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
116. The cleft referred to, with its pillar, may be seen to the
right of the preceding engraving of the Mer de Glace. Below the cleft
is also seen the little glacier just referred to.
117. We may reach this cleft by a steep gully, visible from our
present position, and leading directly up to the cleft. But these
gullies, or couloirs, are very dangerous, being the pathways of
stones falling from the heights. We will therefore take the rocks
to the left of the gully, by close inspection ascertain their
assailable points, and there attack them. In the Alps as elsewhere
wonderful things may be done by looking steadfastly at difficulties,
and testing them wherever they appear assailable. We thus reach our
station, where the glory of the prospect, and the insight that we
gain as to the formation of the Mer de Glace, far more than repay us
for the labour of our ascent.
118. For we see the glacier below us, stretching its frozen tongue
downwards past the Montanvert. And we now find this single glacier
branching out into three others, some of them wider than itself.
Regard the branch to the right, the Glacier du Géant. It stretches
smoothly up for a long distance, then becomes disturbed, and then
changes to a great frozen cascade, down which the ice appears to
tumble in wild confusion. Above the cascade you see an expanse of
shining snow, occupying an area of some square miles.
§ 14. _Ice-cascade and Snows of the Col du Géant._
119. Instead of climbing to the height where we now stand, we might
have continued our walk upon the Mer de Glace, turned round the
promontory of Trélaporte, and walked right up the Glacier du Géant.
We should have found ice under our feet up to the bottom of the
cascade. It is not so compact as the ice lower down, but you would
not think of refusing to call it ice.
120. As we approach the fall, the smooth and unbroken character of
the glacier changes more and more. We encounter transverse ridges
succeeding each other with augmenting steepness. The ice becomes more
and more fissured and confused. We wind through tortuous ravines,
climb huge ice-mounds, and creep cautiously along crumbling crests,
with crevasses right and left. The confusion increases until further
advance along the centre of the glacier is impossible.
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