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
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.
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