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 1: In this neighbourhood, the _montagne_ of any _commune_ is
represented by the feminine form of the name of the village: thus,
_L'Arzière_ is the _montagne_ of Arzier, and _La Bassine_ of Bassin.
This has a curious effect in the case of some villages--such, for
instance, as S. Georges--one of the landmarks of the district between
the lakes of Joux and Geneva being the _Châlet de la S. Georges_, a
grammatical anomaly which puzzles a stranger descending the southernmost
slope of the Jura from the Asile de Marchairuz. This law of formation is
not universal; for the _montagnes_ of Rolle and S. Livres are called the
_Prè de Rolle_ and the _Prè de S. Livres_, while the _Fruitière de Nyon_
is the rich upland possession of the town of that name.]
[Footnote 2: Probably a relic of the time when the earlier Barons of
Coppet possessed this district. The families of Grandson, Lesdiguières,
and Dohna successively held the barony; and in later times the title _de
Coppet_ hid a name more widely known, for on the Châlet of _Les
Biolles_, some distance to the east of La Baronne, the name of _Auguste
de Staël de Holstein de Coppet_ is carved, after the fashion of Swiss
châlets. This was Madame de Staël's son, who built Biolles in 1817; it
was afterwards sold to the commune of Nyon, and finally purchased by
Arzier two or three years ago.]
[Footnote 3: 'Cornhill Magazine,' June 1863, 'How we slept at the Châlet
des Chèvres.']
[Footnote 4: This is only a guess, made from a comparison with the
ascertained heights of neighbouring points.]
[Footnote 5: The patois of Vaud has a prettier name for this kind of
stone--_le sex_ (or _scex) qui plliau_, the weeping-stone.]
[Footnote 6: I brought one of these to England, and am told that it is
the _Stenophylax hieroglyphicus_ of Stephens, or something very like
that fly.]
[Footnote 7: Since writing this, I have been told that some English
officers who visited the cave in the August of 1864 found no ice in any
part.]
[Footnote 8: See also p. 231.]
[Footnote 9: P. 145.]
[Footnote 10: P. 301.]
[Footnote 11: It is possible that the freezing of the surface may play a
curious part in the phenomena of the spring season in such caves.
Supposing the surface to be completely frost-bound, all atmospheric
pressure will be removed from the upper surface of the water in the long
fissures, and thus water may be held in suspension, in the centre of
large masses of fissured rock, during the winter months. The first
thorough thaw will have the same effect as the removal of the thumb from
the upper orifice in the case of the hand-shower-bath; and the water
thus rained down into the cave will have a temperature sufficiently high
to destroy some portion of the cold stored up by the descent of the
heavy atmosphere of winter, or at least to melt out the ice which may
have blocked up the lower ends of the fissures.]
* * * * *
CHAPTER II.
THE GLACIÈRE OF S. GEORGES, IN THE JURA.
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