Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
The action of volcanoes is still more limited, and more local, than
any of those which have yet been mentioned. Although we have no
precise idea of the means by which nature keeps up these violent
fires at such great depths, we can judge decidedly, by their effects,
of the changes which they may have produced at the surface of the
globe. After a volcano has announced itself, by some shocks of an
earthquake, it forms for itself an opening. Stones and ashes are
thrown to a great distance, and lava is vomited forth. The more fluid
part of the lava flows in long streams, while the less fluid portion
stops at the edges of the opening, raises its margins all round, and
forms a cone, terminated by a crater. Thus volcanoes accumulate upon
the surface matters which were previously buried in the bowels of
the earth, after modifying their nature, and raise themselves into
mountains. By these means, they have formerly covered some parts of
our continent, and have also suddenly produced islands in the middle
of the sea. But these mountains and islands have always been composed
of lava, and all their materials have undergone the action of fire:
they are disposed as matters should be, which have flowed from an
elevated point. Volcanoes, therefore, neither raise nor overturn the
strata through which their apertures pass; and if some causes acting
from those depths have contributed, in certain cases, to raise up
large mountains, they cannot have been volcanic agents of the same
nature as those which exist at the present day.
* * * * *
Thus, we repeat, it is in vain that we search, among the powers
which now act at the surface of the earth, for causes sufficient
to produce the revolutions and catastrophes, the traces of which
are exhibited by its crust: And if we have recourse to the constant
external forces with which we are as yet acquainted, we shall have no
greater success.
_Constant Astronomical Causes._
The pole of the earth moves in a circle around the pole of the
ecliptic, and its axis is more or less inclined to the plane of
the ecliptic; but these two motions, the causes of which are now
ascertained, are much too limited for the production of effects like
those whose magnitude we have just been stating. At any rate, their
excessive slowness would render them altogether inadequate to account
for catastrophes which, as we have shewn, must have been sudden.
The same reasoning applies to all other slow motions which have been
conceived as causes of the revolutions in question, chosen doubtless
in the hope that their existence could not be denied, because it
might always be easy to hold out that their very slowness rendered
them imperceptible. But whether they be true or not is of little
importance, for they explain nothing, as no cause acting slowly could
have produced sudden effects.
Public-domain text, read in full here on John Shaqi.
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