Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
Things continued in this state for several centuries; during which
period, it is probable that the inhabitants of these lands were
often, by various catastrophes, disturbed in the enjoyment of them,
though not discouraged. But in 516, by which time these people were
become very numerous, more than 600 of them perished by one of the
concurrences of fatal circumstances already defined. It was then
that they undertook the astonishing enterprise of enclosing these
lands. They dug ditches around all the _marsches_, heaping up on
their exterior edge the earth which was taken out; and thus they
opposed to the sea, dikes of eight feet in height. After this,
comprehending that nothing could contribute more to the safety of
their dwellings, than to remove the sea to a greater distance,
they undertook, with that view, to exclude it from the intervals
between the islands, by uniting, as far as should be possible,
those islands with each other. I will describe the process by which
they effected this, after I shall have recalled to attention some
circumstances leading to it.
From all that I have already said of the _fore-lands_, and of the
manner in which they are increased, it may be understood, that
the common effects of the _waves_ and of the _tides_ is to bring
materials from the bottom of the sea towards the coasts; and
that the process continues in every state of the sea. The land
winds produce no _waves_ on the coasts, which can carry back to
the bottom of the sea what has been brought thence by the winds
blowing against the shore; and as for the _tides_, it may have
been already comprehended (and shall soon be proved), that the
_ebb_ carries back but very little of what has been brought by the
_flood_. So that, but for some extraordinary circumstances, the
materials continually impelled towards the shore, which first form
islands, would at last unite against the coast in a continuous
soil. The rare events, productive of great catastrophes, do not
carry back these materials towards the bottom of the sea; they
only, as it has been said before, ravage the surface, diminishing
the heights, and destroying the effect of vegetation. These, then,
were the effects against which it was necessary to guard.
Public-domain text, read in full here on John Shaqi.
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