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
243. In the summer of 1864 Mr. Hirst and myself set out three lines
of stakes across the glacier. The first line crossed the ice high up;
the second a good distance lower down, and the third lower still.
Even the third line, however, was at a considerable distance above
the actual snout of the glacier. The daily motion of these three
lines was as follows:--
First Line.
Stake 1 2 3 4 5 6 7 8 9 10 11
Inches 8 12 13 13 14 13 12 12 10 7 5
Second Line.
Stake 1 2 3 4 5 6 7 8 9 10 11
Inches 1 4 6 8 10 11 11 11 11 11 11
Third Line.
Stake 1 2 3 4 5 6 7 8 9 10 11
Inches 1 2 4 5 6 6 7 7 5 5 4
244. Compare these lines together. You notice the velocity of the
first is greater than that of the second, and the velocity of the
second greater than that of the third.
245. The lines were permitted to move down wards for 100 hours,
at the end of which time the spaces passed over by the points of
swiftest motion of the three lines were as follows:
Maximum Motion in 100 Hours.
First line 56 inches.
Second line 45 "
Third line 30 "
246. Here then is a demonstration that the upper portions of the
Morteratsch glacier are advancing on the lower ones. _In 1871 the
motion of a point on the middle of the glacier near its snout was
found to be less than two inches a day!_
247. What, then, is the consequence of this swifter march of
the upper glacier? Obviously to squeeze this medial moraine
longitudinally, and to cause it to spread out laterally. We have here
distinctly revealed the cause of the widening of the medial moraine.
248. It has been a question much discussed, whether a glacier is
competent to scoop out or deepen a valley through which it moves, and
this very Morteratsch glacier has been cited to prove that such is
not the case. Observers went to the snout of the glacier, and finding
it sensibly quiescent, they concluded that no scooping occurred. But
those who contended for the power of glaciers to excavate valleys
never stated, or meant to state, that it was the snout of the
glacier which did the work. In the Morteratsch glacier the work of
excavation, which certainly goes on to a greater or less extent,
must be far more effectual high up the valley than at the end of the
glacier.
§ 36. _Birth of a Crevasse: Reflections._
249. Preserving the notion that we are working together, we will
now enter upon a new field of enquiry. We have wrapped up our
chain, and are turning homewards after a hard day's work upon the
Glacier du Géant, when under our feet, as if coming from the body
of the glacier, an explosion is heard. Somewhat startled, we look
enquiringly over the ice. The sound is repeated, several shots
being fired in quick succession. They seem sometimes to our right,
sometimes to our left, giving the impression that the glacier is
breaking all round us. Still nothing is to be seen.
Public-domain text, read in full here on John Shaqi.
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