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Browne, George Forrest

"Ice-Caves of France and Switzerland"

The approach is by ladders, down a pit 30
fathoms wide and 24 deep; and when the bottom of this pit is reached,
an entrance is found to the cave in the north wall, in the
neighbourhood of which is congealed snow which shortly becomes ice.
The floor of the first chamber is composed of glacier-ice, separated
from the side walls by a cleft from 1 to 3 feet wide, where it shows a
depth of from 4 to 6 feet; it is as smooth as glass, and about 6
fathoms from the entrance a cone of ice stands upon it, 8 or 9 feet
high. Both the floor and the cone are at once seen to be transformed
remains of ancient masses of snow, and are of a dirty yellow colour.
At the back of this chamber, a narrow passage opens towards the interior
of the mountain, and winds steeply down with a height of 4 feet, and a
length of a few fathoms, till a magnificent dome is reached, on the
beauties of which Herr Peters becomes eloquent. The floor is so smooth
that crimpons are necessary, and stalagmites and stalactites of ice are
found in rich profusion, the latter being generally formed on small
limestone stalactites, while the former have no such nucleus.


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