Ice-Caves of France and SwitzerlandBrowne, G. F. (George Forrest)
Science
Ice-Caves of France and Switzerland
Browne, G. F. (George Forrest)
Ice caves
[Footnote 97: M. de Thury calculated that the thickness of the roof at
the lower part of the cave was about 60 feet of rock. He also noticed
the peculiar structure of the ice, which afforded great surprise to his
party. It was discovered by means of the coloured rays which were thrown
into the different parts of the cave, when some one had casually placed
a torch in a cavity in one of the columns.]
* * * * *
CHAPTER XV.
OTHER ICE CAVES.
_The Cave of Szelicze, or Szilitze, in Hungary_.[98]
Matthew Bell, the historian of Hungary, sent an account of this cavern
to England, in the middle of the last century, which was printed in the
original Latin in the 'Philosophical Transactions' of 1739-40 (pp. 41,
&c.).
This account states that the cave is in the county of Thorn,[99] among
the lowest spurs of the Carpathians. The entrance, which faces the
north, and is exposed to the cold winds from the snowy part of the
Carpathian range, is 18 fathoms high and 9 broad; and the cave spreads
out laterally, and descends to a point 50 fathoms below the entrance,
where it is 26 fathoms in breadth, and of irregular height. Beyond this
no one had at that time penetrated, on account of the unsafe footing,
although many distant echoes were returned by the farther recesses of
the cave; indeed, to get even so far as this, much step-cutting was
necessary.
When the external frost of winter comes on, the account proceeds, the
effect in the cave is the same as if fires had been lighted there: the
ice melts, and swarms of flies and bats and hares take refuge in the
interior from the severity of the winter. As soon as spring arrives, the
warmth of winter disappears from the interior, water exudes from the
roof and is converted into ice, while the more abundant supplies which
pour down on to the sandy floor are speedily frozen there. In the
Dog-days, the frost is so intense that a small icicle becomes in one day
a huge mass of ice; but a cool day promptly brings a thaw, and the cave
is looked upon as a barometer, not merely feeling, but also presaging,
the changes of weather. The people of the neighbourhood, when employed
in field-work, arrange their labour so that the mid-day meal may be
taken near the cave, when they either ice the water they have brought
with them, or drink the melted ice, which they consider very good for
the stomach. It had been calculated that 600 weekly carts would not be
sufficient to keep the cavern free from ice. The ground above the cave
is peculiarly rich in grass.
Public-domain text, read in full here on John Shaqi.
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