On the Old Road, Vol. 2 (of 2): A Collection of Miscellaneous Essays and Articles on Art and LiteratureRuskin, John
General
On the Old Road, Vol. 2 (of 2): A Collection of Miscellaneous Essays and Articles on Art and Literature
Ruskin, John
Art; Essays; Literature
296. III. _Sculpture._--The final reductions of mountainform are owing
either to disintegration, or to the action of water, in the condition of
rain, rivers, or ice, aided by frost and other circumstances of
temperature and atmosphere.
All important existing forms are owing to disintegration, or the action
of water. That of ice had been curiously over-rated. As an instrument of
sculpture, ice is much less powerful than water; the apparently
energetic effects of it being merely the exponents of disintegration. A
glacier did not produce its moraine, but sustained and exposed the
fragments which fell on its surface, pulverizing these by keeping them
in motion, but producing very unimportant effects on the rock below; the
roundings and striation produced by ice were superficial; while a
torrent penetrated into every angle and cranny, undermining and wearing
continually, and carrying stones, at the lowest estimate, six hundred
thousand times as fast as the glacier. Had the quantity of rain which
has fallen on Mont Blanc in the form of snow (and descended in the
ravines as ice) fallen as rain, and descended in torrents, the ravines
would have been much deeper than they are now, and the glacier may so
far be considered as exercising a protective influence. But its power of
carriage is unlimited, and when masses of earth or rock are once
loosened, the glacier carries them away, and exposes fresh surfaces.
Generally, the work of water and ice is in mountain surgery like that of
lancet and sponge--one for incision, the other for ablution. No
excavation by ice was possible on a large scale, any more than by a
stream of honey; and its various actions, with their limitations, were
only to be understood by keeping always clearly in view the great law of
its motion as a viscous substance, determined by Professor James Forbes.
Public-domain text, read in full here on John Shaqi.
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