The Forms of Water in Clouds and Rivers, Ice and GlaciersTyndall, John
Science
The Forms of Water in Clouds and Rivers, Ice and Glaciers
Tyndall, John
Clouds; Glaciers; Ice; Rivers; Water
205. The width of the Glacier de Léchaud we find to be 3,725 links,
or 825 yards.
206. The width of the Talèfre we find to be 2,900 links, or 638 yards.
207. The sum of the widths of the three branch glaciers is therefore
2,597 yards.
208. At Trélaporte these three branches are forced through a gorge
893 yards wide, or one-third of their previous width, at the rate of
twenty inches a day.
209. If we limit our view to the Glacier de Léchaud, the facts are
still more astonishing. Previous to its junction with the Talèfre,
this glacier has a width of 825 yards; in passing through the jaws of
the granite vice at Trélaporte, its width is reduced to eighty-eight
yards, or in round numbers to one-tenth of its previous width. (Look
to the sketch on the next page.)
[Illustration: SKETCH-PLAN SHOWING THE MORAINES, _a_, _b_, _c_, _d_,
_e_, OF THE MER DE GLACE.]
210. Are we to understand by this that the ice of the Léchaud is
squeezed to one-tenth of its former _volume_? By no means. It is
mainly a change of _form_, not of volume, that occurs at Trélaporte.
Previous to its compression, the glacier resembles a plate of ice
_lying flat_ upon its bed. After its compression, it resembles a
plate _fixed upon its edge_. The squeezing, doubtless, has deepened
the ice.
§ 30. _Longitudinal Compression of a Glacier._
211. The ice is forced through the gorge at Trélaporte by a pressure
from behind; in fact the Glacier du Géant, immediately above
Trélaporte, represents a piston or a plug which drives the ice
through the gorge. What effect must this pressure have upon the plug
itself? Reasoning alone renders it probable that the pressure will
shorten the plug; that the lower part of the Glacier du Géant will to
some extent yield to the pressure from behind.
212. Let us test this notion. About three-quarters of a mile above
the Tacul, and on the mountain slope to the left as we ascend, we
observe a patch of verdure. Thither we climb; there we plant our
theodolite, and set out across the Glacier du Géant, a line, which we
will call line No. 1 (F F' upon sketch, p. 68).
213. About a quarter of a mile lower down we find a practicable
couloir on the mountain side; we ascend it, reach a suitable
platform, plant our instrument, and set out a second line, No. 2 (G
G' upon sketch). We must hasten our work here, for along this couloir
stones are discharged from a small glacier which rests upon the slope
of Mont Tacul.
214. Still lower down by another quarter of a mile, which brings us
near the Tacul, we set out a third line, No. 3 (H H' upon sketch),
across the glacier.
215. The daily motion of the centres of these three lines is as
follows:--
Inches Distances asunder
No. 1 50·55 }
} 545 yards.
No. 2 15·43 }
} 487 "
No. 3 12·75 }
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