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
From these combined causes, the ebbing and flowing of the tides, and the
motion of the earth, we may fairly conclude, that although the earth was
a perfect sphere in its original form, yet its diurnal motion, together
with the constant flux and reflux of the sea, must, by degrees, in the
course of time, have raised the equatorial parts, by carrying mud,
earth, sand, shells, &c. from other climes, and there depositing of
them. Agreeable to this idea the greatest irregularities must be found,
and, in fact, are found near the equator. Besides, as this motion of the
tides is made by diurnal alternatives, and been repeated, without
interruption, from the commencement of time, is it not natural to
imagine, that each time the tide flows the water carries a small
quantity of matter from one place to another, which may fall to the
bottom like a sediment, and form those parallel and horizontal strata
which are every where to be met with? for the whole motion of the water,
in the flux and reflux, being horizontal, the matters carried away with
them will naturally be deposited in the same parallel direction.
But to this it may be said, that as the flux and reflux of the waters
are equal and regularly succeed, two motions would counterpoise each
other, and the matters brought by the flux would be returned by the
reflux, and of course this cause for the formation of the strata must be
chimerical; that the bottom of the sea could not experience any material
alteration by two uniform motions, wherein the effects of the one would
be regularly destroyed by the other; much less could they change the
original form by the production of heights and inequalities.
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