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
352. From the Æggischhorn I might lead you along the mountain ridge
by the Betten See, the fish of which we have already tasted, to the
Rieder Alp, and thence across the Aletsch to the Bel Alp. This is a
fine mountain ramble, but you and I prefer making the glacier our
highway downwards. Easy at some places, it is by no means child's
play at others to unravel its crevasses. But the steady constancy and
close observation which we have hitherto found availing in difficult
places do not forsake us here. We clear the fissures; and, after four
hours of exhilarating work, we find ourselves upon the slope leading
up to the Bel Alp hotel.
353. This is one of the finest halting-places in the Alps. Stretching
before us up to the Æggischhorn and Märgelin See is the long last
reach of the Aletsch, with its great medial moraine running along its
back. At hand is the wild gorge of the Massa, in which the snout of
the glacier lies couched like the head of a serpent. The beautiful
system of the Oberaletsch glaciers is within easy reach. Above us
is a peak called the Sparrenhorn, accessible to the most moderate
climber, and on the summit of which little more than an hour's
exertion will place you and me. Below us now is the Oberaletsch
glacier, exhibiting the most perfect of medial moraines. Near us
is the great mass of the Aletschhorn, clasped by its névés, and
culminating in brown rock. It is supported by other peaks almost as
noble as itself. The Nesthorn is at hand; while sweeping round to the
west we strike the glorious triad already referred to, the Weisshorn,
the Matterhorn, and the Dom. Take one glance at the crevasses of the
glacier immediately below us. It tumbles at its end down a steep
incline, and is greatly riven. But the crevasses open before the
steep part is reached, and you notice the coalescence of marginal and
transverse crevasses, producing a system of curved fissures with the
convexities of the curves pointing upwards. The mechanical reason of
this is now known to you. The glacier-tables are also numerous and
fine. I should like to linger with you here for a week, exploring the
existing glaciers, and tracing out the evidences of others that have
passed away.
§ 52. _The Riffelberg and Görner Glacier._
354. And though our measurements and observations on the Mer de Glace
are more or less representative of all that can be made or solved
elsewhere, I am unwilling to leave you unacquainted with the great
system of glaciers which stream from the northern slopes of Monte
Rosa and the adjacent mountains. From the Bel Alp we can descend to
Brieg, and thence drive to Visp; but you and I prefer the breezy
heights, so we sweep round the promontory of the Nessel, until we
stand over the Rhone valley, in front of Visp. From this village an
hour's walking carries us to Stalden, where the valley divides into
two branches: the one leading through Saas over the Monte Moro, and
the other through St. Nicholas to Zermatt. The latter is our route.
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