Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
Mr Cuvier in the present work, and more recently in a note to Mr
Lemaire’s edition of Ovid’s Metamorphoses, enumerates the Mosaic,
Grecian, Assyrian, Persian, Indian, and Chinese traditions,
concerning a universal deluge; and concludes from them, that the
surface of the globe, five or six thousand years ago, underwent a
general and sudden revolution, by which the lands inhabited by the
human beings who lived at that time, and by the various species of
animals known at the present day, were overflowed by the ocean; out
of which emerged the present habitable portions of the globe. This
celebrated naturalist maintains, that these regions of the earth
were peopled by the few individuals who were preserved, and that the
tradition of the catastrophe has been preserved among these new races
of people, variously modified by the difference of their situation
and their social disposition. According to Mr Cuvier, similar
revolutions of nature had taken place, at periods long antecedent
to that of the Mosaic deluge. The dry land was inhabited, if not by
human beings, at least by land animals at an earlier period; and must
have been changed from the dry land to the bed of the ocean; and it
might even be concluded from the various species of animals contained
in it, that this change, as well as its opposite, had occurred more
than once.
This opinion being brought forward in a geognostic work, especially
in a work abounding in such valuable matters of fact, and stated
as the result of geognostic investigation, we may be permitted, in
this point of view, to examine it; and to ask, whether, from the
phenomena exhibited by the present condition of the earth’s surface,
we are entitled to conclude that it owes its conformation to such a
universal deluge.
We know, from arguments suggested by chemistry and the higher
mechanics, that the globe was once in a state of fluidity; hence it
might be maintained with some appearance of probability, that the
condition of the earth, previous to the existence of organic matter,
depended upon fusion; and that the primitive rocks are of igneous
origin. Since, however, granite has been found above rocks of various
kinds which contain the remains of organic bodies, we are under no
necessity of ascribing to primitive rocks an origin different from
that of subsequent formations; and, without having recourse to other
arguments, the fact, that aquatic animals are the most abundant of
fossil organic remains from the earliest of the transition to the
latest of the secondary and tertiary formations, affords evidence
that they are precipitates from water.
Public-domain text, read in full here on John Shaqi.
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