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nearly so dry, nor so completely covered with ice, as when we first saw
the glaciere, three years before, in the middle of an exceptionally hot
August. Under the low roof all was very dry, though even there the ice
had not an average thickness of more than 8 inches. It may be as well to
say, once for all, that the ice in these caves is never found in a sheet
on a pool of water; it is always solid, forming the floor of the cave,
filling up the interstices of the loose stones, and rising above them,
in this case with a surface perfectly level.
[Illustration: ICE-COLUMNS IN THE GLACIERE OF LA GENOLLIERE.]
We found four principal columns of ice, three of which, in the loftiest
part of the cave, are represented in the accompanying engraving: I call
them three, and not two, because the two which unite in a common base
proceeded from different fissures. The line of light at the foot of the
rock-wall is the only entrance to the glaciere. The lowest column was
11-2/3 feet high and 1-2/3 feet broad, not more than 6 inches thick in
the middle, half-way up, and flattened symmetrically so as to be
comparatively sharp at the edges, like a huge double-edged sword. It
stood clear of the rock through its whole height, but scarcely left room
between itself and the wall of the cave for a candle to be passed up and
down. The other two columns shown in the engraving poured out of
fissures in the rock, streaming down as cascades, the one being 13-1/2
and the other 15 feet high; and when we tied a candle to the end of an
alpenstock, and passed it into the fissures, we found that the bend of
the fissures prevented our seeing the termination of the ice. An
intermittent disturbance of the air in these fissures made the flame
flicker at intervals, though generally the candle burned steadily in
them, and we could detect no current in the cave. The fourth column was
in the low part of the cave, and we were obliged to grovel on the ice to
get its dimensions: it was 3-1/4 feet broad and 4-1/3 feet high, the
roof of the cave being only 2-3/4 feet high; and it poured out of the
vertical fissure like a smooth round fall of water, adhering lightly to
the rock at its upper end like a fungus, and growing out suddenly in its
full size. This column was dry, whereas on the others there were
abundant symptoms of moisture, as if small quantities of water were
trickling down them from their fissures, though the fissures themselves
appeared to be perfectly
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