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Browne, George Forrest

"Ice-Caves of France and Switzerland"

We passed, on our
return, by the source of water which springs from the foot of a rock at
some distance from the glaciere, and is supposed to form the outlet for
the drainage of the cave; but it is difficult to understand how this can
be the case, considering the form and character of the intervening
ground.
The two ice-caves so far described are the least interesting of all that
I have visited; but a peasant informed me, a day or two after, that if
we had penetrated to the back of the pyramid of snow which lay half
under the open hole, being the remains of the large collection which is
formed there in the winter, we might have found a deep pit which is
sometimes exposed by the melting of the snow. He had some idea that its
depth was 30 feet a few years ago, and that its sides were solid ice. I
shall have occasion to mention such pits in another glaciere; if one
does exist here, it has probably been quarried in the ice by the drops
from the hole in the roof, and there might be some interest attached to
an attempt to investigate it.[17]
We reached S.


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