Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
We say for the _last_ time, because, if we examine with still greater
care those remains of organised bodies, we discover, in the midst
of even the oldest strata of marine formation, other strata replete
with animal or vegetable remains of terrestrial or fresh-water
productions; and, amongst the more recent strata, or, in other
words, those that are nearest the surface, there are some in which
land animals are buried under heaps of marine productions. Thus, the
various catastrophes which have disturbed the strata, have not only
caused the different parts of our continents to rise by degrees from
the bosom of the waves, and diminished the extent of the basin of
the ocean, but have also given rise to numerous shiftings of this
basin. It has frequently happened, that lands which have been laid
dry, have been again covered by the waters, in consequence either
of their being ingulphed in the abyss, or of the sea having merely
risen over them. The particular portions also, of the Earth, which
the sea abandoned in its last retreat,--those which are now inhabited
by man and terrestrial animals,--had already been once laid dry,
and had then afforded subsistence to quadrupeds, birds, plants, and
land productions of all kinds: the sea which left it had, therefore,
covered it at a previous period[4].
The changes in the level of the waters have not, therefore, consisted
solely in a more or less gradual, or more or less general retreat;
there have been various successive irruptions and retreats, the final
result of which, however, has been a universal depression of the
level of the sea.
_Proofs that these Revolutions have been sudden._
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