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
355. We reach Zermatt, but do not halt here. On the mountain ridge,
4,000 feet above the valley, we discern the Riffelberg hotel. This
we reach. Right in front of us is the pinnacle of the Matterhorn,
upon the top of which it must appear incredible to you that a human
foot could ever tread. Constancy and skill, however, accomplished
this, but in the first instance at a terrible price. In the little
churchyard of Zermatt we have seen the graves of two of the greatest
mountaineers that Savoy and England have produced: and who, with two
gallant young companions, fell from the Matterhorn in 1865.
356. At the Riffelberg we are within an hour's walk of the famous
Görner Grat, which commands so grand a view of the glaciers of Monte
Rosa. But yonder huge knob of perfectly bare rock, which is called
the Riffelhorn, must be our station. What the Cleft Station is to
the Mer de Glace, the Riffelhorn is to the Görner glacier and its
tributaries. From its lower side the rock, easy as it may seem, is
inaccessible. Here, indeed, in 1865, a fifth good man met his end,
and he also lies beside his fellow countrymen in the churchyard of
Zermatt. Passing a little tarn, or lake, called the Riffel See, we
assail the Riffelhorn on its upper side. It is capital rock-practice
to reach the summit; and from it we command a most extraordinary
scene.
357. The huge and many-peaked mass of Monte Rosa faces us, and we
scan its snows from bottom to top. To the right is the mighty ridge
of the Lyskamm, also laden with snow; and between both lies the
Western Glacier of Monte Rosa. This glacier meets another from the
vast snow-fields of the Cima di Jazzi; they join to form the Görner
glacier, and from their place of junction stretches the customary
medial moraine. On this side of the Lyskamm rise two beautifully
snowy eminences, the Twins Castor and Pollux; then come the brown
crags of the Breithorn, then the Little Matterhorn, and then the
broad snow-field of the Théodule, out of which springs the Great
Matterhorn, and which you and I will cross subsequently into Italy.
358. The valleys and depressions between these mountains are filled
with glaciers. Down the flanks of the Twin Castor comes the Glacier
des Jumeaux, from Pollux comes the Schwartze glacier, from the
Breithorn the Trifti glacier, then come the Little Matterhorn glacier
and the Théodule glacier, each, as it welds itself to the trunk,
carrying with it its medial moraine. We can count nine such moraines
from our present position. And to a still more surprising degree
than on the Mer de Glace, we notice the power of the ice to yield to
pressure; the broad névés being squeezed on the trunk of the Görner
into white stripes, which become ever narrower between the bounding
moraines, and finally disappear under their own shingle.
[Illustration: THE GÖRNER GLACIER, WITH MONTE ROSA IN THE DISTANCE,
AND THE RIFFELHORN TO THE LEFT.]
Public-domain text, read in full here on John Shaqi.
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