The Glaciers of the Alps: Being a narrative of excursions and ascents, an account of the origin and phenomena of glaciers and an exposition of the physical principles to which they are relatedTyndall, John
Science
The Glaciers of the Alps: Being a narrative of excursions and ascents, an account of the origin and phenomena of glaciers and an exposition of the physical principles to which they are related
Tyndall, John
Alps -- Description and travel; Glaciers -- Alps
No matter in what direction a solar beam is sent through lake-ice, the
liquid flowers are all formed parallel to the surface of freezing. The
beam may be sent parallel, perpendicular, or oblique to this surface;
the flowers are always formed in the same planes. Every line
perpendicular to the surface of a frozen lake is in fact an axis of
symmetry, round which the molecules so arrange themselves, that, when
taken down by the delicate fingers of the sunbeam, the six-leaved liquid
flowers are the result.
In the ice of glaciers we have no definite planes of freezing. It is
first snow, which has been disturbed by winds while falling, and whirled
and tossed about by the same agency after it has fallen, being often
melted, saturated with its own water, and refrozen: it is cast in
shattered fragments down cascades, and reconsolidated by pressure at the
bottom. In ice so formed and subjected to such mutations, definite
planes of freezing are, of course, out of the question.
[Sidenote: CONSTITUTION OF GLACIER-ICE.]
The flat round disks and vacuous spots to which I have referred come
here to our aid, and furnish us with an entirely new means of analysing
the internal constitution of a glacier. When we examine a mass of
glacier-ice which contains these disks, we find them lying in all
imaginable planes; not confusedly, however--closer examination shows us
that the disks are arranged in groups, the members of each group being
parallel to a common plane, but the parallelism ceases when different
groups are compared. The effect is exactly what would be observed,
supposing ordinary lake-ice to be broken up, shaken together, and the
confused fragments regelated to a compact continuous mass. In such a
jumble the original planes of freezing would lie in various directions;
but no matter how compact or how transparent ice thus constituted might
appear, a solar beam would at once reveal its internal constitution by
developing the flowers parallel to the planes of freezing of the
respective fragments. A sunbeam sent through glacier-ice always reveals
the flowers in the planes of the disks, so that the latter alone at
once informs us of its crystalline constitution.
[Sidenote: VACUOUS CELLS MISTAKEN FOR AIR-CELLS.]
Public-domain text, read in full here on John Shaqi.
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