Ice-Caves of France and SwitzerlandBrowne, G. F. (George Forrest)
Science
Ice-Caves of France and Switzerland
Browne, G. F. (George Forrest)
Ice caves
While we were in the cave, we noticed that the surfaces of the columns
were covered by very irregular lines, marked somewhat deeply in the
ice, and dividing the surface into areas of all shapes, a sort of
network, with meshes of many different shapes and sizes. These areas
were smaller towards the edges of the columns; the lines containing
them were not, as a rule, straight lines, and almost baffled our
efforts to count them, but, to the best of my belief, there were
meshes with three, four, and up to eight sides. The column which
stood clear of the rock was composed of very limpid ice, without
admixture of air; but the cascades were interpenetrated by veins of
looser white ice, and, where the white ice came, the surface lines
seemed to disappear. As we sat on the grass outside, arranging our
properties for departure, my attention was arrested by the columnar
appearance of the fractured edge of the block of ice which we had used
at luncheon. It was about 5 inches thick, and had formed part of a
stalagmite whose horizontal section, like that of the free column,
would be an ellipse of considerable eccentricity; and, on examination,
it turned out that the surface areas, which varied in size from a
large thumb-nail to something very small, were the ends of prisms
reaching through to the other side of the piece of ice, at any rate in
the thinner parts, and presenting there similar faces. Not only so,
but the prisms could be detached with great ease, by using no
instrument more violent than the fingers; while the point of a thin
knife entered freely at any of the surface lines, and split the ice
neatly down the sides of the prisms. When one or two of the sides of a
prism were exposed, at the edge of the piece of ice, the prism could
be pushed out entire, like a knot from the edge of a piece of wood. In
some cases there seemed to be capillary fissures coincident with the
lines where several sides of prisms met. Considering the shape of the
whole column, it is clear that the two ends of each prism could not be
parallel; neither was one of the ends perfectly symmetrical with the
other, and I do not think that the prisms were of the nature of
truncated pyramids. On descending again, I found that the columns
were without exception formed of this prismatic ice, either in whole,
as in the clear column, or in part, as where limpid prisms existed
among the white ice which ran in veins down the cascades. In the free
vertical column the prisms seemed to be deposited horizontally, and in
the thicker parts they did not pass clear through. We carried a large
piece of ice down to Arzier in a botanical tin, and on our arrival
there we found that all traces of external lines had disappeared.
Public-domain text, read in full here on John Shaqi.
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