The Glaciers of the Alps: Being a narrative of excursions and ascents, an account of the origin and phenomena of glaciers and an exposition of the physical principles to which they are relatedTyndall, John
Science
The Glaciers of the Alps: Being a narrative of excursions and ascents, an account of the origin and phenomena of glaciers and an exposition of the physical principles to which they are related
Tyndall, John
Alps -- Description and travel; Glaciers -- Alps
[Sidenote: MOULIN OF GRINDELWALD GLACIER.]
[Sidenote: DEPTH OF THE SHAFT.]
The first time I had an opportunity of seeing these remarkable
glacier-chimneys was in the summer of 1856, upon the lower glacier of
Grindelwald. Mr. Huxley was my companion at the time, and on crossing
the so-called Eismeer we heard a sound resembling the rumble of distant
thunder, which proceeded from a perpendicular shaft formed in the ice,
and into which a resounding cataract discharged itself. The tube in fact
resembled a vast organ-pipe, whose thunder-notes were awakened by the
concussion of the falling water, instead of by the gentle flow of a
current of air. Beside the shaft our guide hewed steps, on which we
stood in succession, and looked into the tremendous hole. Near the first
shaft was a second and smaller one, the significance of which I did not
then understand; it was not more than 20 feet deep, but seemed filled
with a liquid of exquisite blue, the colour being really due to the
magical shimmer from the walls of the moulin, which was quite empty. As
far as we could see, the large shaft was vertical, but on dropping a
stone into it a shock was soon heard, and after a succession of bumps,
which occupied in all seven seconds, we heard the stone no more. The
depth of the moulin could not be thus ascertained, but we soon found a
second and still larger one which gave us better data. A stone dropped
into this descended without interruption for four seconds, when a
concussion was heard; and three seconds afterwards the final shock was
audible: there was thus but a single interruption in the descent.
Supposing all the acquired velocity to have been destroyed by the shock,
by adding the space passed over by the stone in four and in three
seconds respectively, and making allowance for the time required by the
sound to ascend from the bottom, we find the depth of the shaft to be
about 345 feet. There is, however, no reason to suppose that this
measures the depth of the glacier at the place referred to. These shafts
are to be found in almost all great glaciers; they are very numerous in
the Unteraar Glacier, numbers of them however being empty. On the Mer de
Glace they are always to be found in the region of Trelaporte, one of
the shafts there being, _par excellence_, called the Grand Moulin. Many
of them also occur on the Glacier de Lechaud.
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