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
might suit a purely spiritual essence, they are not congenial to flesh
and blood, and you gladly escape from its magnificence to the sunshine
of the world above.
[Sidenote: BIRTH OF A CREVASSE.]
From their numbers it might be inferred that the formation of crevasses
is a thing of frequent occurrence and easy to observe; but in reality it
is very rarely observed. Simond was a man of considerable experience
upon the ice, but the first crevasse he ever saw formed was during the
setting out of one of our lines, when a narrow rent opened beneath his
feet, and propagated itself through the ice with loud cracking for a
distance of 50 or 60 yards. Crevasses always commence in this way as
mere narrow cracks, which open very slowly afterwards. I will here
describe the only case of crevasse-forming which has come under my
direct observation.
On the 31st of July, 1857, Mr. Hirst and myself, having completed our
day's work, were standing together upon the Glacier du Geant, when a
loud dull sound, like that produced by a heavy blow, seemed to issue
from the body of the ice underneath the spot on which we stood. This was
succeeded by a series of sharp reports, which were heard sometimes above
us, sometimes below us, sometimes apparently close under our feet, the
intervals between the louder reports being filled by a low singing
noise. We turned hither and thither as the direction of the sounds
varied; for the glacier was evidently breaking beneath our feet, though
we could discern no trace of rupture. For an hour the sounds continued
without our being able to discover their source; this at length revealed
itself by a rush of air-bubbles from one of the little pools upon the
surface of the glacier, which was intersected by the newly-formed
crevasse. We then traced it for some distance up and down, but hardly at
any place was it sufficiently wide to permit the blade of my penknife to
enter it. M. Agassiz has given an animated description of the terror of
his guides upon a similar occasion, and there was an element of awe in
our own feelings as we heard the evening stillness of the glacier thus
disturbed.
[Sidenote: MECHANICAL ORIGIN.]
With regard to the mechanical origin of the crevasses the most vague and
untenable notions had been entertained until Mr. Hopkins published his
extremely valuable papers. To him, indeed, we are almost wholly indebted
for our present knowledge of the subject, my own experiments upon this
portion of the glacier-question being for the most part illustrations of
the truth of his reasoning. To understand the fissures in their more
complex aspects it is necessary that we should commence with their
elements. I shall deal with the question in my own way, adhering,
however, to the mechanical principles upon which Mr. Hopkins has based
his exposition.
[Illustration: Fig. 25. Diagram explanatory of the mechanical origin of
Crevasses.]
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