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
121. But with the aid of an axe to cut steps in the steeper ice-walls
and slopes we might, by swerving to either side of the glacier, work
our way to the top of the cascade. If we ascended to the right,
we should have to take care of the ice avalanches which sometimes
thunder down the slopes; if to the left, we should have to take care
of the stones let loose from the Aiguille Noire. After we had cleared
the cascade, we should have to beware for a time of the crevasses,
which for some distance above the fall yawn terribly. But by caution
we could get round them, and sometimes cross them by bridges of snow.
Here the skill and knowledge to be acquired only by long practice
come into play; and here also the use of the Alpine rope suggests
itself. For not only are the 'snow bridges often frail, but whole
crevasses are sometimes covered, the unhappy traveller being first
made aware of their existence by the snow breaking under his feet.
Many lives have thus been lost, and some quite recently.
122. Once upon the plateau above the ice-fall we find the surface
totally changed. Below the fall we walked upon ice; here we are
upon snow. After a gentle but long ascent we reach a depression of
the ridge which bounds the snow-field at the top, and now look over
Italy. We stand upon the famous Col du Géant.
123. They were no idle scamperers on the mountains that made these
wild recesses first known; it was not the desire for health which
now brings some, or the desire for grandeur and beauty which brings
others, or the wish to be able to say that they have climbed a
mountain or crossed a col, which I fear brings a good many more; it
was a desire for _knowledge_ that brought the first explorers here,
and on this col the celebrated De Saussure lived for seventeen days,
making scientific observations.
§ 15. _Questioning the Glaciers._
124. I would now ask you to consider for a moment the facts which
such an excursion places in our possession. The snow through which
we have in idea trudged is the snow of last winter and spring. Had
we placed last August a proper mark upon the surface of the snow, we
should find it this August at a certain depth beneath the surface. A
good deal has been melted by the summer sun, but a good deal of it
remains, and it will continue until the snows of the coming winter
fall and cover it. This again will be in part preserved till next
August, a good deal of it remaining until it is covered by the snow
of the subsequent winter. We thus arrive at the certain conclusion
that on the plateau of the Col du Géant _the quantity of snow that
falls annually exceeds the quantity melted_.
Public-domain text, read in full here on John Shaqi.
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