it is every where distributed
alike, since by placing a cold body on one that is hot, the latter
will communicate to the other sufficient heat to render heat of the
same degree of temperature in a short time. It must not, therefore, be
supposed that towards the poles there are strata of colder matters less
permeable to the heat than in other climates, for of whatever nature
they may be supposed to be, experience has demonstrated that in a very
short time they would become as hot as the rest.

It is evident that great cold in the north does not proceed from these
pretended obstacles which might oppose themselves to the issue of
heat, nor from the slight difference which that of the diameters of
the terrestrial spheroid must produce; but it appears to me, after
much reflection upon it, that we ought to attribute the equality of
the summers, and the great inequality of the winters to a much more
simple cause, but which, notwithstanding, has escaped the notice of all
naturalists.

It is certain that as the native heat of the earth is much greater than
that which comes to it from the sun, the summers ought to appear nearly
equal every where, because this same heat from the sun makes only a
small augmentation to the stock of real heat which the earth possesses;
and consequently if this heat issuing from the sun, be only 1/[T.N.]
of the native heat of the globe, the greater or less stay of it on
the horizon, its greater or less obliquity on the climate, and even
its total absence, would only produce one-fiftieth difference on the
temperature of the climate, and hence the summers must appear, and are,
in fact, nearly equal in all the climates of the earth. But what makes
the winters so very unequal is the emanations of this internal heat of
the globe being in a great measure suppressed as soon as the cold and
frost bind and consolidate the surface of the earth and waters.

[T.N.: denominator missing from printed version.]

This heat which issues from the globe, decreases in the air in
proportion, and in the same ratio as the space increases, and the
sole condensation of the air by this cause is sufficient to produce
cold winds, which acting against the surface of the earth, bind and
freeze it. As long as this confinement of the external strata of the
earth remains, the emanations of the internal heat are retained, and
the cold appears to be, nay in fact is, very considerably increased by
this suppression of a part of this heat; but as soon as the air becomes
milder, and the superficial strata of the globe loses its rigidity,
the heat, retained all the time of the frost, issues out in greater
abundance than in climates where it does not freeze, so that the sum
of the emanations of the heat becomes equal and every where alike; and
this is the reason that plants vegetate quicker, and the harvest is
reaped in much less time in northern countries; and for the same reason
it is, that often at the beginning of summer we feel such considerable
heats.

If there were any doubt of the suppression of the emanations of the
internal heat by the effect of frost, we might easily be convinced
of the fact; for it is a circumstance universally known, that after
a frost, we may perceive snow to thaw in pits, acqueducts, cisterns,
quarries, subterraneous vaults or mines, when even these depths, pits
or cisterns, contain no water; the emanations of the earth having
their free issue through these kinds of vents, the ground which covers
this top is never frozen so strong as the open land; to the emanations,
it permits their general course, and their heat is sufficient to melt
the snow, especially in hollow places, at the same time that it remains
on all the rest of the surface where the earth is not excavated.

This suppression of the emanations of the native heat of the earth is
not only made by the frost, but likewise by the simple binding of the
earth, often occasioned by a less degree of cold than that which is
necessary to freeze the surface; there are very few countries where it
freezes in the plains beyond the 35th degree latitude, particularly in
the northern hemisphere. It appears, therefore, that from the equator,
as far as the 35th degree, the emanations of the terrestrial heat
having always their free issue, there ought to be in that part little
or no difference between winter and summer, since this difference
proceeds only from two causes, both too slight to produce any sensible
effect. The first cause is the difference of the solar action, but as
this action is itself much smaller than that of the terrestrial heat,
its difference is too inconsiderable to be regarded as any thing. The
second cause is the thickness of the globe, which towards the 35th
degree, is near 1/590th part less than at the equator, but even this
difference can only produce a very slight effect, since at 35 degrees
the relation of the emanations of the terrestrial to the solar heat is
in summer from 33 to 1, and in winter from 153 to 1, which gives 186 to
2 or 93 to 1. From hence it can only be owing to the consolidation of
the earth occasioned by the cold, or even to the cold produced by the
durable rains which fall in these climates, that we can attribute this
difference between winter and summer; the binding of the earth by cold
suppresses a part of the emanations of the internal heat, and the cold,
always renewed by the fall of rain, diminishes its intensity; these two
causes, therefore, together produce the difference between winter and
summer.

After having proved that the heat which comes to us from the sun
is greatly inferior to the native heat of our globe; after having
explained that, by supposing it only 1/50 part, the refrigeration of
the globe to actual temperature cannot be made but in 75,832 years;
after having demonstrated that the time of this refrigeration would
still be longer, if the heat sent from the sun to the earth were in
a greater relation, namely, of 1/25 or 1/10 instead of 1/50, we
cannot be blamed for having adopted that proportion which appears the
most plausible from physical reasonings, and at the same time the
most probable, as it does not extend too far back the time of the
commencement of nature, which we have fixed at 37 or 38,000 years,
dating it from the first day.

I nevertheless acknowledge that this time, all considerable as it
is, does not appear sufficiently long for certain changes, certain
successive alterations, which Natural History demonstrates to have
taken place, and which seem to have required a still longer course of
centuries; and from which I should be inclined to imagine, that, in
reality, this time would be increased perhaps double if every phenomena
were completely investigated; but I have confined myself to the least
terms, and restrained, the limits of time as much as possible, without
contradicting facts and experiments.

This theory, perhaps, may be attacked by another objection, which it is
right to guard against. It may be told me that I have supposed, after
Newton, the heat of boiling water to be three times greater than that
of the sun in summer, and iron heated red-hot eight times greater than
boiling water, that is, 24 or 25 times greater than that of the actual
temperature of the earth, and that there is something hypothetical
in this supposition, on which I have founded the second basis of my
calculations, whose results would be, without doubt, very different if
this red heat of iron, or glass in incandescence, instead of being, in
fact, 25 times greater than the actual heat of the globe, were, for
example only 5 or 6 times as great.

The better to feel the force of this objection, let us make a
calculation of the refrigeration of the earth, upon the supposition
that in the time of incandescence it was only five times hotter than
it is according to our calculations; this solar heat, instead of a
compensation of 1/50 would have only made the compensation of 1/250 in
the time of incandescence, these two terms added together gives 6/250,
which multiplied by 2-1/2, the half of the sum of all the terms of the
diminution of heat, gives 15/250 for the total compensation which the
heat of the sun has made during the whole period of the deperdition
of the innate heat of the globe, which is 74047 years: therefore we
shall have : 15/250 :: 74047 : 888-14/25 from which we see that the
prolongation of refrigeration, which for a heat 28 times greater
than actual temperature, has been only 770 years, should have been
888-14/25 in the supposition that this first heat should have been only
five times greater than this actual temperature. This alone shews us
that if we even suppose this primitive heat below 25, there would only
be a longer prolongation of the refrigeration of the globe, and that
alone appears to me sufficient to satisfy the objection.

It may likewise be said, "you have calculated the duration of the
refrigeration of the planets, not only by the inverted ratio of their
diameters, but also by the inverted ratio of their density; this
might be well founded if we could imagine that in fact there exists
matter whose density is as different from that of our globe: but does
it exist? What, for example, will be the matter of which Saturn is
composed, since its density is more than five times less than that of
the earth?

To this I answer, that it would be very easy to find, in the vegetable
class, matters five or six times less dense than a mass of iron,
marble, hard calcareous stone, &c. of which we know that the earth is
principally composed; but without quiting the mineral kingdom, and
considering the density of these five matters, we have 21-10/72 for
iron, 8-25/72 for white marble, for gres 7-24/72, for common marble
and calcareous stone 7-20/72; taking the mean term of the densities
of these five matters, of which the terrestrial globe is principally
composed, we find its density to be 10-5/18. It is therefore required
to find a matter whose density is in the relation of 189 to 1000
density, which is the same as that between Saturn and the Earth. Now
this matter might be a kind of pumice stone, somewhat less dense than
common pumice stone, whose relative density is here 1-66/70; whence it
appears that Saturn is principally composed of a light matter similar
to pumice stone.

So likewise the density of the Earth being to that of Jupiter as 1000
to 292, we must suppose that Jupiter is composed of a more dense matter
than pumice stone, but much less dense than chalk.

The density of the Earth being to that of the Moon as 1000 to 702, this
secondary planet appears composed of a matter whose density is not
quite so great as that of hard calcareous stone, but more so than soft.

The density of the Earth being to that of Mars as 1000 to 730, this
planet must be composed of a matter somewhat more dense than that of
gres, and not so great as that of white marble.

But the density of the Earth being to that of Venus as 1000 to 12700,
it may be supposed that this planet is chiefly composed of a more
dense matter than emery, and less dense than zinc.

Finally, the density of the Earth being to that of Mercury :: 1000 :
2040, or :: 10-5/18 : 20,(966-2/3)/1000, it must be thought that this
planet is composed of a matter less dense than iron but more so than
tin.

To the question, how can animated nature, which you suppose every where
established, exist in planets of iron, emery, or pumice stone? I shall
answer, by the same causes, and by the same means as it exists on the
terrestrial globe, although composed of stone, gres, marble, iron, and
glass. There are other planets like our globe, whose principal is one
of these matters; but the external causes will soon have altered its
superficial strata, and according to the different degrees of heat or
cold, dryness or humidity, they will have converted this matter into a
fertile earth proper to receive the seeds of organized nature, which
only needs heat and moisture to develope itself.

Having answered the most obvious objections, it is necessary now to
explain the facts, and observations, by which we are assured that the
sun is only an accessory to the real heat, which continually emanates
from the globe of the earth; and it will be just, at the same time, to
see how comparable thermometers have taught us in a certain manner that
the heat in summer is equal in all the climates of the earth, excepting
Senegal, and some other parts of Africa, where the heat is greater than
elsewhere.

It may be incontestibly demonstrated, that the light, and consequently
the heat of the sun, emitted on the earth in the summer, is very great,
comparatively with that emitted by the same body in winter; and yet, by
very exact and reiterated observations, the difference of the real heat
of the sun in summer is very small. This alone would be sufficient to
prove that the heat of the sun makes only a small part of that of the
terrestrial globe; but in addition to this M. Amontons, by receiving
the rays of the sun on the same thermometer in summer and winter,
observed that the greatest heat in summer in our climate differs from
the cold in winter, when the water congeals, as only 7 differs from 6;
whereas it can be demonstrated that the action of the sun in summer is
about 66 times greater than that of the sun in winter; it therefore
cannot be doubted, that there is a fund of very great heat in the
terrestrial globe, on which, as a basis, the degrees of heat arise,
and that at the surface it does not give a greater quantity of heat
than that which comes from the sun.

If it be asked, how we can then assert that the heat in summer is 66
times grater than that in winter in our climate? I cannot give a better
answer than by referring to the memoirs given by the late M. de Mairan
in 1719, 1722, and 1765, and inserted in those of the Academy, where
he examines, with a scrupulous attention, the vicissitudes of summers
in different climates; the various causes for which may be reduced
to four principal ones: 1. The inclination under which the light of
the sun falls according to the different height of the sun on the
horizon; 2dly. The greater or less intensity of light in proportion
as its passage in the atmosphere is more or less oblique; 3dly. The
different distance of the earth to the sun in summer and winter; and
4thly. The inequalities of the length of days in different climates.
By the principle that heat is proportional to the action of light it
will be easily demonstrated, that these four united causes, combined
and compared, diminish with respect to our climate, this action of
the sun's heat in a ratio of about 66 to 1 between the summer and
the winter solstice; and this theoretical truth may be regarded as
certain, as the second truth from experience, and which demonstrates,
by the observations of the thermometer, immediately exposed to the
sun's rays in winter and summer, that the difference of real heat in
these two is, nevertheless, at most only from 7 to 6; I say at most,
for this determination given by M. Amontons is not nearly so exact as
that which has been made by M. de Mairan, who, after a great number
of final observations, proves that this relation is only as 32 to 31.
What, therefore, must indicate this prodigious inequality between
these two relations of the action of the _solar heat_, in summer and
winter, which is from 66 to 1; and of that of the _real heat_, which
is only from 32 to 31? Is it not evident that the innate heat of the
globe of the earth is considerably greater than that which comes to
us from the sun? It appears, in fact, that in the climate of Paris
this heat of the earth is 29 times greater in summer, and 491 times
greater in winter than that of the sun, as M. de Mairan has determined
it. But I have already said that we must not conclude, from these two
combined relations, the real one of the heat of the globe of the earth
to that which comes from the sun, and I have given reasons which have
determined me to suppose that we may estimate this heat of the sun 49
times less than the heat which emanates from the earth.

From the year 1701 to 1756 inclusive, a variety of observations were
made with thermometers, and the following were the results. The
greatest degree of heat, and of cold, which was experienced at Paris
in each year was collected; a total of these was made, and it was
found that the mean estimate, in all the thermometers, reduced to
Rheaumur's division, was 1026, for the greatest heat in summer, that
is 26 degrees above the freezing point; and that the mean degree of
cold in winter, during those 56 years, was 994, or 6 degrees below the
freezing point of water, whence we concluded that the greatest heat
in our summers at Paris differs from the greatest cold of our winters
only 1/32, since 994 : 1026 :: 31 : 32; and it was on this foundation
that we stated the latter to be the relation of the greatest heat to
the greatest cold. But it may be objected against the precision of
this valuation, the defect of the construction of the thermometer, and
Rheaumur's division (to which we have here reduced the scale of all the
rest); and this defect is extending only 1000 degrees below that of
ice, as if 1000 degrees were in fact, that of absolute cold, whereas
absolute cold does not exist in nature; and that of the smallest
heat should be supposed 10,000 instead of 1000, which would alter the
thermometer's gradation. It may likewise be said that it is possible
all our sensations between the greatest heat and the greatest cold are
comprised in as small an interval as that of a unit on 32 of heat, but
that the voice of judgment seems to be raised against this opinion,
and tells us this limit is too confined, and that it is much easier to
reduce this interval than to give it an eighth, or a seventh instead of
a thirty-second.

But be this valuation as it may, there can be no doubt of the truth
of these facts which we have drawn from our observations, for in the
same manner as we found, from the comparison of 56 successive years,
the heat of summer at Paris 1026, or 26 degrees above the freezing
point, we also found, with the same thermometers, that the heat in
summer was 1026 in every climate of the earth, from the equator to
the polar circle;[K] at Madagascar, in the islands of France and
Bourbon, Roderigo, Siam, and the East-Indies; at Algiers, Malta,
Cadiz, Montpelier, Lyons, Amsterdam, Upsal, Petersburgh, and as far
as Lapland, near the polar circle. At Cayenne, Peru, Martinico,
Carthagena in America; at Panama; in short, in all the climates of
the two hemispheres and continents where observations could be made,
it has been constantly found that the liquor of the thermometer rose
equally to 25, 26, or 27 degrees in the hottest days in summer; and
hence ensues the incontestible fact of the equality of heat in summer
in all climates of the earth. There are indeed some exceptions, for
at Senegal, and some few other places, the thermometer rises 5 or 6
degrees higher, to 31 or 32 degrees; but that arises from accidental
and local causes, which do not alter the truth of the observations,
nor the certainty of the general fact, which alone might demonstrate
to us, that there really exists a very great heat in the terrestrial
globe, that the effect, or the emanations, of which are nearly equal
in all the points of its surface, and that the sun, very far from
being the only sphere of heat which animates nature, is at best only
the regulator. This important fact, which we consign to posterity,
will enable it to discover the real progression of the diminution of
the heat of the terrestrial globe, which we have been only able to
determine in a hypothetical manner. In a few centuries, I am confident
it will be found that the greatest heat of summer, instead of raising
the liquor of the thermometer to 26, will not raise it to more than 25,
or 24; and from this effect, which is the result of all the combined
causes, a judgment may be formed of the value of each of the particular
causes, which produce the total effect of heat on the surface of
the globe; for the heat which belongs to the earth, and which it
has possessed from the time of incadescence, has very considerably
diminished, and will continue to diminish with the course of time: this
heat is independent of that which comes from the sun; the latter may
be looked upon as constant, and consequently in futurity will make a
greater compensation than at present. To the loss of this innate heat
of the globe there are two other particular causes, which may add a
considerable quantity of heat to the effect of the two first, the only
ones we have as yet taken notice of.

[K] See the Memoirs of Rheaumur in those of the Academy (year 1735 and
1741), and also of the Memoirs of M. de Mairan in those of the year
1765, p. 213.

One of these particular causes proceeds, in some measure, from the
first general cause, and may add something to it. It is certain that
during the time of incadescence, and indeed all the subsequent ages
till that of the refrigeration of the earth, not any of the volatile
matters could reside at the surface, or even in the internal part,
of the globe; they were raised and dispersed in the form of vapours,
and could not deposit themselves but successively in proportion as it
cooled, by which means some of these matters have penetrated through
the clefts and crevices of the earth to great depths, in an infinity of
places; and this is the primitive foundation of volcanos, which are all
found in lofty mountains, where the clefts of the earth are so much the
greater as these points of the globe are more projecting and isolated.
This deposit of the volatile combustible matters of the first ages
will have been greatly augmented by the addition of every combustible
matter which has been subsequently formed. Pyrites, sulphurs, coal,
bitumen, &c. have penetrated into the principal cavities of the earth,
and produced almost every where great masses of inflammable matters,
and often conflagrations, which have been manifested by earthquakes,
erruptions of volcanos, and by the hot springs which flow from
mountains, or run internally in the cavities of the earth. It may,
therefore, be presumed that these subterraneous fires, some of which
burn without explosion, and others with great noise and violence,
somewhat increase the general heat of the globe. Nevertheless this
addition of heat can be only very slight, for it has been observed
that it is nearly as cold on the top of volcanos as on the top of other
mountains of the same height, except at the very time when the volcano
throws out inflamed vapours or burning matters.

The second cause, which seems not to have been thought of, is the
motion of the moon round the earth. This secondary planet performs its
evolution round the earth in 27 days and one third, and being 85,325
leagues distance, it goes over a circumference of 536,329 leagues in
this space of time, which makes a motion of 817 leagues in an hour,
or from 13 to 14 leagues in a minute. Although this rout is, perhaps,
the slowest of all the celestial bodies, yet it is rapid enough to
produce on the earth, which serves for the axis or pivot to this
motion, a considerable heat by the friction which results from the
weight and velocity of this planet. But it is not possible to estimate
the quantity of heat produced by this exterior cause, because hitherto
we have had nothing which might serve us for a term of comparison. But
if we ever can discover the number, magnitude, and velocity, of all
the planets which circulate round the sun, we shall then be able to
judge of the quantity of heat which the moon can give to the earth, by
the much greater quantity of fire which all these vast bodies excite
in the sun. For my own part I am greatly inclined to think that the
heat produced by this cause in the globe of the earth, forms a very
considerable part of its own heat: and that, in consequence, we must
still extend the limits of time for the duration of nature. But let us
return to our principal object.

We have observed that the summers are very nearly equal in all climates
of the earth, and that this truth is founded on incontestible facts;
but it is not the same with respect to winters; they are very unequal,
and vary in different climates, as we remove further from that of the
equator, where the heat in winter and summer is nearly the same. I
think I have already explained in a satisfactory manner the cause of
this, viz, the suppression of the terrestrial heat. This suppression
is, as I have said, occasioned by the cold winds, which fall from the
air, bind the earth, freeze the waters, and shut up the emanations of
the terrestrial heat during the time the frosts remain; so that it is
not at all surprising that the cold in winter is in fact so much the
greater as we advance further towards the climates where the mass of
air, receiving the rays of the sun more obliquely is for that reason
colder.

But with respect to the cold as well as to the heat, there are some
countries which are an exception to the general rule. At Senegal,
Guinea, Angola, and probably in every country where the natives are
black, as in Nubia, the country of the Papous, New Guinea, &c. it
is certain that the heat is greater there than in any other part of
the earth; but this arises from local causes and therefore in those
particular climates where the east wind reigns during the whole year,
passes over a very considerable track of land, and receives a scorching
heat before it arrives to them, it is not surprising that the heat
is found 5, 6, and even 7 degrees greater than it is elsewhere. The
excessive colds of Siberia, are also to be attributed to that part of
the surface of the globe being much higher than that which surrounds
it. "The northern Asiatic countries (says the Baron Strahlenberg in
his description of the Russian Empire) are considerably more elevated
than the European. They are like a table, in comparison of the bed on
which they appear so be placed; for on coming from the west and leaving
Russia, we pass to the east by the mountains Ripha and Rymnikas to
enter Siberia, and constantly advance to an ascent." "There are many
places in Siberia," says M. Gmelin, "which are not less elevated above
the rest of the earth, nor less remote from its centre, than are many
high mountains in many other regions." These plains of Siberia, appear,
in fact, to be as high as the summit of the Riphean mountains, on
which the ice and snow do not wholly melt during summer; and if the
same effect do not happen in the plains of Siberia, it is because they
are less detached, for this local circumstance also adds much to the
duration and to the intensity of cold and heat. A vast plain once made
hot will retain its heat longer than a detached mountain, though both
are alike elevated; and for the same reason the mountain once cooled
will retain its snow or ice longer than the plain.

But if we compare the excess of heat with that of cold produced by
these particular and local causes, we shall be surprized to find, that
in Senegal, &c. where the heat is greatest, it never exceeds seven
degrees beyond the summer heat in other countries, which is 26 degrees
above the freezing point, while on the contrary, the colds of Siberia
sometimes reach 60 or 70 degrees below it, and that at Petersburgh,
Upsal, &c. under the same latitude as Siberia, the greatest cold is
not more than to 25 or 26 degrees below the freezing point; therefore,
we must conclude, that these local causes have much more influence in
cold than in hot climates. Although we cannot pretend to determine
what this great difference in the excess of cold and heat may produce,
yet by reflecting on it, it appears that we may easily conceive the
reason of this difference. The augmentation of the heat in such a
climate as Senegal can only proceed from the action of the air, the
nature of the soil, and the depression of the ground; for this country
being almost on a level with the sea, it is in a great measure covered
with scorching sands, over which an easterly wind continually blows;
this, instead of refreshing the air, only renders it more burning,
because it traverses over more than 2000 leagues of land in its way,
and consequently acquires a considerable degree of heat. But in
such countries as Siberia, where the plains are elevated like the
summits of mountains above the level of the rest of the earth, this
sole difference of elevation must produce an effect proportionally
greater than the depression of the ground of Senegal, which cannot be
supposed more than that of the level of the sea; for if the plains of
Siberia be only elevated 4 or 500 fathoms above the level of Upsal, or
Petersburgh, we must cease from being astonished that the excess of
cold is so great there; since the heat which emanates from the earth,
decreases at each point as the space increases, and this elevation of
the ground alone suffices to explain this great difference of cold
under the same latitude.

On this point there remains only one interesting question. Men,
animals, and plants, may, for some time, support the rigour of this
cold, which is 60 degrees below the freezing point; but could they also
support a heat which should be 60 degrees above it? To this we answer,
yes, provided we knew as well how to guard against the heat as we do
to shelter ourselves from the cold; and if the air could, during the
remainder of the year, refresh the earth, in the same manner as the
emanations of the heat of the globe warms the air in cold countries.
We know of plants, insects, and fish, which live and grow in baths of
45, 50, and even 60 degrees of heat; there are, therefore, species in
living nature which can support this degree of heat; and as the negroes
are in the human race those whom a strong heat the least incommodes,
might we not conclude, according to this hypothesis, that the earth
has continued to decline from its original heat, and that the race of
negroes are more ancient than that of white people?




_GENERAL VIEWS OF NATURE._


FIRST VIEW.

Nature is that system of laws established by the Creator for regulating
the existence of bodies and the succession of beings. Nature is
therefore not a body, for if it were so, it would comprehend every
thing; neither is it a being, for in that case it would necessarily be
God. We must rather consider Nature as an immense living power, which
is in subordination to the Supreme Being, and by his command animates
the universe, and whose actions are dependent on, and continued by, his
concurrence or consent. This power is that part of Divine omnipotence
which is manifested to mankind; it is the cause and effect, the mode
and substance, the design and execution. Extremely different from all
human art, whose productions are inanimate, Nature is herself a work
perpetually alive, an active, an unceasing operator, who knows how to
make use of every material, and whose power, though always employed on
the same invariable plan, instead of suffering diminution, is perfectly
inexhaustible: time, space, and matter, are her means; the universe her
object; and motion and life her end.

Every object in the universe is the effect of this power. Those springs
which she makes use of are active forces which time and space can
only limit but can never destroy; forces which unite, balance, and
oppose, but are incapable of annihilating each other. Some penetrate
and connect bodies, others heat and animate them. It is principally
by attraction and impulsion, that this power acts upon brute matter,
while heats and organic molecules are her chief active agents, which
she employs in the formation and expansion of organized beings. Aided
by such instruments, how can the operations of Nature be limited? She
only wants the additional power to create and annihilate to become
omnipotent. But these two extremes the Almighty has reserved to
himself alone; the power of creating and annihilating are his peculiar
attributes; while that of changing, destroying, unfolding, renewing,
and producing, are the only privileges he has conferred on this or any
other agent. Nature, the minister of his _irrevocable_ commands, the
depositary of his _immutable_ decrees, never deviates from the laws
he has prescribed to her; she never changes any part of his original
plan, but in all her operations she exhibits the will and design of
the eternal Lord of the universe. This grand design, this unalterable
impression of all existence, is the model upon which she invariably
acts; a model of which all the features are so strongly impressed, that
they can never be effaced; a model which the infinite number of copies,
instead of impairing, only serve to renew.

We may therefore affirm that every thing has been created, but nothing
annihilated; Nature acts between the two without ever reaching either
the one or the other. It is in some points of this vast space, which
she has filled and traversed from the beginning of ages, that we must
endeavour to lay hold of her to bring her into view.

What an infinity of objects, comprehending an infinity of matter,
which would have been created in vain, had it not been divided into
portions, separated from each other by almost inconceivable spaces!
Myriads of luminous globes, placed at immense distances, are the bases
which support the fabric of the universe, and millions of opaque
globes, which circulate round them, constitute the moving order of its
architecture. By two primitive forces, each of which are in continual
action, these masses are revolved and carried through the immensity of
space; and their combined efforts produce the zones of the celestial
spheres, and in the midst of vacuity establish fixed stations, and
regular routes and orbits. From motion proceeds the equilibrium of
worlds, and the repose of the universe. The first of these forces is
equally divided, but the second is separated in unequal proportions.
Every atom of matter contains the same degree of attractive force,
while every individual globe has a different quantity of impulsive
force assigned to each. Of the stars, some are fixed and others
wandering; some globes appear formed to attract, and others to impel or
be impelled. Some spheres have received a common impulsion in the same
direction, and others a particular impulsion. Some stars are alone,
and others are attended by satellites; some are luminous, and others
opaque masses. There are planets whose different parts successively
enjoy a borrowed light, and there are comets which, after being lost
in the immensity of space for several ages, return to receive the
influence of the solar heat. There are some suns which appear and
disappear as if they were alternately kindled and extinguished; and
there are others which merely shew themselves and then are seen no
more. Heaven abounds with great events, which the human eye is scarcely
able to perceive. A sun which expires and annihilates a world, or
system of worlds, has no other effect upon the eyes of man than an
_ignis-fatuus_, which gives a transitory blaze and then vanishes for
ever. Man, confined to the terrestrial atom on which he vegetates,
considers this atom as a world, and looks upon other worlds as atoms.

This earth which we inhabit is scarcely distinguishable among the
other globes, and perfectly invisible to the distant spheres; it is at
least a million times smaller than the sun by which it is illuminated,
and even a thousand times less than some of the planets which, by its
influence, the sun compels to circulate round him. Saturn, Jupiter,
Mars, the Earth, Venus, Mercury, and the Sun, occupy that small
portion of the heavens which we term our Universe. These planets, with
their satellites, moving with amazing celerity in the same direction,
and almost in the same plane, compose a wheel of an immense diameter,
whose axis supports the whole weight, and which by the rapidity of its
own rotation must inflame and diffuse heat and light throughout the
whole circumference. As long as this regular motion continues (and
which will be eternal, unless the Divine Mover exert the same force
to destroy as He thought necessary to create them) the sun will burn
and illuminate all the spheres of this universe with his splendor;
and as, in a system where the whole of the bodies mutually attract
each other, nothing can be lost or removed without being returned, the
quantity of matter must always remain the same; this great source of
light and life can never be extinguished or exhausted, for other suns,
which also continually dart forth their fires, constantly restore to
our sun as much light as they take from him. Comets are more numerous
than planets, and like them depend on the power of the sun; they also
press on the common focus, and by augmenting the weight increase the
inflammation. They may also be said to form a part of our universe,
for, like the planets, they are subject to the attraction of the sun.
But in their projectile and impelled motions they have nothing in
common either with each other or with the planets. Every one of them
circulates in a different plane, and they each describe orbits in
different periods of time; for some perform their revolutions in a few
years, while others require several centuries. The sun, simply moving
round his own centre, remains, as it were at rest in the midst, and,
at the same time, serves as a torch, a focus, and an axis, to all and
every part of this wonderful machine.

That the sun continues immoveable, and regulates the motions of the
other globes, is to be ascribed to his magnitude alone. The force of
attraction being in proportion to the mass of matter; as the sun is
so considerably larger than any of the comets, and contains above a
thousand times more matter than the most extensive planet, they can
neither derange him nor diminish his influence, which extending to
immense distances keeps the whole within the bounds of his power,
and thus at particular periods recals those which have stretched
furthest into the regions of space. Some of these on being brought
back, approach so near the sun, that after having cooled for ages
they receive an inconceivable degree of heat. From experiencing these
alternate extremes of heat and cold, they are subject to singular
vicissitudes, as well as from the inequalities of their motions, which
at some times are most inconceivably rapid, and at others so amazingly
slow as to be scarcely perceptible. In comparison with the planets the
comets may be considered as worlds in disorder, for to them the orbits
of the planets are regular, their movements equal, their temperature
always the same; they appear to be places of rest, where, every thing
being permanent, Nature, has the power of establishing a uniform plan
of operation, and successively to mature her various productions. Among
the planets the Earth, which we inhabit, seems to possess peculiar
advantages; from being less distant from the Sun than Saturn, Jupiter,
and Mars, it does not experience that excess of cold; nor is it so
scorched as Venus and Mercury, which appear to revolve in an orbit too
near the body of that luminary. Besides, what a peculiar magnificence
from Nature does the earth enjoy? A pure light, gradually extending
from east to west, alternately gilds both hemispheres of this globe;
which is also surrounded with a pure transparent element. By a mild
and fertile heat all the germs of existence are animated and unfolded,
and they are nourished and supported by a plentiful supply of excellent
waters. Considerable eminences dispersed over the surface of the land,
not only check, but collect the moist vapours which float in the air,
and give rise to perpetual fountains. Immense cavities evidently formed
for the reception of those waters, separate islands and continents.
The sea in extent is equal to that of the land: nor is this a cold and
barren element, but a new empire, no less rich and no less furnished
with inhabitants. By the finger of the Almighty the limits of the
waters are marked out. If the sea encroach on the western shores, it
retreats from those of the east. This great mass of water, though
inactive of itself, is agitated, and put in motion by the influence
of the celestial bodies, whence arise its regular and constant flux
and reflux; it rises and falls with the course of the moon, and is
always at the highest when the action of the sun and moon concurs; it
is from these causes uniting at the time of the equinoxes, that the
tides are then higher than at any other time; and this is certainly
the strongest mark of the connection of this globe with the heavens.
These general and constant motions are the cause of many variable and
particular circumstances; it is by those that the removals of earth are
occasioned, which falling in the form of sediment, produce mountains at
the bottom of the sea, similar to those which are on the surface of the
land; they also give rise to currents, which following the direction
of these chains of mountains, bestow on them a figure, whose angles
correspond, and maintain a course in the midst of the waves as waters
run upon land; they may in fact, be considered as sea-rivers.

The Air being lighter and more fluid than water, is subject to the
influence of a greater number of powers. It is constantly agitated
by the effects of the sun and moon, by the immediate action of the
sea, and by the rarefaction and condensation of heat and cold. The
winds are, as it may be said, its currents; they force and collect the
clouds, they give rise to meteors, and transport the moist vapours
of the ocean to the surfaces of islands and continents; from them
proceed storms, and they diffuse and distribute the fertile dews and
rains over the land; they interfere with the regular motions of the
sea, agitate the waters, sometimes stop, and at others precipitate the
currents, elevate the waves, and excite dreadful storms and tempests.
Forced by them the troubled ocean rises towards the heavens, and with
a tremendous noise and violence, rushes against those immoveable
barriers, which it can neither destroy nor surmount.

The earth being elevated above the level of the sea, it is thus
defended against its irruptions. Its surface is beautifully enamelled
with various flowers, and a constant renewing verdure; it is inhabited
by numberless species of inhabitants, among which, man, placed to
assist the intentions of Nature, presides over every other being, finds
a place of perfect repose, and a delightful habitation. He alone is
endowed with knowledge, and dignified with the faculty of admiration;
the Almighty has rendered him capable of distinguishing the wonders of
the universe, and a witness of his increasing miracles. Animated by a
ray of divinity, he participates the mysteries of the Deity. It is by
this ray that he is enabled to think and reflect, and that he perceives
and understands the wonderful works of his Creator.

The external throne of the Divine magnificence is Nature; and man, by
contemplating her, advances by degrees to the internal throne of the
Almighty. He is formed to adore his Creator, and to have dominion over
every other creature; he is the vassal of heaven, and the lord of the
earth; by him this nether globe is peopled, ennobled, and enriched; he
establishes order, subordination, and harmony among living beings, and
even to Nature herself he gives polish, extension, cultivation, and
embellishment; for he cuts down the thistle and the bramble, and, by
his care, multiplies the vine and the rose. In those dreary desarts
where man has not inhabited, we find them over-run with thorns and
briars; the trees deformed, broken and corrupted, and the seeds which
ought to renew and embellish the scene, are choaked by surrounding
rubbish, and reduced to sterility. Nature, whom we find in other
situations adorned with the splendour of youth, has here the appearance
of old age and decrepitude. Here the earth, overloaded with the spoils
of its productions, instead of presenting a scene of beautiful verdure,
exhibits only a rude mass of coarse herbage, and trees loaded with
parasitical plants, as lichens, agaries, and other impure and corrupted
fruits; the low grounds are covered with putrid and stagnant waters;
these miry lands being neither solid nor fluid, are not only impassable
but are entirely useless to the inhabitants of both land and water;
and the marshes abounding with stinking aquatic plants, serve only to
nourish venomous insects, and to harbour infectious animals. There
is, indeed, between the putrid marshes of the low ground, and the
decayed forests of the high parts of the country, a species of lands,
or savannas, but which are very different from our meadows; for in
them there is an abundance of noxious herbs which spring up and check
the growth of the useful kinds: instead of that delicate enamelled
turf, which may be considered as the down of the earth, they are
covered over with coarse vegetables and hard prickly plants, which
are so interwoven, that they appear to have more connection with each
other, than with the soil; and by a constant and successive generation
at length form a kind of rough mat several feet thick. In these
uncultivated and desolate regions, there is no road, no communication,
and no vestige of intelligence. Man, when seeking to destroy the wild
beasts, is compelled to follow their tracks, and to be constantly on
the watch, lest he should become a victim to their savage fury; alarmed
and terrified by their frequent roarings, and even awed by the profound
silence of those dreary solitudes, he shrinks back and exclaims;
"Uncultivated Nature is hideous and unflourishing; it is I alone who
can render her agreeable and vivacious. Let us drain the marshes,
and give animation to the waters, by converting them into brooks and
canals; let us make use of that active and devouring element, whose
power we have discovered; let us apply fire to this burthensome load
of vegetables, and to those decaying forests which are already half
destroyed; let us complete the work by destroying with iron what cannot
be removed by fire; and then instead of coarse reeds and water-lilies,
from which the toad is said to extract his poison, we shall soon behold
the ranunculus, truffles, and other mild and salutary herbs spring up;
that land, which was formerly impassable, will become a flourishing
pasture for flocks of cattle, where they will find plenty of food, and
where, by the excellence of their sustenance, they will increase and
multiply, and thus reward us for our labours and the protection we have
given them. Let us go still further, and subject the ox to the yoke;
let his strength and weight of body be employed to plough the ground,
which acquires fresh vigour from culture. Thus will the operations of
Nature be assisted, and acquire double strength and splendor from the
skill and industry of man."

How beautiful is cultivated Nature! How lovely does she appear when
decorated by the hand of man! He is himself her chief ornament, her
noblest production, and by multiplying his own species he increases the
most precious of her works. She even seems to multiply in proportion
to his attention, for by his art he developes all that she has
concealed in her bosom. What a source of unknown treasures has been
brought to light! flowers, fruits and grains, matured to perfection,
and multiplied to infinity; the usual species of animals transported,
propagated and increased, without number; the noxious and destructive
kinds diminished and driven from the habitations of men; gold, and
iron a more useful metal, extracted from the bowels of the earth;
torrents restrained, rivers directed in their courses and confined
within their banks, and even the ocean itself subdued, investigated
and traversed from one hemisphere to the other; the earth rendered
active, fertile, and accesible, in every part; the vallies and plains
changed into blooming meadows, rich pastures, and cultivated fields;
the hills surrounded with vines and fruits, and their summits crowned
with useful trees; the desarts converted into populous cities, whose
inhabitants spread from its centre to its utmost extremities; roads and
communications opened, established, and frequented, as so many proofs
of the union and strength of society. There are besides a thousand
other monuments of power and _glory_, which clearly demonstrate that
man is the lord of the earth; that he has changed and improved its
surface; and that from the earliest periods of time he alone has
divided the empire of the world between him and Nature.

It is by the right of conquest, however, that he reigns; he rather
enjoys than possesses, and it is by perpetual activity and vigilance
that he preserves his advantage; if those are neglected every thing
languishes, changes, and returns to the absolute dominion of Nature,
she resumes her power, and destroys the operations of man; envelopes
with moss and dust his most pompous monuments, and in the progress of
time entirely effaces them, leaving him to regret having lost by his
negligence what his ancestors had acquired by their industry. Those
periods in which man loses his empire, those ages in which every thing
valuable perishes, commence with war, and are completed by famine
and depopulation. Although the strength of man depends solely upon
the union of numbers, and his happiness is derived from peace, he is,
nevertheless, so regardless of his own comforts as to take up arms
and to fight, which are never-failing sources of ruin and misery.
Incited by insatiable avarice, or blind ambition, which is still more
insatiable, he becomes callous to the feelings of humanity; regardless
of his own welfare, his whole thoughts turn upon the destruction of his
own species, which he soon accomplishes. The days of blood and carnage
over, and the intoxicating fumes of glory dispelled, he beholds,
with a melancholy eye, the earth desolated, the arts buried, nations
dispersed, an enfeebled people, the ruins of his own happiness, and the
loss of his real power.

Omnipotent God! by whose presence Nature is supported, and harmony
among the laws of the universe maintained; who seest from thy
immoveable throne in the empyrean all the celestial spheres rolling
under thy feet without deviation or disorder; who, from the bosom of
repose, every instant renewest their vast movements, and who alone
governs in profound peace an infinite number of heavens and of earths,
restore, restore tranquillity to a troubled world! Let the earth be
silent! Let the presumptuous tumults of war and discord be dispelled
by the sound of thy voice! Merciful God! author of all beings, whose
paternal regards extend to every created object, and to man, thy
principal favourite; thou hast illumined his mind with a ray of thy
immortal light; penetrate also his heart with a shaft of thy love;
thy divine sentiment, when universally diffused, will unite the most
hostile spirits; man will no longer dread the sight of man, nor will
his hand any longer continue to be armed with murdering steel; the
devouring flames of war will no longer stop the sources of generations;
the human species, which are now weakened, mutilated, and prematurely
mowed down, will germinate anew, and multiply without number. Nature,
groaning under the pressure of calamity, sterile and abandoned, will
soon resume with additional vigour her former fecundity; and we,
beneficent God! shall aid, cultivate, and incessantly contemplate her
operations, that we, at every moment, may be enabled to offer thee a
fresh tribute of gratitude and admiration.




SECOND VIEW.


Individuals of whatever kind, or however numerous, are of no estimation
in the universe; it is species alone that are existences in Nature,
for they are as ancient and permanent as herself. To have a clear
and distinct idea of this subject we must not consider a species as
a collection or succession of similar individuals, but as a whole,
independently of number or time, always active, and always the same;
a whole which was considered but as one in the works of the creation,
and therefore constitutes only a unit in Nature. Of these units the
human species is to be placed in the first rank; all the others, from
the elephant to the mite, from the cedar to the hyssop, belong to
the second and third orders. Notwithstanding that they are different
in form, substance, and even life, yet each sustains its appointed
destination, and subsists independently of others, while the whole, in
a general view, represents animated Nature, who has hitherto supported,
and will continue to support, herself in the same manner as she is seen
at present. Her duration is not to be estimated by a day, a year, an
age, nor any given period of time, for time itself relates only to
individuals, to beings whose existence is limited. It is not so with
respect to species, for their existence is constant; their permanence
produces duration, and their differences give rise to number. It is
in this light that we must consider species, and give to each an
equal right to the indulgence and support of Nature; for so _she_ has
certainly considered them, by bestowing on each the means of existing
as long as herself.

Let us now consider the species as having changed places with the
individual. In our preceding observations we have seen the relation
which Nature holds in respect to man; let us now then take a view
in what light she would appear to a being who represented the whole
human species. We perceive that in the spring the fields renew their
verdure, the buds and flowers expand, the bees revive from their
state of torpor, the swallows return to our climates, the nightingale
chaunts her song of love, the lamb frisks, and the bull laws with
desire, and all animated creatures are eager to unite and multiply
their species; and we can then have no ideas but those of reproduction
and the increase of life. But when the dark season of cold and frost
approaches, these same beings become indifferent to and avoid each
other; many of the feathered race desert our clime, and the inhabitants
of the waters lose their freedom under the massy congelations of ice;
various animals dig retreats for themselves in the ground, where they
fall into a state of torpor; the earth becomes hard, the plants wither,
and the trees, deprived of their foliage, are covered with frost and
snow; every object excites the idea of languor and annihilation.
These appearances, however, of renovation and destruction, images,
as it were, of life and death, although they seem general, are only
individual and particular. Man, as an individual, concludes in this
manner, but the being whom we have supposed as a representative of the
species, thinks and judges in a manner more exalted and general; in
that constant succession of destruction and renovation, and in those
various vicissitudes, he perceives only permanence and duration. The
different seasons in one year appear to him the same as those of the
preceding, the same as those of millions of ages. The animal which may
be the thousandth in the order of generation is the same to him as the
first. In a word, if man had no period to his existence, and if all
the beings by which he is surrounded existed in the same manner as they
do at present, the idea of time would vanish and the individual would
in fact become the species.

Let us then consider Nature for a few moments under this new aspect.
Man certainly comes into the world enveloped in darkness. His mind is
equally naked with his body; he is born without knowledge and without
defence, and brings nothing with him but passive qualities. He is
compelled to receive the impressions of objects on his organs; even
the light shines on his eyes long before he is able to recognize it.
To Nature he is at first indebted for every thing, without making her
any return. No sooner, however, do his senses acquire strength and
activity, and he can compare his sensations, than he reflects upon the
universe; he forms ideas, which he retains, extends, and combines. Man,
after receiving instruction, is no longer a simple individual, for
he then, in a great measure, represents the whole human species. He
receives from his parents the knowledge which had been transmitted to
them from their forefathers; and thus, by the divine arts of writing
and printing, the present age, in some sort, becomes identified with
those that are past. This accumulation of experience in one man, almost
extends the limits of his being to infinity. He is born no more than
a simple individual, like other animals, capable only of attending to
present sensations; but he becomes afterwards nearly the being which
we supposed to represent the whole species; he reads what has past,
sees the present, and judges of the future; and in the torrent of time,
which carries off and absorbs all the individuals of the universe,
he perceives that the species are permanent, and Nature invariable.
As the relations of objects are always the same, to him the order of
time appears to be nothing; he considers the laws of renovation as
only counterbalancing those of permanency. An uninterrupted succession
of similar beings, is, in effect, only equivalent to the perpetual
existence of one of them.

What purposes then are gained by this immense train of generations,
this profusion of germs, many thousands of which are abortive for one
that is brought into life? Does not this perpetual propagation of
beings, which are alternately destroyed and renewed, uniformly exhibit
the same scene, and occupy the same proportion in Nature? From what
cause proceed all these changes of life and death, these laws of
growth and decay, all these individual vicissitudes, and reiterated
representations of the same identical thing? They certainly arise from
the very essence of Nature, and depend on the first establishment of
the universal machine; the whole of which is fixed and stable, but
each of its parts being endowed with the power of motion, the general
movements of the celestial bodies have produced the particular ones of
this terrestrial globe. The penetrating forces by which these immense
bodies are animated, and by which they act reciprocally upon each other
at a distance, at the same time animate every particle of matter; and
this strong propensity, which every part has towards each other, is
the first bond of beings, the ground of consistence and permanency in
Nature, and the support of harmony in the universe. From these great
combinations the smaller relations are derived. The earth moving on
its own axis having separated the portions of duration into day and
night; all its animated inhabitants have their stated periods of light
and darkness, of their times of waking and sleeping. The action of the
senses, and the motions of the members which form a great part of the
animal economy, are related to this first combination; for in a world
where perpetual darkness reigned, would there be senses alive to the
enjoyment of light.

As the inclination of the axis of the earth, in its annual course round
the sun, produces considerable variations of heat and cold, which we
call seasons, all its vegetables have also, either wholly or partially,
their seasons of life and death. The fall of the leaves, and the decay
of fruits, the withering of herbs and the destruction of insects,
depend entirely on this second combination. In those climates where
there is not this variation, by the inclination not being so material,
the life of the vegetable is not suspended, and every insect completes
the stated period of its existence. Where the four seasons, in fact,
make but one, as under the line, the surface of the earth is constantly
covered with flowers, the trees have a perpetual foliage, and Nature
seems to enjoy a continual spring.

Both in animals and plants, their particular constitution is relatively
to the general temperature of the earth, and which temperature depends
upon its situation and distance from the sun. If they were removed to
a greater distance, neither our animals, nor our plants, could live or
vegetate; the water, sap, blood, and all their liquors, would lose
their fluidity; if on the contrary they were more near they would
vanish and dissipate in vapour. Ice and fire are the elements of death,
and temperate heat the first support of life. The living particles so
generally diffused through all organized bodies are related, not only
by their activity but number, to the particles of light which strike
and penetrate almost all matter with their heat; for in every place
where the sun can heat the earth with its rays, the surface will be
covered with verdure, and peopled with animals; even ice is no sooner
dissolved into water than it swarms with inhabitants. Water, indeed, is
apparently more fertile than the earth; from heat it receives motion
and life. In one season the sea produces more animals than the earth
sustains; but its production of vegetables is infinitely less. And
because that the inhabitants of the ocean have not a sufficient and
permanent supply of vegetables, they are compelled to feed upon each
other; and it is to this necessity that their immense multiplication
may be referred.

As in the beginning every species was created, the first individual
of each has served for a model to their descendants. The body of each
animal or vegetable is a mould, to which are assimilated indifferently
the organic particles of all animals or vegetables which have been
destroyed by death, or consumed by time. The brute particles, of which
part of their composition was formed, returned to the common mass
of inanimate matter; but the organic particles, whose existence is
permanent, are again resumed by organized bodies: they are extracted at
first from the earth by vegetables, and then absorbed by animals who
feed thereon; and thus serve for the support, growth, and expansion of
both. By this constant and perpetual circulation from body to body,
they serve to animate all organized beings. These living substances in
quantity are always the same, and differ only in form and appearance.
In fertile ages, and when population is the greatest, the whole surface
of the earth seems to be covered with men, domestic animals, and useful
plants. But in the times of famine and depopulation, the ferocious
animals, poisonous insects, parasitical plants, and useless herbs,
resume, in their turn, dominion over the earth. To man these changes
are material, but to Nature they are perfectly indifferent. The silk
worm so inestimable to the former, is to the latter only a caterpillar
of the mulberry tree. Though this caterpillar, which so materially
assists in the supply of our luxuries, should disappear; though the
plants, from which our domestic animals procure their nourishment,
should be devoured by other caterpillars; though still others should
destroy the substance of our corn before the harvest; in short, though
man and the larger animals should be starved by the inferior tribes,
Nature would not be less abundant nor less alive; she never protects
one at the expence of another, but especially supports the whole. As
to individuals she is regardless of number; she considers them only as
successive images of the same impression; as passing shadows of which
the species is the substance.

In earth, air, and water, then, there exists a certain quantity of
organic matter which cannot be destroyed, but which is constantly
assimilated in a certain number of moulds, that are perpetually
undergoing destruction and renewal: these moulds, or rather
individuals, tho' varying in number in every species, are nevertheless
always the same, that is, proportioned to the quantity of living
matter; and this appears to be absolutely the case, for if there were
any redundance of this matter, or if it were not at all times fully
occupied by the individuals of the species which exist, it would, most
assuredly, form itself into new species, for being alive it would not
remain without action; and once uniting with brute matter is sufficient
to form organized bodies; and it is by this constant combination, and
invariable proportion, that Nature preserves her form and consistence.

The laws of Nature, both with respect to the number of species and of
their support and equilibrium, being fixed and constant, she would
invariably have the same appearance, and be in all climes absolutely
the same, if her complexion did not so completely vary in almost every
individual form. The figure of each species is an impression, in which
the principal characters are so strongly engraven as never to be
effaced; but the accessory parts and shades are so greatly varied that
no two individuals have a perfect resemblance to each other; and in all
species there are a number of varieties. The human species, which has
such superior pretensions, varies from white to black, from small to
great, &c. The Laplander, the Patagonian, the Hottentot, the European,
the American, and the Negro, though the offspring of the same parents,
have by no means the resemblance of brothers.

It is evident, therefore, that every species is subject to individual
differences, but that each of them does not equally possess the
constant varieties which are perpetuated through successive
generations; the more dignified the species, the less changeable is
its figure, and the less are the varieties of it. The multiplication
of animals being inversely in proportion to their magnitude, as the
possibility of variation must be in exact proportion to the numbers
they produce, there consequently must be more varieties among the small
than the large animals; and also, for the same reason, there will be a
greater number of species which seem to approach each other; for the
unity of the species in the large animals is more fixed, and the nature
of their separation more extended. What a number of various and similar
species surround those of the squirrel, the rat, and other small
quadrupeds, while the massy elephant stands alone, without a compeer,
and at the head of the whole.

The brute matter, of which the body of the earth is principally
composed, is a substance that has not undergone many alterations,
though the whole has more than once been disturbed and put in motion
by the hand of Nature. The globe of the earth has been penetrated by
fire, and afterwards covered and disordered by water. The sand, which
occupies the interior parts of the earth, is a vitrified matter; and
the layers of clay, by which its surface is covered, are nothing
but the same sand having been decomposed by the operation of the
waters. Granite, free-stone, flint, nay, all metals, are composed of
this same vitrified matter, whose particles have been condensed or
separated, according to the laws of their affinity. These substances
are totally destitute of animation; they exist, and will continue to
do so, independently of animals and vegetables. There are, however,
many other substances, which, although they have the appearance of
being equally inanimate, originate from organized bodies; and of
this description are marble, lime-stone, chalk, and marl; they being
composed of the fragments of shells, and of those small animals which
by transforming the water of the sea into stone, produce coral, and
all the madrepores, whose varieties are numberless, and whose quantity
are almost immense. Pit-coal, turf, and many other substances found in
the upper strata, are also of this nature, they being only the residue
of vegetables which have been more or less corrupted or consumed.
Besides these, there are other substances which have been produced
by the second action of fire upon original matter; these are but few
in number, and consist of such as pumice-stones, sulphur, the scoria
of iron, asbestos, and lava. To one or other of these three great
combinations may be referred all the relations of brute matter, and all
the substances of the mineral kingdom.

The laws of affinity, by which the various particles of these different
substances separate from each other, in order to unite among themselves
and form homogeneous masses, are perfectly similar to that general law
by which the celestial bodies act upon each other; in both cases their
exertions are the same. Globules of water, of sand, or of metal, have
the same influence, and act upon each other as the earth acts upon the
moon; and if the laws of affinity have hitherto been deemed different
from those of gravity, it is because the subject has been considered in
a very confined point of view. The mutual action of celestial bodies
is very little influenced by figure; their distance from each other
is so very great, that this is necessarily the case; but when they
are not far asunder, then the effect of figure is considerable. For
instance, if the earth and moon, instead of spherical figures, were
both short cylinders, and exactly equal throughout in their diameters,
their reciprocal action would be very little varied from what it is at
present, because the distances of all their parts from each other would
be very little changed. But if these two globes were cylinders of great
extent, and approached near to each other, the law of their reciprocal
action would seem to be different, inasmuch as the distances of their
parts would be greatly varied; and hence whenever figure becomes a
principle in distance the law will appear to vary, although in fact it
is always the same.

The human intellect guided by this principle, may advance one step
further in penetrating into the operations of nature. The figure of
the constituent particles of bodies still remains unknown; we cannot
entertain the smallest doubt that water, air, earth, metals, and all
homogeneous particles, are composed of elementary particles, which are
perfectly similar, although we are still ignorant of their figure. By
the aid of calculation this at present unknown field of knowledge may
be disclosed by posterity, and the figure of the elementary bodies be
ascertained with tolerable precision. They may take the principle we
have established as the basis of their enquiry; namely, "that all
matter is attracted in the inverse ratio of the square of the distance;
and this law seems to admit of no variation in particular attractions
but what arises from the figure of the constituent particles of each
substance, because this figure enters as an element or principle into
the distance;" and having once discovered, by repeated experiments,
the law of attraction in any particular substance, they may then, by
the aid of calculation, be able to trace the figure of its constituent
particles. To render this point more clear, let us suppose, that by
placing mercury on a perfectly polished surface, repeated experiments
prove that this fluid metal is always attracted in the inverse ratio of
the cube of the distance; it will then become necessary to investigate
what figure gives this expression; and this figure will be certainly
that of the constituent particles of mercury. If it should appear, by
such experiments, that the attraction of mercury was in the inverse
ratio of the square of the distance, it would be clearly demonstrated
that its constituent particles were spherical, because a sphere is the
only figure which observes this law, and at whatever distance globes
are placed the law of their attraction is always the same.

Newton had some idea that chemical affinities (which are nothing more
in fact than these particular attractions which we have mentioned)
were produced by the same kind of laws as those of gravitation; but he
does not appear to have perceived that all those particular laws were
merely simple modifications of the general one, and that their apparent
difference arose solely from the circumstance of the figure of the
atoms, which attract each other, having, when at small distances, a
greater influence upon the force of this law than the mass of matter.

It is, notwithstanding, upon this theory that the perfect knowledge
of brute matter depends. The basis of all matter is the same, and
its form throughout would be perfectly similar, if the figures of
its constituent particles were not different; and thus it is that
one homogeneous substance can differ from another only in proportion
to the difference of their original particles. A body composed of
spherical particles ought to be one half specifically lighter than
that whose particles are cubical, because as the first only touch each
other by their points, they leave intermediate spaces equal to what
they occupy, whereas the cubical particles join without leaving the
smallest interval, and must consequently form a matter half as heavy
again. Although the figures are considerably varied, that variation is
by no means so great as we might imagine, since Nature has fixed the
limits of lightness and gravity. Gold and air, with respect to density,
are the two extremes, and therefore all the figures in Nature must be
comprehended as coming between those two; such as would have produced
heavier or lighter substances have been rejected.

In speaking of figures, as employed by Nature, I do not mean to imply
that they must be necessarily, or are exactly, similar to those
geometrical figures which we form in our imagination. We form laws by
supposition, and then endeavour to render them simple by abstraction.
It is very possible that there are neither exact cubes nor perfect
spheres in the universe; but as nothing certainly exists without form,
and as from the variation of substances the figures of the elements are
different, some of them most undoubtedly must approach to the sphere,
the cube, and all the other regular figures which we have conceived.
The precise, absolute, and abstract figures which our minds are so
frequently induced to admit, cannot have any existence, because all
objects are related, and differ only by almost imperceptible shades.
It is by the same rule that when I speak of one substance as being
entirely full, because composed of cubical particles, and another as
being not more than half full, because its parts are spherical, I mean
only comparatively, and not that such substances really exist; for
experience has fully informed us that in transparent bodies, such as
glass, which is both dense and heavy, there is but a small quantity of
matter in proportion to the extent of the intervals; nay, as we have
before observed, it might be demonstrated that even gold, which is the
most dense species of matter, has more vacuities than substance.

To investigate the powers of Nature is the object of rational
mechanics, while active mechanics is solely confined to a combination
of particular powers, and consequently the art of constructing
machines. This art has at all times been certain of cultivation from
necessity and convenience; and both ancients and moderns have equally
excelled in it. But rational mechanics is a science invented in our
days; for, from the days of Aristotle to those of Descartes, even the
philosophers have reasoned no better upon the nature of motion, than
uniformly to mistake the effect for the cause. Impulsion was the only
force with which they were acquainted; to it they attributed the
effects of others, and all the phenomena of the universe. If this idea
of theirs had been probable, or even possible, impulsion, which they
regarded as the sole cause, must have been a general effect, which
equally belonged to all matter, and which equally exerted itself in all
places, and at all times; but every day demonstrated the contrary to be
the fact; for they must have perceived that this force had no existence
in bodies at rest; that it had but a short subsistence in projected
bodies, being soon destroyed by resistance; that a fresh impulse was
absolutely necessary for its renewal, and that, consequently, so far
from being a general cause, it was only a particular effect produced by
others more general.

It is true, however, that we ought to consider a general effect as a
cause, for we cannot become acquainted with the real cause of this
effect, because all our knowledge is derived from comparison; and as
there is not any thing to which we can compare an effect, which is
supposed general, and equally belonging to every thing, we can know
it only by the fact. According to this view, attraction, or gravity,
being a general effect common to all matter, and clearly evinced by the
fact, ought to be considered as a cause; and to which all particular
causes should be referred, nay even that of impulsion, since it is
less general and less constant; and the principal difficulty is to
perceive how impulsion can be an effect of attraction; for if we rest
on the communication of motion by impulse, we are then persuaded that
it can only be transmitted from one body to another by elasticity, and
that all the hypotheses, which suppose a communication of motion in
hard bodies, are mere ideal fancies, which do not exist in Nature. A
perfectly hard or a perfectly elastic body is entirely imaginary, as
neither of them really exist; for it is certain that nothing exists
absolutely or in extreme; and the idea of perfection must suppose one
or the other.

It is certain that if there were no elasticity in matter there would be
no impulsive force; for instance, if we throw a stone, the motion it
acquires is communicated by the elasticity of the arm. When motion is
communicated by one body in action encountering another at rest, how
can we possibly suppose it to be done otherwise than by compressing the
spring of the elastic particles it contains, which recovering itself
almost immediately after, gives to the whole mass a force equal to
that which it received? How a perfectly hard body should admit this
force, or receive motion, is beyond comprehension; and the enquiry is
unnecessary, since no such body exists; for, all bodies are endowed
with elasticity. The force of electricity is proved by experiments to
be elastic, and to belong to matters in general; and therefore, if no
other elasticity existed in the interior parts of bodies but that of
this electrical matter, that would be sufficient for the communication
of motion; and consequently to this great spring, as a general effect,
the particular cause of impulsion must be attributed.

A little reflection on the mechanism of elasticity will convince us
that its force depends on that of attraction. To have a still more
clear idea of this subject, let us suppose a spring the most simple,
such as of a solid angle of iron, or of any other hard substance, and
then see what will be the result of compressing it. By compression
we oblige the parts adjacent to the top of the angle to bend, or to
separate a little from each other; but the pressure being removed they
again approach as near as they had done before. Their adhesion, from
which the cohesion of bodies results, is clearly an effect of their
mutual attraction. Upon the spring being pressed this adhesion is not
destroyed, because, although the particles are separated, they are not
removed beyond the sphere of their mutual attraction; consequently the
moment the pressure is taken away the force is renewed, the separated
parts draw near, and their spring is restored. But if the pressure be
too violent, they will, in that case, be removed beyond the sphere of
their attraction, and the spring will break, because the compressing
force will be greater than that of cohesion, or that of mutual
attraction, by which the particles are kept together. This proves
that elasticity can only exert itself in proportion to the cohesion
of the particles of matter, that is, in proportion as they are united
by the force of their mutual attraction; from which it results, that
elasticity in general, which alone can produce impulsion, and impulsion
itself, are owing to the force of attraction, and are only particular
effects which depend on that general one.

Notwithstanding that these ideas appear to be perfectly clear to me,
I do not expect to see them adopted. People in general reason only
from their sensations, and natural philosophers determine from their
prejudices; as, therefore, both these must be set aside, very few will
remain to form a proper judgment; but such is the dignity of Truth,
that she is content with a few admirers, and is always lost in a crowd;
she is at all times august and majestic, notwithstanding which she is
frequently obscured by fantastic opinions, and obliterated by fanciful
chimeras. I, however, view and understand Nature in this manner, and am
almost induced to believe that she is still more simple; the phenomena
exhibited by brute matter is caused by a single force, and from this
force, combined with that of heat, originate those living particles
which gave rise to, and support all, the various effects of organized
bodies.




FINNIS.




T. Gillet, Crown-court, Fleet-street.


       *       *       *       *       *


Transcriber Note


All obvious typographical errors were corrected. Where several variant
spellings were used, the most prevalent version was use to standardize
them. Although the printed version capitalized the first word in the
major sections, they are presented as first letter only capital. On
page 188, the odd fraction of 87 divided by 1 was left as printed. In
addition to obvious typographical corrections, the following were made:

  Page(s)   Change
  ========  =================
  134       "proxility" changed to "prolixity"
  135-143   Best judgement used in the table where numbers not clearly
              decipherable in the best images available
  142       BISMUTH, with Antimony starts with 10004 all others start
              with 10000. The "4" assumed typo changed to "10000".
  143       Shows 10,0000. the last '0' assumed typo and removed.
  167       Twice shows a fraction of "16/11 of gold". Although this may
              be a typo for "10/11 of gold" it was left unchanged.
  248       "aoules" changed to "aoutes"