Theory of the Earth, With Proofs and Illustrations, Volume 1 (of 4)Hutton, James
Science
Theory of the Earth, With Proofs and Illustrations, Volume 1 (of 4)
Hutton, James
Geology -- Early works to 1800
Let us examine places much more exposed to the fury of the waves and
currents than the coast of Carthagena, the narrow fretum, for example,
between Italy and Sicily. It does not appear, that this passage is
sensibly wider than when the Romans first had known it. The Isthmus of
Corinth is also apparently the same at present as it had been two or
three thousand years ago. Scilla and Charibdis remain now, as they had
been in ancient times, rocks hazardous for coasting vessels which had to
pass that strait.
It is not meant by this to say, these rocks have not been wasted by the
sea, and worn by the attrition of moving bodies, during that space of
time; were this true, and that those rocks, the bulwarks of the land
upon those coasts, had not been at all impaired from that period, they
might remain for ever, and thus the system of interchanging the place of
sea and land upon this globe might be frustrated. It is only meant
to affirm, that the quantity which those rocks, or that coast, have
diminished from the period of our history, has either been too small
a thing for human observation, or, which is more probable, that no
accurate measurement of the subject, by which this quantity of decrease
might have been ascertained, had been taken and recorded. It must be
also evident, that a very small operation of an earthquake would be
sufficient to render every means of information, in this manner of
mensuration, unsatisfactory or precarious.
Pliny says Italy was distant from Sicily a mile and a half; but we
cannot suppose that this measure was taken any otherwise than by
computation, and such a measure is but little calculated to afford us
the just means of a comparison with the present distance. He also says,
indeed, that Sicily had been once joined with Italy. His words are:
"Quondam Brutio agro cohaerens, mox interfuso mari avulsa.[18]" But all
that we can conclude from this history of Pliny is, that, in all times,
to people considering the appearances of those two approached coasts,
it had seemed probable, that the sea formed a passage between the two
countries which had been once united; in like manner as is still more
immediately perceived, in that smaller disjunction which is made between
the island of Anglesey and the continent of Wales.
[Note 18: Lib. 3. cap. 8.]
Public-domain text, read in full here on John Shaqi.
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