Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
I now come to the plan of uniting the _islands_, formed by these
early inhabitants. They availed themselves for that purpose of
all such parts of the sand-banks as lay in the intervals between
the large islands, and were beginning to produce grass. These,
when surrounded with dikes, are what are called _Hoogs_; and
their effects are to break the waves, thus diminishing their
action against the dikes of the large islands, and, at the same
time, to determine the accumulation of the mud in the intervals
between those islands. In this manner a large _marsch_ island,
named Everschop, was already, in 987, united to Eyderstede by the
point on which Poppenbull is situated; and in 995, the union of
the same _marsches_ was effected by another point, namely, that
of Tetenbull. Lastly, in the year 1000, Eyderstede received a
new increase by the course of the Hever, prolonged between the
sand banks, being fixed by a dike; but the whole still remained
an _island_. This is an example of the manner in which the
_marsch_ islands were united by the _hoogs_; and the chronicle of
the country says, that, by these labours, the islands were so
considerably enlarged in size, and the intervals between them so
much raised, that, at low water, it was possible to pass on foot
from one to the other. The extent of these _marsches_ was so great
on the coast of Sleswigh alone, that they were divided into three
provinces, two of which comprehended the islands, and the third
comprised the _marsches_ contiguous to the coast; and the same
works were carried on upon the _marsches_ of the coast of Holstein.
But the grounds thus gained from the sand-banks were very
insecure; these people, though they had inhabited them more than
ten centuries, had not yet understood the possibility of that
combination of fatal circumstances above described, against which
their dikes formed but a very feeble rampart; the North Sea, by the
extraordinary elevations of its level, being much more formidable
in this respect than the ocean, where the changes of absolute level
are much less considerable. I shall give an abridged account of the
particulars extracted by M. Hartz from the chronicle of Dankwerth,
relative to the great catastrophes which these _marsches_
successively underwent, previously to the time when experience led
to the means necessary for their security.
Public-domain text, read in full here on John Shaqi.
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