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
"The sea," continues he, "therefore, covered the whole earth, and from
thence it proceeds that all the beds of stone in the plains are
horizontal and parallel; fish must have also been the most ancient
inhabitants of the globe, as there was no sustenance for either birds or
terrestrial animals." But how did the sea retire into these vast basins
which it at present occupies? What presents itself the most natural to
the mind is, that the earth, at least at a certain depth, was not
entirely solid, but intermixed with some great vacuums, whose vaults
were supported for a time, but at length, sunk in suddenly: then the
waters must have fallen into these vacancies, filled them, and left
naked a part of the earth's surface, which became an agreeable abode to
terrestrial animals and birds. The shells found in quarries perfectly
agree with this idea, for only the bony parts of fish could be preserved
till now. In general, shells are heaped up in great abundance in certain
parts of the sea, where they are immovable, and form a kind of rock, and
could not follow the water, which suddenly forsook them: this is the
reason that we find more shells than bones of the fish, and this even
proves a sudden fall of the sea into its present basins. At the same
time as our supposed vaults gave way, it is very possible that other
parts of the globe were raised by the same cause, and that mountains
were placed on this surface with quarries already formed, but the beds
of these quarries could not preserve the horizontal direction they
before had, unless the mountains were raised precisely perpendicular to
the surface of the earth, which could happen but very seldom: so also,
as we have already observed, in 1705, the beds of stone in mountains are
always inclined to the horizon, though parallel with each other; for
they have not changed their position with respect to each other, but
only with respect to the surface of the earth[205:A].
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account