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
_How the facts may be explained by assuming a uniform series of
changes._--The readiest way, perhaps, of persuading the reader that we
may dispense with great and sudden revolutions in the geological order
of events, is by showing him how a regular and uninterrupted series of
changes in the animate and inanimate world may give rise to such breaks
in the sequence, and such unconformability of stratified rocks, as are
usually thought to imply convulsions and catastrophes. It is scarcely
necessary to state, that the order of events thus assumed to occur, for
the sake of illustration, must be in harmony with all the conclusions
legitimately drawn by geologists from the structure of the earth, and
must be equally in accordance with the changes observed by man to be now
going on in the living as well as in the inorganic creation. It may be
necessary in the present state of science to supply some part of the
assumed course of nature hypothetically; but if so, this must be done
without any violation of probability, and always consistently with the
analogy of what is known both of the past and present economy of our
system. Although the discussion of so comprehensive a subject must carry
the beginner far beyond his depth, it will also, it is hoped, stimulate
his curiosity, and prepare him to read some elementary treatises on
geology with advantage, and teach him the bearing on that science of the
changes now in progress on the earth. At the same time it may enable him
the better to understand the intimate connection between the second and
third books of this work, the former of which is occupied with the
changes in the inorganic, the latter with those of the organic creation.
In pursuance, then, of the plan above proposed, I shall consider in this
chapter, first, what may be the course of fluctuation in the animate
world; secondly, the mode in which contemporaneous subterranean
movements affect the earth's crust; and, thirdly, the laws which
regulate the deposition of sediment.
UNIFORMITY OF CHANGE CONSIDERED FIRST IN REFERENCE TO THE LIVING
CREATION.
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