Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of GeologyLyell, Charles, Sir
Science
Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of Geology
Lyell, Charles, Sir
Geology
Now, if it would be reasonable to draw such inferences with respect to
the future, we cannot but apply the same rules of induction to the
past. We have no right to anticipate any modifications in the results of
existing causes in time to come, which are not conformable to analogy,
unless they be produced by the progressive development of human power,
or perhaps by some other new relations which may hereafter spring up
between the moral and material worlds. In the same manner, when we
speculate on the vicissitudes of the animate and inanimate creation in
former ages, we ought not to look for any anomalous results, unless
where man has interfered, or unless clear indications appear of some
other _moral_ source of temporary derangement.
CHAPTER X.
SUPPOSED INTENSITY OF AQUEOUS FORCES AT REMOTE PERIODS.
Intensity of aqueous causes--Slow accumulation of strata proved by
fossils--Rate of denudation can only keep pace with
deposition--Erratics, and effects of ice--Deluges, and the causes to
which they are referred--Supposed universality of ancient deposits.
_Intensity of aqueous causes._--The great problem considered in the
preceding chapters, namely, whether the former changes of the earth made
known to us by geology, resemble in kind and degree those now in daily
progress, may still be contemplated from several other points of view.
We may inquire, for example, whether there are any grounds for the
belief entertained by many, that the intensity both of aqueous and of
igneous forces, in remote ages, far exceeded that which we witness in
our own times.
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