Ice-Caves of France and SwitzerlandBrowne, G. F. (George Forrest)
Science
Ice-Caves of France and Switzerland
Browne, G. F. (George Forrest)
Ice caves
The Schafloch does not take its name from the bones contained in it, as
is the case with the Kühloch in Franconia,[58] but from the fact that
when a sudden storm comes on, the sheep and goats make their way to the
cave for shelter, never, I was told, going so far as the commencement of
the ice. The entrance faces ESE., and is of large size, with a low wall
built partly across it to increase the shelter for the sheep: Dufour
calls the entrance 50 feet wide and 25 feet high, but I found the width
at the narrowest part, a few yards within the entrance, to be 33
feet.[59] For a short distance the cave passes horizontally into the
rock, in a westerly direction, and is quite light; it then turns sharp
to the south, the floor beginning to fall, and candles becoming
necessary. Here the height increases considerably, and the way lies over
a wild confusion of loose masses of rock, which have apparently fallen
from the roof, and make progression very difficult. We soon reached a
point where ice began to appear among the stones; and as we advanced it
became more and more prominent, till at length we lost sight of the
rock, and stood on solid ice.
On either side of the cave was a grand column of ice forming the
portal, as it were, through which we must pass to further beauties.
The ice-floor rose to meet these columns in a graceful swelling curve,
perfectly continuous, so that the general effect was that of two
columns whose roots expanded and met in the middle of the cave; and,
indeed, that may have been really the order of formation. The
right-hand column was larger than its fellow, but, owing to the more
gradual expansion of the lower part of its height, and the steepness
of the consequent slope, we were unable to measure its girth at any
point where it could be fairly called a column. Christian had been in
the cave a few days before, and he assured me that the swelling base
of this column had increased very considerably since his last visit,
pointing out a solid surface of ice, at one part of our track, where
he had before walked on bare rock. The cave was by no means extremely
cold, that is to say, it was rather above than below the freezing
point, and the splashing of drops of water was audible on all sides;
so that, if Christian spoke the truth,--it was sad to be so often
reminded of Legree's plaintive soliloquy in the opening pages of
'Uncle Tom's Cabin,'--the explanation, I suppose, might be that the
drops of water, falling on the top of the column or stalagmite, run
down the sides, and carry with them some melted portion from the upper
part of the column, and after a course of a few yards become so far
refrigerated as to form ice.[60] The pillar on the left was more
approachable, but we were unable to determine its dimensions; for on
the outer side, where it stood a few feet or yards clear of the side
of the cave, the rounded ice at its foot fell off at once into a dark
chasm, a sort of smooth enticing _Bergschrund_, which we did not care
Public-domain text, read in full here on John Shaqi.
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