Scientific American Supplement, No. 508, September 26, 1885Various
Science
Scientific American Supplement, No. 508, September 26, 1885
Various
Science -- Periodicals
This grotto is one of the most beautiful in the Pyrenees, and presents
to the visitor a succession of vast halls with roofs that are curved
like a dome, or are in the form of an ogive, or are as flat as a
ceiling. It is easy to explore these halls, for the floor is covered
with a thick stalagmitic stratum, and is not irregular as in the
majority of large caves.
[Illustration: FIG. 1.--SECTION OF THE GROTTO OF GARGAS.]
Upon entering through the iron gate at the mouth of the grotto, one
finds himself in Bear Hall, wherein a strange calcareous concretion
offers the form of the carnivorous animal after which the room is
named. This chamber is about 80 feet in width by 98 in length. We
first descend a slope formed of earth and debris mostly derived from
the outside. This slope, in which are cut several steps, rests upon a
hard, compact, and crystalline stalagmitic floor. Upon turning to the
right, we come to the Hall of Columns, the most beautiful of all. Here
the floor bristles with stalagmites, which in several places are
connected with the stalactites that depend from the ceiling. This room
is about 50 feet square. After this we reach the Hall of Crevices, 80
feet square, and this leads to the great Hall of Gargas, which is
about 328 feet in length by 80, 98, and 105 in width. In certain
places enormous fissures in the vault rise to a great height. Some of
these, shaped like great inverted funnels, are more than 60 yards in
length. The grotto terminates in the Creeping Hall. As its name
indicates, this part of the cave can only be traversed by lying flat
upon the belly. It gives access to the upper grotto through a narrow
and difficult passage that it would be possible to widen, and which
would then allow visitors to make their exit by traversing the
beautiful upper grotto, whose natural entrance is situated 150 yards
above the present one. This latter was blasted out about thirty years
ago.
Upon following the direction of the great crevices, we reach a small
chamber, wherein are found the Oubliettes of Gargas--a vertical well
65 feet feet in depth. The aperture that gives access to this strange
well (rendered important through the paleontological remains collected
in it) is no more than two feet in diameter. Such is the general
configuration of the grotto.
In 1865 Dr. Garrigou and Mr. De Chastaignier visited the grotto, and
were the first to make excavations therein. These latter allowed these
scientists to ascertain that the great chamber contained the remains
of a quaternary fauna, and, near the declivity, a deposit of the
reindeer age.
Public-domain text, read in full here on John Shaqi.
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