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 subsequently spent several hours upon the glacier; and on this day I
noticed for the first time a contemporaneous exhibition of _bedding_ and
_structure_ to which I shall refer at another place. We passed finally
to the left bank of the glacier, at some distance below the base of the
AEggischhorn, and traced its old moraines at intervals along the flanks
of the bounding mountain. At the summit of the ridge we found several
fine old _roches moutonnees_, on some of which the scratchings of a
glacier long departed were well preserved; and from the direction of the
scratchings it might be inferred that the ice moved down the mountain
towards the valley of the Rhone. A plunge into a lonely mountain lake
ended the day's excursion.
[Sidenote: END OF THE ALETSCH GLACIER. 1858.]
On the 7th of August we quitted this noble station. Sending our guide on
to Viesch to take a conveyance and proceed with our luggage down the
valley, Ramsay and myself crossed the mountains obliquely, desiring to
trace the glacier to its termination. We had no path, but it was hardly
possible to go astray. We crossed spurs, climbed and descended pleasant
mounds, sometimes with the soft grass under our feet, and sometimes
knee-deep in rhododendrons. It took us several hours to reach the end of
the glacier, and we then looked down upon it merely. It lay couched like
a reptile in a wild gorge, as if it had split the mountain by its frozen
snout. We afterwards descended to Moerill, where we met our guide and
driver; thence down the valley to Visp; and the following evening saw us
lodged at the Monte Rosa hotel in Zermatt.
The boiling point of water on the table of the _salle a manger_, I found
to be 202.58 deg. Fahr.
[Sidenote: MEADOWS INVADED BY ICE. 1858.]
On the following morning I proceeded without my friend to the Goerner
glacier. As is well known, the end of this glacier has been steadily
advancing for several years, and when I saw it, the meadow in front of
it was partly shrivelled up by its irresistible advance. I was informed
by my host that within the last sixty years forty-four chalets had been
overturned by the glacier, the ground on which they stood being occupied
by the ice; at present there are others for which a similar fate seems
imminent. In thus advancing the glacier merely takes up ground which
belonged to it in former ages, for the rounded rocks which rise out of
the adjacent meadow show that it once passed over them.
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