Buffon's Natural History. Volume 10 (of 10): Containing a Theory of the Earth, a General History of Man, of the Brute Creation, and of Vegetables, Minerals, &c. &cBuffon, Georges Louis Leclerc, comte de
History
Buffon's Natural History. Volume 10 (of 10): Containing a Theory of the Earth, a General History of Man, of the Brute Creation, and of Vegetables, Minerals, &c. &c
Buffon, Georges Louis Leclerc, comte de
Natural history
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.
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