Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
Bare rocks cannot be made subservient to the purposes of agriculture.
Lichens indeed, cover the surface of rocks, deriving their chief
nutriment from the atmosphere; mosses draw the water necessary for
their subsistence from the fissures of stones; the roots of grasses
seek in the chinks of rocks for particles of earth sufficient for
their sustenance; various shrubs and trees penetrate here and there
into rocky masses by their roots (having the powerful and continued
action of living wedges), where the cohesion of the parts is
smallest, in order to prepare a fixed seat for themselves, and be
secure from the pernicious effects of the atmosphere. The surface of
the earth is always sterile, however, when it shows a continuity of
naked rock, uncovered by vegetable mould. The cultivation of fields
and woods, and even the rearing of cattle, cannot therefore find
scope in regions which are entirely rocky. Abrupt and precipitous
mountains being generally in this condition are usually barren; but
in plains and on declivities, a bare rocky surface is much less
frequently the cause of sterility than an unfavourable proportion
of mould. Some rocky and moderately elevated regions also occur,
more or less destitute of vegetable mould, whose sterility depends
upon volcanic causes. Iceland, for example, affords cases of this
description. In many parts of Sweden, as in Westrogothia, in
Scotland, &c., there occur many elevated regions, in which gneiss
and granite predominating, exclude to a great extent all kinds of
vegetation excepting lichens. In the same districts we sometimes meet
with pastures and corn-fields interrupted here and there by bare
rocks rising but little above the surface, by which the value of
the ground is much diminished, and great impediments opposed to its
cultivation.
As bare rocks are incapable of all cultivation, their distance
from the under surface of vegetable mould must also be of great
importance. In the plains of the north of Germany, for example, this
distance is often so great that a rocky surface is never found,
while, on the contrary, in other countries, especially such as are
mountainous, the roots of plants not unfrequently touch the subjacent
rock; the variation between these extremes being of all degrees. The
effect of the distance of the surface of the solid rock from the
under surface of productive soil may be both _direct_ and _indirect_,
and may vary much, not only with reference to the species of rock,
but also to the vegetables.
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