Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
MM. Deluc and Dolomieu have most carefully examined the progress
of the formation of new ground by means of matters washed down by
rivers; and although exceedingly opposed to each other on many points
of the Theory of the Earth, they agree in this. These formations
augment very rapidly; they must have increased still more rapidly at
first, when the mountains furnished more materials to the rivers, and
yet their extent is still inconsiderable.
Dolomieu’s Memoir respecting Egypt[90] tends to prove, that the
tongue of land on which Alexander caused his city to be built,
did not exist in the days of Homer; that they were then able to
navigate directly from the island of Pharos into the gulf afterwards
called _Lake Mareotis_; and that this gulf was then, as indicated
by Menelaus, from fifteen to twenty leagues in length. It had,
therefore, only required the nine hundred years that elapsed between
the time of Homer and that of Strabo, to bring things to the state
in which this latter author describes them, and to reduce the gulf
in question to the form of a lake, of six leagues in length. It is
more certain, that, since that time, things have changed still more.
The sand thrown up by the sea and winds have formed, between the
island of Pharos and the site of ancient Alexandria, a tongue of land
two hundred fathoms in breadth, upon which the modern city has been
built. It has blocked up the nearest mouth of the Nile, and reduced
the lake Mareotis to almost nothing; while, during the same period,
the alluvial matter carried down by the Nile, has been deposited
along the rest of the shore, and has greatly increased its extent.
The ancients were not ignorant of these changes. Herodotus says,
that the Egyptian priests regarded their country as a gift of the
Nile. It is only in a manner, he adds, within a short period, that
the Delta has appeared[91]. Aristotle observes, that Homer speaks of
Thebes as if it had been the only great city in Egypt; and nowhere
makes mention of Memphis[92]. The Canopian and Pelusian mouths of
the Nile were formerly the principal ones; and the coast extended in
a straight line from the one to the other; and in this manner it
still appears in the charts of Ptolemy. Since then, the water has
been directed into the Bolbitian and Phatnitic mouths; and it is at
these entrances into the sea that the greatest depositions have been
formed, which have given the coast a semicircular outline. The cities
of Rosetta and Damieta, which were built upon these mouths, close
to the edge of the sea, less than a thousand years ago, are now two
leagues distant from it. According to Demaillet[93], it would only
have required twenty-six years to form a promontory of half a league
in extent before Rosetta.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account