Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
The different conditions of rocks with regard to caloric, may have
some indirect influence upon the vigour of plants. Heat, whether
imparted to the vegetable soil by the sun’s rays, or generated by
various chemical processes in the earth itself, penetrates to the
surface of the subjacent rocks, and is more or less drawn from it in
a longer or shorter time. Columella observes, that rocks in the upper
part of the soil are prejudicial to vines and trees, but in the lower
part cool them. The heat of soil will be more or less drawn from it,
according to the greater or less conducting power of the subjacent
rock. Compact crystalline rocks are probably better conductors of
caloric than those which are of looser texture; siliceous rocks than
argillaceous and calcareous ones. The influence of the subjacent rock
must be greater in this respect, in proportion to the thinness of the
superincumbent soil. The effect of the abduction of caloric is more
particularly sensible, where the roots of cultivated plants touch
the rock, a circumstance which we often see in vineyards. The vine
frequently thrives remarkably on the declivities of mountains, in
which it sends its roots among fragments of stones. Experience shows,
that the quality of wine is influenced by the different conditions
of the stones, among which vines are planted. Albertus Magnus has
observed, that the vine thrives well in earth which is mixed with
fragments of black roofing slate; and Humboldt remarks, that the
vines which grow upon the mountains of the valley of the Rhine,
consisting of black clay-slate, afford an excellent wine. At the Cape
of Good Hope, also, the vine thrives well in a soil produced by the
decomposition of clay-slate, and mixed with fragments of it[413].
It is probable, that the adaptation of this sort of soil to the
cultivation of the vine, depends upon its slow conducting power, and
upon its rapidly imbibing the rays of the sun, on account of its dark
colour, and thus increasing the heat of the ground.
Hitherto we have only spoken of the _proximate_ influence of rocks
upon plants; but it cannot be denied, that the _remote_ effects which
they produce, (inasmuch as vegetable soil is derived from them, and,
therefore, the qualities of this soil depend in a great measure upon
their nature,) are of greater importance.
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