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
I descended, and found my friend beneath an overhanging rock.
Immediately afterwards a peal like that of thunder shook the air, and
right in front of us an avalanche darted down the brown cliffs, then
along a steep slope of snow which reared itself against the mountain
wall, carrying with it the debris of the rocks over which it passed,
until it finally lay a mass of sullied rubbish at the base of the
incline: the whole surface of the Talefre is thus soiled. Another peal
was heard immediately afterwards, but the avalanche which caused it was
hidden from us by a rocky promontory. From this same promontory the
greater portion of the medial moraine which descends the cascade of the
Talefre is derived, forming at first a gracefully winding curve, and
afterwards stretching straight to the summit of the fall. In the chasms
of the cascade its boulders are engulfed, but the lost moraine is
restored below the fall, as if disgorged by the ice which had swallowed
it. From the extremity of the Jardin itself a mere driblet of a moraine
proceeds, running parallel to the former, and like it disappearing at
the summit of the cascade.
[Sidenote: AMONG THE CREVASSES. 1857.]
We afterwards descended towards the cascade, but long before this is
attained the most experienced iceman would find himself in difficulty.
Transverse crevasses are formed, which follow each other so speedily as
to leave between them mere narrow ridges of ice, along which we moved
cautiously, jumping the adjacent fissures, or getting round them, as the
case demanded. As we approached the jaws of the gorge, the ridges
dwindled to mere plates and wedges, which being bent and broken by the
lateral pressure, added to the confusion, and warned us not to advance.
The position was in some measure an exciting one. Our guide had never
been here before; we were far from the beaten track, and the riven
glacier wore an aspect of treacherous hostility. As at the base of the
_seracs_, a subterranean noise sometimes announced the falling of
ice-blocks into hollows underneath, the existence of which the resonant
concussion of the fallen mass alone revealed. There was thus a dash of
awe mingled with our thoughts; a stirring up of the feelings which
troubled the coolness of the intellect. We finally swerved to the right,
and by a process the reverse of straightforward reached the Couvercle.
Nightfall found us at the threshold of our hotel.
FOOTNOTES:
[A] The recent hydraulic researches of Professor Magnus furnish some
beautiful illustrations of this action.
(10.)
[Sidenote: ROUND HAILSTONES. 1857.]
[Sidenote: A DANGEROUS LEAP. 1857.]
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account