Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
Towards the middle of the twelfth century, the flood-waters of the
Po were retained on their left or northern side by dikes near the
small city of _Ficarolo_, which is about 19,000 _metres_[390] to
the north-west of Ferrara, spreading themselves southwards over
the northern part of the territory of Ferrara and the _Polesine_
of Rovigo, and flowed through the two formerly mentioned canals of
_Mazzorno_ and _Toi_. It seems perfectly ascertained, that this
change in the direction of the waters of the Po had been produced by
the effects of human labours; and the historians who have recorded
this remarkable fact only differ from each other in some of the
more minute details. The tendency of the river to flow in the new
channels, which had been opened for the more ready discharge of its
waters when in flood, continually increased; owing to which the
two ancient chief branches, the _Volano_ and _Primaro_, rapidly
decreased, and were reduced in less than a century to their present
comparatively insignificant size; while the main direction of the
river was established between the mouth of the Adige to the north,
and what is now called _Porto di Goro_, on the south. The two
before-mentioned canals of _Mazzorno_ and _Toi_ becoming insufficient
for the discharge, others were dug; and the principal mouth, called
_Bocco Tramontana_, or the northern mouth, having approached the
mouth of the Adige, the Venetians became alarmed in 1604; when they
excavated a new canal of discharge, named _Taglio de Porto Viro_, or
_Po delle Fornaci_, by which means the _Bocco Maestra_, was diverted
from the Adige towards the south.
During four centuries, from the end of the twelfth to that of the
sixteenth, the alluvial formations of the Po gained considerably upon
the sea. The northern mouth, which had usurped the situation of the
_Mazzorno_ canal, becoming the _Rama di Trimontana_, had advanced
in 1600 to the distance of 20,000 _metres_[391] from the meridian
of Adria; and the southern mouth, which had taken possession of
the canal of _Toi_, was then 17,000 _metres_[392] advanced beyond
the same point. Thus the shore had become extended nine or ten
thousand _metres_[393] to the north, and six or seven thousand to
the south[394]. Between these two mouths there was formerly a bay,
or a part of the coast less advanced than the rest, called _Sacca
di Goro_. During the same period of four hundred years previous to
the commencement of the seventeenth century, the great and extensive
embankments of the Po were constructed; and also, during the same
period, the southern slopes of the Alps began to be cleared and
cultivated.
Public-domain text, read in full here on John Shaqi.
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