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
But our hopes were doomed to disappointment. A vast quantity of snow
fell during the night, and, when we arose, we found the glacier covered,
and the air thick with the descending flakes. We waited, hoping that it
might clear up, but noon arrived and passed without improvement; our
fire-wood was exhausted, the weather intensely cold, and, according to
the men's opinion, hopelessly bad; they opposed the idea of ascending
further, and we had therefore no alternative but to pack up and move
downwards. What was snow at the higher elevations changed to rain lower
down, and drenched us completely before we reached the Grimsel. But
though thus partially foiled in our design, this visit taught us much
regarding the structure and general phenomena of the glacier.
[Sidenote: THE RHONE GLACIER. 1856.]
The morning of the 24th was clear and calm: we rose with the sun,
refreshed and strong, and crossed the Grimsel pass at an early hour. The
view from the summit of the pass was lovely in the extreme; the sky a
deep blue, the surrounding summits all enamelled with the newly-fallen
snow, which gleamed with dazzling whiteness in the sunlight. It was
Sunday, and the scene was itself a Sabbath, with no sound to disturb its
perfect rest. In a lake which we passed the mountains were mirrored
without distortion, for there was no motion of the air to ruffle its
surface. From the summit of the Mayenwand we looked down upon the Rhone
glacier, and a noble object it seemed,--I hardly know a finer of its
kind in the Alps. Forcing itself through the narrow gorge which holds
the ice cascade in its jaws, and where it is greatly riven and
dislocated, it spreads out in the valley below in such a manner as
clearly to reveal to the mind's eye the nature of the forces to which it
is subjected. Longfellow's figure is quite correct; the glacier
resembles a vast gauntlet, of which the gorge represents the wrist;
while the lower glacier, cleft by its fissures into finger-like ridges,
is typified by the hand.
Furnishing ourselves with provisions at the adjacent inn, we devoted
some hours to the examination of the lower portion of the glacier. The
dirt upon its surface was arranged in grooves as fine as if produced by
the passage of a rake, while the laminated structure of the deeper ice
always corresponded to the superficial grooving. We found several
shafts, some empty, some filled with water. At one place our attention
was attracted by a singular noise, evidently produced by the forcing of
air and water through passages in the body of the glacier; the sound
rose and fell for several minutes, like a kind of intermittent snore,
reminding one of Hugi's hypothesis that the glacier was alive.
[Sidenote: RINGS AROUND THE SUN. 1856.]
Public-domain text, read in full here on John Shaqi.
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