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 — John Shaqi
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
The hail ceased and the heights above us cleared as we ascended. At the
top of the pass we found ourselves on the verge of a great _neve_, which
lay between two ranges of summits, sloping down to the base of each
range from a high and rounded centre: a wilder glacier scene I have
scarcely witnessed. Wishing to obtain a more perfect view of the region,
I diverged from the track followed by Dr. Frankland and the guide, and
climbed a ridge of snow about half a mile to the right of them. A
glorious expanse was before me, stretching itself in vast undulations,
and heaping itself here and there into mountainous cones, white and
pure, with the deep blue heaven behind them. Here I had my first
experience of hidden crevasses, and to my extreme astonishment once
found myself in the jaws of a fissure of whose existence I had not the
slightest notice. Such accidents have often occurred to me since, but
the impression made by the first is likely to remain the strongest. It
was dark when we reached the wretched Wirthshaus at Fend, where, badly
fed, badly lodged, and disturbed by the noise of innumerable rats, we
spent the night. Thus ended my brief glacier expedition of 1856; and on
the observations then made, and on subsequent experiments, was founded a
paper presented to the Royal Society by Mr. Huxley and myself.[B]
FOOTNOTES:
[A] I take the following account of a grander storm of the above
character from Hooker's 'Himalayan Journals,' vol. ii. p. 405.
"On the 20th (March, 1849) we had a change in the weather: a violent
storm from the south-west occurred at noon, with hail of a strange form,
the stones being sections of hollow spheres, half an inch across and
upwards, formed of cones with truncated apices and convex bases: these
cones were aggregated together with their bases outwards. The large
masses were followed by a shower of the separate conical pieces, and
that by heavy rain. On the mountains this storm was most severe: the
stones lay at Darjeeling for seven days, congealed into masses of ice
several feet long and a foot thick in sheltered places: at Purneah,
fifty miles south, stones one and two inches across fell, probably as
whole spheres."
[B] 'Phil. Trans.' 1857, pp. 327-346.--L. C. T.
[Sidenote: THE LAKE OF GENEVA. 1857.]
EXPEDITION OF 1857.
THE LAKE OF GENEVA.
(4.)
The time occupied in the observations of 1856 embraced about five whole
days; and though these days were laborious and instructive, still so
short a time proved to be wholly incommensurate with the claims of so
wide a problem. During the subsequent experimental treatment of the
subject, I had often occasion to feel the incompleteness of my
knowledge, and hence arose the desire to make a second expedition to the
Alps, for the purpose of expanding, fortifying, or, if necessary,
correcting first impressions.
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