Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
We know, from the testimony of Strabo, that Ravenna stood among
lagunes in the time of Augustus, as Venice does now; but at present
Ravenna is a league distant from the shore. Spina had been built by
the Greeks at the edge of the sea; yet in Strabo’s time it was ninety
stadia from it, and is now destroyed. Adria in Lombardy, which gave
name to the Adriatic sea, and of which it was, somewhat more than
twenty centuries ago, the principal port, is now six leagues distant
from it. Fortis has even rendered it probable that, at a more remote
period, the Euganian Mountains may have been islands.
M. de Prony, a learned member of the Institute, and inspector-general
of bridges and roads, has communicated to me some observations which
are of the greatest importance, as explaining those changes that
have taken place along the shores of the Adriatic[97]. Having been
directed by government to investigate the remedies that might be
applied to the devastations occasioned by the floods of the Po, he
ascertained that this river, since the period when it was shut in
by dikes, has so greatly raised the level of its bottom, that the
surface of its waters is now higher than the roofs of the houses in
Ferrara. At the same time, its alluvial depositions have advanced so
rapidly into the sea, that, by comparing old charts with the present
state, the shore is found to have gained more than six thousand
fathoms since 1604, giving an average of a hundred and fifty or a
hundred and eighty, and in some places two hundred feet yearly.
The Adige and the Po, are at the present day higher than the whole
tract of land that lies between them; and it is only by opening
new channels for them in the low grounds, which they have formerly
deposited, that the disasters which they now threaten may be averted.
The same causes have produced the same effects along the branches of
the Rhine and the Meuse; and thus the richest districts of Holland
have continually the frightful view of their rivers held up by
embankments at a height of from twenty to thirty feet above the level
of the land.
M. Wiebeking, director of bridges and highways in the kingdom of
Bavaria, has written a memoir upon this subject, so important as to
be worthy of being properly understood, both by the people and the
government, in all countries where these changes take place. In this
memoir, he shews that the property of raising the level of their beds
is common in a greater or less degree to all rivers.
Public-domain text, read in full here on John Shaqi.
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