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
Although Pythagoras is introduced by the poet as delivering his doctrine
in person, some of the illustrations are derived from natural events
which happened after the death of the philosopher. But notwithstanding
these anachronisms, we may regard the account as a true picture of the
tenets of the Pythagorean school in the Augustan age; and although
perhaps partially modified, it must have contained the substance of the
original scheme. Thus considered, it is extremely curious and
instructive; for we here find a comprehensive summary of almost all the
great causes of change now in activity on the globe, and these adduced
in confirmation of a principle of a perpetual and gradual revolution
inherent in the nature of our terrestrial system. These doctrines, it is
true, are not directly applied to the explanation of geological
phenomena; or, in other words, no attempt is made to estimate what may
have been in past ages, or what may hereafter be, the aggregate amount
of change brought about by such never-ending fluctuations. Had this been
the case, we might have been called upon to admire so extraordinary an
anticipation with no less interest than astronomers, when they endeavor
to define by what means the Samian philosopher came to the knowledge of
the Copernican system.
Let us now examine the celebrated passages to which we have been
adverting:[13]
"Nothing perishes in this world; but things merely vary and change their
form. To be born, means simply that a thing begins to be something
different from what it was before; and dying, is ceasing to be the same
thing. Yet, although nothing retains long the same image, the sum of the
whole remains constant." These general propositions are then confirmed
by a series of examples, all derived from natural appearances, except
the first, which refers to the golden age giving place to the age of
iron. The illustrations are thus consecutively adduced.
1. Solid land has been converted into sea.
2. Sea has been changed into land. Marine shells lie far distant from
the deep, and the anchor has been found on the summit of hills.
3. Valleys have been excavated by running water, and floods have washed
down hills into the sea.[14]
4. Marshes have become dry ground.
5. Dry lands have been changed into stagnant pools.
6. During earthquakes some springs have been closed up, and new ones
have broken out. Rivers have deserted their channels, and have been
re-born elsewhere, as the Erasinus in Greece, and Mysus in Asia.
7. The waters of some rivers, formerly sweet, have become bitter; as
those of the Anigris, in Greece, &c.[15]
8. Islands have become connected with the mainland by the growth of
deltas and new deposits; as in the case of Antissa joined to Lesbos,
Pharos to Egypt, &c.
9. Peninsulas have been divided from the main land, and have become
islands, as Leucadia; and according to tradition, Sicily, the sea having
carried away the isthmus.
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