Buffon's Natural History, Volume 02 (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 02 (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
For supposing that the chain of the highest mountains which cross
South America from the Magellanic lands to New Grenada, and the Gulph
of Darien, had been produced by an earthquake, and then let us see by
calculations the effect of this explosion. This chain of mountains is
near 1700 leagues in length, and commonly 40 in breadth, comprehending
the Sieras, which are not so lofty as the Andes. The surface therefore
is 68,000 square leagues; I suppose the thickness of the matter
displaced by the earthquake to be about one league, that is, the
height of these mountains taken from the top to the caverns, which
according to this hypothesis must support them, is one league, then I
say, the power of an explosion must have raised a quantity of earth
equal to 68,000 cubical leagues to a league in height. Now the action
being equal to the re-action, this explosion must have communicated
the same motion to the rest of the globe. The whole globe consists of
12,310,523,801 cubical leagues, from which subtracting 68,000, there
remains 12,310,455,801 cubical leagues, the quantity of which motion
will be equal to that of 68,000 cubical leagues raised one league; from
whence we perceive that the force which will have been great enough to
elevate 68,000 cubical leagues would not have displaced the whole globe
a single inch.
There would therefore be no absolute impossibility in the supposition
that mountains have been raised by earthquakes, if their internal
composition as well as their external form were not evident proofs of
their being the work of the sea. Their internal parts are composed
of regular and parallel strata, intermingled with shells, and
their external consists of a figure whose angles are every where
correspondent: is it credible then that this uniform composition and
regular form should have been produced by irregular shocks and sudden
explosions?
But as this opinion has prevailed among some philosophers, and as the
nature and effects of earthquakes are not well understood, it may
possibly be pertinent to hazard a few ideas with a view of explaining
those intricate subjects.
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