Journal of a Tour in the Years 1828-1829, through Styria, Carniola, and Italy, whilst Accompanying the Late Sir Humphry DavyTobin, J. J.
History
Journal of a Tour in the Years 1828-1829, through Styria, Carniola, and Italy, whilst Accompanying the Late Sir Humphry Davy
Tobin, J. J.
Davy, Humphry, Sir, 1778-1829; Europe -- Description and travel
The _Tournier-platz_ or Place of the
Tournament, is a lofty and extensive cavern, the floor of which is
formed of very fine sand, and is exceedingly level and firm. The shape
of the vault is oval, and the sides have some slight resemblance to an
amphitheatre. On Whit-Monday the whole of the grotto is illuminated,
and hundreds flock to behold this curious scene, the _Tournier-platz_
being arranged as a ball-room, and in which the visitors dance till a
very late hour. From thence we went through long passages and caverns,
each of which presents something remarkable. In one, a large pillar
rises from the ground, which, on being struck with a stone or stick,
gives out a sound resembling the deep and sonorous tone of a tolling
bell; and in another, stands a large fluted pillar, to which the
guides give the strange name of the _Kanonen-Säule zu Moskau_, or the
Pillar of Canons at Moscau. In another part of the cavern we see a
vase, on the top of a small pillar, constantly full of water, which
falls into it, drop by drop, from the roof; it is perfectly clear,
and icy cold. Beyond this font, we came to the _great curtain_, the
most striking single stalactite in the whole cavern. The limestone
here descends in many a waving and beautiful fold from the roof, from
a height of upwards of twenty feet, and projecting about six feet out
from the rock. The whole mass is exceedingly thin, and is bordered
by a stripe of red. Seen from a distance, when the guides hold their
lamps behind it, the effect is highly striking, and the spectator can
hardly believe that the transparent curtain before him is formed of
hard stone. The red colour in the edge of this mass of limestone, is
the only instance of the kind I met with in the grotto, the general
colour of the stalactites being either pure white or whitish brown:
and they are often covered with a crust of very fine crystals. At some
distance beyond the curtain, the cave divides into two branches, one
of which ends with a large block of limestone, that bears the name
of the _high altar_; the other has been rarely trodden by the foot
of a stranger, for my guide said that this was only the second time
that he had been there, since the discovery of that part of the cave,
by him and another of the men who were with me, six or seven years
ago. It extends for a considerable way, till all further progress is
stopped by a large pool of water, over which the guides said no one had
ever crossed. This pool did not appear to me to be of any very great
extent, and I felt persuaded, that with the help of a few long poles,
it would have been possible to have passed over the slippery rocks on
its sides; we had, however, nothing of the kind with us, and I was
obliged to abandon the idea, nor did the guides appear at all inclined
to continue our peregrinations, having already penetrated to a greater
distance than usual. I carefully examined the water, but in vain, to
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