Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
many other geognostic appearances, time rather than force is to be
taken into account. Another circumstance, perhaps, corresponds with
this, that the change produced by the weather, not only by the first
disunion, but also by the progressive disintegration of the rocks,
by the blunting of the edges and corners, by the diminution of the
fragments, and generally in the origin of the boulders and fragments
of rocks of every description, has just as much influence as the
mechanical operation of the water; and that a great part of the land
called Alluvial, generally owes its existence to this cause[404]. But
if, upon farther consideration, the conglomerates appear to derive
their origin in a similar way with rolled masses of gravel, they
afford evidence, nevertheless, of the elevated station of the water
in the neighbourhood, from which they had been before removed; for
their conglomeration could take place only under water; and, with few
exceptions, they occupy an incomparably greater elevation than any of
the coal formations, or any of the beds of rocks which enclose the
remains of land animals.
Geognosy certainly contains many facts, which cannot be explained,
but by a change from dry land to the bottom of the sea, although our
knowledge of them is still so imperfect, that we cannot hazard a
probable conjecture respecting the numbers of these changes, whether
they commence at the same or at different periods in the various
quarters of the world, and whether they are local or universal.
These changes appear neither sudden nor violent, such as we consider
revolutions of the earth, but at all times proceed with silent and
regular steps, and depend upon similar causes, concealed it is true
from us, such as the universal retreat of the waters from their
original height to the present bed of the ocean. We do not belong to
those geologists who divert the world from its axis for the purpose
of explaining the inequalities of its surface, at whose command the
Earth sometimes opens her bosom to engulf the sea, and at other times
the floodgates of Heaven are lifted up to pour down another ocean.
He who reflects on the devastation caused by earthquakes, inundations
and the fall of mountains, even though they are merely local
appearances confined to particular quarters, cannot help putting
the question to himself, how the order, regularity and connection
exhibited by strata of rocks, could in any measure exist, if the same
or similar accidents had happened throughout the whole world, and
if mechanical power had operated with such energy, and to such an
extent? All our knowledge of the structure of the earth, and of the
existence of its inhabitants, declares rather a quiet uninterrupted
and continually progressive advancement in its formation and
development.
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