Ice-Caves of France and SwitzerlandBrowne, G. F. (George Forrest)
Science
Ice-Caves of France and Switzerland
Browne, G. F. (George Forrest)
Ice caves
fallen into the pit, and now lay in partial contact with the ruined
ladder; and there were on the trunk various little knobs, which might
possibly be of some use as a supplement to the rare steps of the
ladder. The snow at the bottom of the pit was surrounded on all sides
by perpendicular rock, and on the side opposite to the ladder I saw an
arch at the foot of the rock, apparently 2 or 3 feet high, leading
from the snow into darkness; and that, of course, was the entrance to
the glacière. I succeeded in getting down the ladder, by help of the
supplement, and looked down into the dark hole to see that it was
practicable, and then returned to report progress in the upper
regions. We had brought no alpenstocks to Couvet, so we sent the guide
off into the woods, where we had heard the sound of an axe, to get
three stout sticks from the woodmen; but he returned with such
wretched, crooked little things, that A. went off herself to forage,
and, having found an impromptu cattle-fence, came back with weapons
resembling bulbous hedge-stakes, which she skinned and generally
modified with a powerful clasp-knife, her constant companion. She then
cut up the crooked sticks into _bâtons_ for a contemplated repair of
the ladder, while M. and I investigated the country near the pit. We
found two other pits, which afterwards proved to communicate with the
glacière. We could approach sufficiently near to one of these to see
down to the bottom, where there was a considerable collection of snow:
this pit was completely sheltered from the sun by trees, and was 66
feet deep and 4 or 5 feet in diameter. The other was of larger size,
but its edge was so treacherous that we did not venture so near as to
see what it contained: its depth was about 70 feet, and the stone and
a foot or two of the string came up wet. The sides of the main pit, by
which we were to enter the glacière, were, as has been said, very
sheer, and on one side we could approach sufficiently near the edge to
drop a plummet down to the snow: the height of this face of rock was
59 feet, measuring down to the snow, and the level of the ice was
eventually found to be about 4 feet lower. Although it was now not
very far from noon, the sun had not yet reached the snow, owing partly
to the depth of the pit as compared with its diameter, and partly to
the trees which grew on several sides close to the edge. One or two
trees of considerable size grew out of the face of rock.
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