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
We made the Grimsel our station for a day, which was spent in examining
the evidences of ancient glacier action in the valley of Hasli. Near the
Hospice, but at the opposite side of the Aar, rises a mountain-wall of
hard granite, on which the flutings and groovings are magnificently
preserved. After a little practice the eye can trace with the utmost
precision the line which marks the level of the ancient ice: above this
the crags are sharp and rugged; while below it the mighty grinder has
rubbed off the pinnacles of the rocks and worn their edges away. The
height to which this action extends must be nearly two thousand feet
above the bed of the present valley. It is also easy to see the depth to
which the river has worked its channel into the ancient rocks. In some
cases the road from Guttanen to the Grimsel lay right over the polished
rocks, asperities being supplied by the chisel of man in order to
prevent travellers from slipping on their slopes. Here and there also
huge protuberant crags were rounded into domes almost as perfect as if
chiselled by art. To both my companion and myself this walk was full of
instruction and delight.
On the 28th of July we crossed the Grimsel pass, and traced the
scratchings to the very top of it. Ramsay remarked that their direction
changed high up the pass, as if a tributary from the summit had produced
them, while lower down they merged into the general direction of the
glacier which had filled the principal valley. From the summit of the
Mayenwand we had a clear view of the glacier of the Rhone; and to see
the lower portion of this glacier to advantage no better position can be
chosen. The dislocation of its cascade, the spreading out of the ice
below, its system of radial crevasses, and the transverse sweep of its
structural groovings, may all be seen. A few hours afterwards we were
among the wild chasms at the brow of the ice-fall, where we worked our
way to the centre of the ice, but were unable to attain the opposite
side.
Having examined the glacier both above and below the cascade, we went
down the valley to Viesch, and ascended thence, on the 30th of July, to
the Hotel Jungfrau on the slopes of the AEggischhorn. On the following
day we climbed to the summit of the mountain, and from a sheltered nook
enjoyed the glorious prospect which it commands. The wind was strong,
and fleecy clouds flew over the heavens; some of which, as they formed
and dispersed themselves about the flanks of the Aletschhorn, showed
extraordinary iridescences.
[Sidenote: THE MAeRJELEN SEE. 1858.]
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