The Forms of Water in Clouds and Rivers, Ice and GlaciersTyndall, John
Science
The Forms of Water in Clouds and Rivers, Ice and Glaciers
Tyndall, John
Clouds; Glaciers; Ice; Rivers; Water
139. There is, in fact, no way that we can see of disposing of the
excess of snow above the snow-line; there is no way of making good
the constant waste of the ice below the snow-line; there is no way of
accounting for the medial moraines of the glacier, but by supposing
that from the highest snow-fields of the Col du Géant, the Léchaud,
and the Talèfre, to the extreme end of the Glacier des Bois, the
whole mass of frozen matter is moving downwards.
140. If you were older, it would give me pleasure to take you up
Mont Blanc. Starting from Chamouni, we should first pass through
woods and pastures, then up the steep hill-face with the Glacier des
Bossons to our right, to a rock known as the _Pierre Pointue_; thence
to a higher rock called the _Pierre l'Échelle_, because here a ladder
is usually placed to assist in crossing the chasms of the glacier.
At the Pierre l'Échelle we should strike the ice, and passing under
the Aiguille du Midi, which towers to the left, and which sometimes
sweeps a portion of the track with stone avalanches, we should cross
the Glacier des Bossons; amid heaped-up mounds and broken towers of
ice; up steep slopes; over chasms so deep that their bottoms are hid
in darkness.
141. We reach the rocks of the Grands Mulets, which form a kind
of barren islet in the icy sea; thence to the higher snow-fields,
crossing the _Petit Plateau_, which we should find cumbered by blocks
of ice. Looking to the right, we should see whence they came, for
rising here with threatening aspect high above us are the broken
ice-crags[B] of the Dôme du Goûté. The guides wish to pass this place
in silence, and it is just as well to humour them, however much you
may doubt the competence of the human voice to bring the ice-crags
down. From the Petit Plateau a steep snow-slope would carry us to the
Grand Plateau, and at day-dawn I know nothing in the whole Alps more
grand and solemn than this place.
[B] Named _séracs_ from their resemblance in shape and colour to an
inferior kind of curdy cheese called by this name at Chamouni.
142. One object of our ascent would be now attained; for here at the
head of the Grand Plateau, and at the foot of the final slope of Mont
Blanc, I should show you a great crevasse, into which three guides
were poured by an avalanche in the year 1820.
[Illustration: CREVASSE ON GRAND PLATEAU.]
143. Is this language correct? A crevasse hardly to be distinguished
from the present one undoubtedly existed here in 1820. But was it
the identical crevasse now existing? Is the ice riven here to-day
the same as that riven fifty-one years ago? By no means. How is this
proved? By the fact that more than forty years after their interment,
the remains of those three guides were found near the end of the
Glacier des Bossons, many miles below the existing crevasse.
Public-domain text, read in full here on John Shaqi.
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