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
These parallel strata, these beds of earth and stone, which have been
formed by the sediment of the sea, often extend to considerable
distances, and we often find in hills, separated by a valley, the same
beds and the same matters at the same level. This observation agrees
perfectly with that of the height of the opposite hills. We may easily
be assured of the truth of these facts, for in all narrow vallies, where
rocks are discovered, we shall find the same beds of stone and marble on
both sides at the same height. In a country where I frequently reside, I
found a quarry of marble which extended more than 12 leagues in length,
and whose breadth was very considerable, although I have never been able
precisely to determine it. I have often observed that this bed of marble
is throughout of the same thickness, and in hills divided from this
quarry by a valley of 100 feet depth, and a quarter of a mile in
breadth, I found the same bed of marble at the same height. I am
persuaded it is the same in every stone and marble quarry where shells
are found; but this observation does not hold good in quarries of
freestone. In the course of this work, we shall give reasons for this
difference, and describe why freestone is not dispersed, like other
matters, in horizontal beds, and why it is in irregular blocks, both in
form and position.
We have likewise observed that the strata are the same on both sides the
straits of the sea. This observation, which is important, may lead us to
discover the lands and islands which have been separated from the
continent; it proves, for example, that England has been divided from
France; Spain from Africa; Sicily from Italy; and it is to be wished
that the same observation had been made in all the straits. I am
persuaded that we should find it almost every where true. We do not know
whether the same beds of stone are found at the same height on both
sides the straits of Magellan, which is the longest; but we see, by the
particular maps and exact charts, that the two high coasts which confine
it, form nearly, like the mountains of the earth, correspondent angles,
which also proves that the Terra del Fuega, must be regarded as part of
the continent of America; it is the same with Forbisher's Strait and
the island of Friesland, which appear to have been divided from the
continent of Greenland.
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