An Introduction to the History of ScienceLibby, Walter
History
An Introduction to the History of Science
Libby, Walter
Science -- History
Hutton's imagination, on the basis of what can be observed to-day,
pictured the chemical and mechanical disintegration of the rocks; and
saw ice-streams bearing huge granite boulders from the declivities of
primitive and more gigantic Alps. He believed (as Desmarest) that
rivulets and rivers have constructed, and are constructing, their own
valley systems, and that the denudation ever in progress would be
eventually fatal to the sustenance of plant and animal and man, if the
earth were not a renewable organism, in which repair is correlative with
waste.
All strata are sedimentary, consolidated at the bottom of the sea by the
pressure of the water and by subterranean heat. How are strata raised
from the ocean bed? By the same subterranean force that helped
consolidate them. The power of heat for the expansion of bodies, is,
says Hutton (possibly having in mind the steam engine), so far as we
know, unlimited. We see liquid stone pouring from the crater of a lofty
volcano and casting huge rocks into mid-air, and yet find it difficult
to believe that Vesuvius and Etna themselves have been formed by
volcanic action. The interior of the planet may be a fluid mass, melted,
but unchanged by the action of heat. The volcanoes are spiracles or
safety-valves, and are widely distributed on the surface of the earth.
Hutton believed that basalt, and the whinstones generally, are of
igneous origin. Moreover, he put granite in the same category, and
believed it had been injected, as also metalliferous veins, in liquid
state into the stratified rocks. If his supposition were correct, then
granite would be found sending out veins from its large masses to pierce
the stratified rocks and to crop out where stratum meets stratum. His
conjecture was corroborated at Glen Tilt (and in the island of Arran).
Hutton was so elated at the verification of his view that the Scotch
guides thought he had struck gold, or silver at the very least. In the
bed of the river Tilt he could see at six points within half a mile
powerful veins of red granite piercing the black micaceous schist and
giving every indication of having been intruded from beneath, with great
violence, into the earlier formation.
Hutton felt confirmed in his view that in nature there is wisdom,
system, and consistency. Even the volcano and earthquake, instead of
being accidents, or arbitrary manifestations of divine wrath, are part
of the economy of nature, and the best clue we have to the stupendous
force necessary to heave up the strata, inject veins of metals and
igneous rocks, and insure a succession of habitable worlds.
In 1795 Dr. Hutton published a more elaborate statement of his theory in
two volumes. In 1802 Playfair printed _Illustrations of the Huttonian
Theory_, a simplification, having, naturally, little originality. Before
his death in 1797 Hutton devoted his time to reading new volumes by
Saussure on the Alps, and to preparing a book on _The Elements of
Agriculture_.
Public-domain text, read in full here on John Shaqi.
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