Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of Geology — John Shaqi
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
To begin with the northern hemisphere. Let us suppose those hills of the
Italian peninsula and of Sicily, which are of comparatively modern
origin, and contain many fossil shells identical with living species, to
subside again into the sea, from which they have been raised, and that
an extent of land of equal area and height (varying from one to three
thousand feet) should rise up in the Arctic Ocean between Siberia and
the north pole. In speaking of such changes, I shall not allude to the
manner in which I conceive it possible that they may be brought about,
nor of the time required for their accomplishment--reserving for a
future occasion, not only the proofs that revolutions of equal magnitude
have taken place, but that analogous operations are still in gradual
progress. The alteration now supposed in the physical geography of the
northern regions, would cause additional snow and ice to accumulate
where now there is usually an open sea; and the temperature of the
greater part of Europe would be somewhat lowered, so as to resemble more
nearly that of corresponding latitudes of North America: or, in other
words, it might be necessary to travel about 10° farther south in order
to meet with the same climate which we now enjoy. No compensation would
be derived from the disappearance of land in the Mediterranean
countries; but the contrary, since the mean heat of the soil in those
latitudes probably exceeds that which would belong to the sea, by which
we imagine it to be replaced.
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