THE GLACIÈRES OF THE BREZON, AND THE VALLEY OF REPOSOIR.
The bill _à la Parfaite Union_ was as small as the accommodation at that
_auberge_, and it was an immense relief to get away from the scene of my
sufferings. The path to Bonneville lies for the earlier part of the way
through pleasant scenery; and when the highest ground is reached, there
is a lovely view of the Lake of Geneva, which may be enjoyed under the
cool shade of a high hedge of trees, in the intervals of browsing upon
wild strawberries. But after passing the curious old town of La Roche,
two hours' walk from Thorens, the heat and dust of the dreary high road
became insupportable; and no pedestrian who undertakes that march with
a heavy knapsack, under a blazing noonday sun, will arrive at Bonneville
without infinite thankfulness that he has got through it. The road is of
the same character as that between Bonneville and Geneva, and that will
sufficiently express its unpleasantness in baking times of drought.
The Glacière of the Brezon lies at no great distance from
Bonneville--perhaps not more than four or five miles to the SE.--but its
elevation is more than 4,000 feet, and the approach is steep. The
Glacière of the Valley of Reposoir, a valley which falls into the main
road between Bonneville and Chamouni at the village of Scionzier, is
considerably higher, and a good deal of climbing is necessary in
visiting it. When I arrived at Bonneville, the whole mass of mountains
in which these caves lie was enveloped in thick dark clouds, and the
faint roar of thunder reached our ears now and then, so that it seemed
useless to attempt to penetrate into the high valleys. Moreover, I was
due for an attempt upon Mont Blanc in the beginning of the next week,
and an incipient bilious fever, with a painful lameness of one leg,
warned me that my powers were coming to an end, and that another day
such as the last had been would put a total stop upon the proposed
ascent; and so I determined to take the fever and the leg to Geneva, and
submit them to medical skill. This determination was strengthened by the
exhortations of a Belgian, who called himself a _grand amateurdes
montagnes_, on the strength of an ascent of the Môle and the Voiron, and
in this character administered Alpine advice of that delightful
description which one meets with in the coffee-rooms at Chamouni. This
Belgian was the only other guest of the Hôtel des Balances; and his
amiability was proof even against the inroads of some nameless species
of _vin mousseux_, recommended to me by the waiter, which supplied
_mal-à-propos_ wine-sauce to the various dishes from which the Belgian
was making his dinner, and did not leave his face and waistcoat free
from stain. He had but one remark to make, however wild might be the
assertions advanced from the English side of the table, '_Vous avez
raison, monsieur, vous avez parfait-e-ment raison_!' It is not quite
satisfactory to hold the same sentiments, in every small particular,
with a man who clips his hair down to a quarter of an inch, and eats
haricots with his fingers; but it was impossible to find any subject on
which he could be roused to dissentience. This phenomenon was explained
afterwards, when he informed me that he was a flannel-merchant
travelling with samples, and pointed out what was only too true, namely,
that the English monsieur's coat was no longer fit to be called a coat.
Professor Pictet read a paper on these glacières before the _Société
Helvétique des Sciences Naturelles_ at Berne, in 1822, which is to be
found in the _Bibl. Universelle de Genève._[77] M. Pictet left Geneva in
the middle of July to visit the caves, but found himself so much knocked
up by the first day's work, that he sent on his grandson to the Glacière
of the Brezon, and gave up the attempt himself. The young man found it
to be of small dimensions, 30 feet by 25, with a height of 10 or 12
feet. The ice on the floor was believed by the guide to be formed in
summer only, and was placed too irregularly to admit of measurement.
Calcareous blocks almost choked the entrance, and an orifice in the
shape of a funnel admitted the snow freely from above, and was partly
filled with snow in July. Cold currents of air proceeded from the rocks
in the neighbourhood of the glacière, giving in one instance a
temperature of 38°·75, the temperature in the shade being 51°. Within
the cave, the temperature was 41°.
M. Morin visited this glacière in August 1828. He describes it as a
sheltered hole, in which the snow collects and is preserved.
M. Thury examined it in August 1859, and gives the same account. He,
too, found the current of air which the younger Pictet discovered, but
in the cave itself the air was perfectly still.
It was clearly, then, no great loss to miss the Glacière of the Brezon;
but that on the Mont Vergy, in the Valley of Reposoir, appears to be
much more interesting. Professor Pictet found himself sufficiently
strong after a day's rest to pass on to Scionzier, and up the Valley of
Reposoir, accompanied by the well-known guide Timothée, whose botanical
knowledge of the district is said to be perfect. He had conducted MM.
Necker and Colladon to the glacière in 1807, and believed that no
_savant_ had since seen it. The rocks are all calcareous, with large
blocks of erratic granite. The glacière lies about 40 minutes from the
Châlet of Montarquis, whence its local name of _La grand' Cave de
Montarquis_. Before reaching it, a spacious grotto presents itself, once
the abode of coiners: this grotto is cold, but affords no ice, and near
it M. Morin found a narrow fissure, leading into a circular vaulted
chamber 15 feet in diameter, in which stood a solitary stalagmite of ice
15 feet high.
The entrance to the glacière itself is elliptical in shape, 43 feet
broad at the base, and the cave increases in size as it extends farther
into the rock, the floor descending gently till a horizontal esplanade
of ice is reached. This esplanade was 66 feet by 30 at the time of
Pictet's visit, deeper in the middle than at the sides, and mounting the
rock at the farther side of the cave; there was a small stalagmite at
one side, but that would seem to have been the only ornamentation
displayed. The temperature was 34°·7, a foot above the ice, and 58° in
the external air. Timothée had been in the glacière in the previous
April, and had found no ice,--nothing but a pool of water of
considerable depth. M. Thury, in August 1859, found two sheets of ice
in the lowest part of the cave: one, nearly 50 feet long, was partially
covered with water; the other, presenting an area of about 14 square
yards, showed more water still. There were no stalactites and columns
such as M. Morin had found in August 1828, nor even the low stalagmite
which Pictet saw in 1822. The summers of 1828 and 1859 were
exceptionally hot, and this fact has been held to account for the
smaller quantity of ice seen in those years. M. Thury found the cold due
to evaporation to be considerably less than 1° F.,[78] and he and M.
Morin both fixed the general temperature of the cave at 36°.5; they
also found a current of air entering by a fissure in the lowest part of
the cave, but it did not disturb the whole of the interior, for in one
part the air was in perfect equilibrium. M. Gampert,[79] in the summer
of 1823, found a strong and very cold current of air descending by this
fissure, along with water which ran from it over the ice; he believed
that this was refrigerated by evaporation, in passing through the
thickness of the moist rock.
Two peasants visited this cave three times in the winter season, viz. on
October 22, November 26, and on Christmas Day; and one of them, by name
Chavan, drew up an account of their experiences, which was read by M.
Colladon before the _Société de Physique et d'Histoire Nat. de Genève_
in 1824.[80] The peasants found very little ice in columns at the time
of the October visit, and there were signs of commencing thaw. The thaw
was much more pronounced in November, when the ice had nearly
disappeared even from the lowest parts of the cave, and they found the
air within quite warm. On Christmas Day they had great difficulty in
reaching the glacière, and narrowly escaped destruction by an avalanche,
which for a time deterred them from prosecuting the adventure: they
persisted, however, and were rewarded by finding only water where in
summer all was ice, and a temperate warmth in the cave. They observed
that the roof had fissures like chimneys.
This account was so circumstantial, that the only thing left was to
attempt an explanation of the phenomena reported, and such explanations
have not been wanting. But M. Thury was not quite satisfied, and he
determined to visit the cave in the winter of 1860-1. Accordingly,
accompanied by M. André Gindroz, who had already joined him in his
unsuccessful attempt to reach the Glacière of the Pré de S. Livres, he
left Geneva on the 10th of January, and slept at the Chartreuse in the
Valley of Reposoir. As the party passed through the village of Pralong
du Reposoir, the peasants told them with one accord that they would find
nothing but warmth and water in the cave; but when M. Thury asked had
any of them seen it themselves, they were equally unanimous in saying
no, explaining that it was not worth anyone's while to go in the winter,
as there was no ice to be seen then,--a circular line of argument which
did not commend itself to the strangers.
At the very entrance of the grotto, they found beautiful stalactites of
clear ice; and here they paused, till such time as they should be cool
enough to enter, for the thermometer stood at 70° in the sun, and their
climb had made them hot. On penetrating to the farther recesses of the
cave, where the true glacière lies, they found an abundance of
stalactites, stalagmites, and columns of ice, with flooring and slopes
of the same material: not a drop of water anywhere. The stalagmites were
very numerous, but none of them more than three feet high; some of the
stalactites, fifteen or so in number, were six or seven feet long, and
there were many others of a smaller size. M. Thury was particularly
struck by the milky appearance of much of the ice, one column in
particular resembling porcelain more than any other substance. This is a
not unusual character of the most beautiful part of the decorations of
the more sheltered ice-caves, as for instance the lowest cave in the
Upper Glacière of the Pré de S. Livres; the white appearance is not due
to the presence of air, for the ice is transparent and homogeneous, and
the naked eye is unable to detect bubbles or internal fissures.
The temperatures at 1.25 P.M. and 2.12 P.M. respectively were as
follows:--In the sun, between 3 and 4 feet above the snow, 72°.1 and
70°·5; in the shade, outside the cave, 36°·7 and 35°·8; at the
Observatory of Geneva, in the shade, 27°·3 and 28°·2, having risen from
24°·5 since noon. In the cave, 1 foot above the surface of the
ice-floor, the thermometer stood at 24°.8; and in a hole in the ice,
some few inches below the surface, 24°·1. In the large fissure, which has
been already mentioned as the source of the summer currents of air, the
temperature at various points was from 29°·3 to 27°·5. The circumstances
of these currents of air were now of course changed. Instead of a steady
current passing from the fissure into the cave, and so out by the main
entrance into the open air, strong enough to incline the flame of a
candle 45°, M. Thury found a gentle current passing from the cave into
the fissure, sufficient only to incline the flame 10°, and near the
entrance 8°, while in the entrance itself no current was perceptible at
4 P.M.
M. Thury remarks that less current was to be expected in winter than in
summer, because the upper ends of the fissures would be probably choked
with snow, and their lower ends with ice. It is evident that the current
which passes up into the fissure in winter, is favourable to the
introduction of the colder air from without; while the opposite current
in summer keeps up a supply of cold air in the cave, and so increases
its powers of resisting the attempts of the heated external air to make
a partial entrance. Both these currents, then, favour the glacial
conditions of the cave, and to some extent counterbalance the
disadvantages of its situation: viz., its aspect, towards the
south-east; the large size of its opening to the air, and the absence of
all shelter near the mouth, such as is so often provided by trees or
rocks. The small depth of the cave, scarcely amounting to 18 feet below
the level of the entrance, is also a great disadvantage.
The people of Pralong asked, on the return of the party, what had been
found in the _grand' cave_, and the answer reduced them to silence for a
few moments. Their prejudices, however, were invincible, and they
persisted in their belief that a true glacière ought to have no ice in
it in the winter. M. Thury did not enquire from what source they drew
their ideas of a true glacière.
There is a book, in three volumes, on the 'Glacières of the Alps,' by M.
Bourrit, dedicated to Buffon, in which is a description of the Valley of
Reposoir; but no mention whatever is made of the _grand' cave_. Indeed,
M. Bourrit merely meant by _glacière_, a glacial district, something
more extensive than a _glacier_, and he had evidently no knowledge of
the existence of caves containing ice.
FOOTNOTES:
[Footnote 77: Première Série, t. xx. pp. 261, &c.]
[Footnote 78: Less than 1/2° C., he says.]
[Footnote 79: _Bibl. Univ. de Genève_, Première Série, t. xxv. pp. 224,
&c.]
[Footnote: 80: _Bibl. Univ_. l.c.]
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