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
In the very bowels of the earth, on the tops of mountains, and even the
most remote parts from the sea, shells, skeletons of fish, marine
plants, &c. are frequently found, and these shells, fish, and plants,
are exactly similar to those which exist in the Ocean. There are a
prodigious quantity of petrified shells to be met with in an infinity of
places, not only inclosed in rocks, masses of marble, lime-stone, as
well as in earth and clays, but are actually incorporated and filled
with the very substance which surrounds them. In short, I find myself
convinced, by repeated observations, that marbles, stones, chalks,
marls, clay, sand, and almost all terrestrial substances, wherever they
may be placed, are filled with shells and other substances, the
productions of the sea.
These facts being enumerated, let us now see what reasonable conclusions
are to be drawn from them.
The changes and alterations which have happened to the earth, in the
space of the last two or three thousand years, are very inconsiderable
indeed, when compared with those important revolutions which must have
taken place in those ages which immediately followed the creation; for
as all terrestrial substances could only acquire solidity by the
continued action of gravity, it would be easy to demonstrate that the
surface of the earth was much softer at first than it is at present, and
consequently the same causes which now produce but slight and almost
imperceptible changes during many ages, would then effect great
revolutions in a very short space. It appears to be a certain fact, that
the earth which we now inhabit, and even the tops of the highest
mountains, were formerly covered with the sea, for shells and other
marine productions are frequently found in almost every part; it appears
also that the water remained a considerable time on the surface of the
earth, since in many places there have been discovered such prodigious
banks of shells, that it is impossible so great a multitude of animals
could exist at the same time: this fact seems likewise to prove, that
although the materials which composed the surface of the earth were then
in a state of softness, that rendered them easy to be disunited, moved
and transported by the waters, yet that these removals were not made at
once; they must indeed have been successive, gradual, and by degrees,
because these kind of sea productions are frequently met with more than
a thousand feet below the surface, and such a considerable thickness of
earth and stone could not have accumulated but by the length of time. If
we were to suppose that at the Deluge all the shell-fish were raised
from the bottom of the sea, and transported over all the earth; besides
the difficulty of establishing this supposition, it is evident, that as
we find shells incorporated in marble and in the rocks of the highest
mountains, we must likewise suppose that all these marbles and rocks
were formed at the same time, and that too at the very instant of the
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