Buffon's Natural History, Volume 01 (of 10): Containing a Theory of the Earth, a General History of Man, of the Brute Creation, and of Vegetables, Mineral, &c. &cBuffon, Georges Louis Leclerc, comte de
History
Buffon's Natural History, Volume 01 (of 10): Containing a Theory of the Earth, a General History of Man, of the Brute Creation, and of Vegetables, Mineral, &c. &c
Buffon, Georges Louis Leclerc, comte de
Natural history
But it may be said, if this theory is true, and if 229 to 230 is the
just relation of the axis, why did the mathematicians, sent to Lapland
and Peru, agree to the relation of 174 to 175? From whence does this
difference arise between theory and practice? And is it not more
reasonable to give the preference to practice and measures, especially
when we have been taken by the most able mathematicians of
Europe[109:A], and with all necessary apparatus to establish the result.
To this I answer, that I have paid attention to the observations made at
the equator and near the polar circle; that I have no doubt of their
being exact, and that the earth may possibly be elevated an 175th part
more at the equator than at the poles. But, at the same time, I maintain
my theory, and I see clearly how the two conclusions may be reconciled.
This difference is about four leagues in the two axes, so that the parts
at the equator are raised two leagues more than they ought to be,
according to my theory; this height answers exactly to the greatest
inequalities on the surface of the globe, produced by the motion of the
sea, and the action of the fluids. I will explain; it appears that when
the earth was formed, it must necessarily have taken, by virtue of the
mutual attraction of its parts, and the action of the centrifugal force,
a spheroidical figure, the axes of which differ a 230th part: the
original earth must have had this figure, which it took when it was
fluid, or rather liquified by the fire; but after its formation the
vapours which were extended and rarefied, as in the atmosphere and tail
of a comet, became condensed, and fell on the surface in form of air and
water: and when these waters became agitated by the flux and reflux, the
matters were, by degrees, carried from the poles towards the equatorial
parts; so that the poles were lowered about a league, and those of the
equator raised in the same proportion; this was not suddenly done, but
by degrees in succession of time; the earth being also exposed to the
action of the winds, air, and sun; all these irregular causes concurred
with the flux and reflux to furrow its surface, hollow it into valleys,
and raise it into mountains; and producing other inequalities and
irregularities, of which, nevertheless, the greatest thickness does not
exceed one league at the equator; this inequality of two leagues, is,
perhaps, the greatest which can be on the surface of the earth, for the
highest mountains are scarce above one league in height, and there is
much probability of the sea's not being more at its greatest depth. The
theory is therefore true, and practice may be so likewise; the earth at
first could not be raised above 6-1/2 leagues more at the equator than
the poles, but the changes which have happened to its surface might
afterwards raise it still more. Natural History wonderfully confirms
this opinion, for we have proved in the preceding discourse that the
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