A Manual of Elementary Geology: or, The Ancient Changes of the Earth and its Inhabitants as Illustrated by Geological MonumentsLyell, Charles, Sir
Science
A Manual of Elementary Geology: or, The Ancient Changes of the Earth and its Inhabitants as Illustrated by Geological Monuments
Lyell, Charles, Sir
Geology
We may often observe in our ponds the _Phryganea_ (or Caddis-fly), in its
caterpillar state, covered with small freshwater shells, which they have
the power of fixing to the outside of their tubular cases, in order,
probably, to give them weight and strength. The individual figured in the
annexed cut, which belongs to a species very abundant in England, has
covered its case with shells of a small _Planorbis_. In the same manner a
large species of caddis-worm, which swarmed in the Eocene lakes of
Auvergne, was accustomed to attach to its dwelling the shells of a small
spiral univalve of the genus _Paludina_. A hundred of these minute shells
are sometimes seen arranged around one tube, part of the central cavity of
which is often empty, the rest being filled up with thin concentric layers
of travertin. The cases have been thrown together confusedly, and often
lie, as in fig. 161., at right angles one to the other. When we consider
that ten or twelve tubes are packed within the compass of a cubic inch, and
that some single strata of this limestone are 6 feet thick, and may be
traced over a considerable area, we may form some idea of the countless
number of insects and mollusca which contributed their integuments and
shells to compose this singularly constructed rock. It is unnecessary to
suppose that the _Phryganeae_ lived on the spots where their cases are now
found; they may have multiplied in the shallows near the margin of the
lake, or in the streams by which it was fed, and their cases may have been
drifted by a current far into the deep water.
In the summer of 1837, when examining, in company with Dr. Beck, a small
lake near Copenhagen, I had an opportunity of witnessing a beautiful
exemplification of the manner in which the tubular cases of Auvergne were
probably accumulated. This lake, called the Fuure-Soe, occurring in the
interior of Seeland, is about twenty English miles in circumference, and in
some parts 200 feet in depth. Round the shallow borders an abundant crop of
reeds and rushes may be observed, covered with the indusiae of the
_Phryganea grandis_ and other species, to which shells are attached. The
plants which support them are the bullrush, _Scirpus lacustris_, and common
reed, _Arundo phragmitis_, but chiefly the former. In summer, especially in
the month of June, a violent gust of wind sometimes causes a current by
which these plants are torn up by the roots, washed away, and floated off
in long bands, more than a mile in length, into deep water. The _Cypris_
swarms in the same lake; and calcareous springs alone are wanting to form
extensive beds of indusial limestone, like those of Auvergne.
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