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Scientific American Supplement, No. 508, September 26, 1885 by Various
page 12 of 137 (08%)
ladder), will give an idea of the form of this strange pocket formed
in the limestone of the mountain through the most complex dislocations
and erosions. Two lateral pockets attracted my attention because of
the enormous quantity of clay and bones that obstructed them. The
first, to the left, was about 15 feet from the orifice. When we had
entirely emptied it, we found that it communicated with the bottom of
the well by a narrow passage. An entire skeleton of the great cave
bear had stopped up this narrow passage, and of this, by the aid of a
small ladder, we gathered the greater part of the skeleton, the state
of preservation of which was remarkable.

The second pocket, which was almost completely filled with clay, and
situated a little lower than the other, likewise communicated with a
third cavity that reached the bottom of the well. The clay of these
different pockets contained so large a quantity of bones that we could
hardly use our picks, and the excavation had to be performed with very
short hooks, and often by hand. In this way I was enabled to remove
the bones without accident. The lower pocket was dug out first, and
with extreme care, the bones being hoisted out by means of a basket
attached to a rope. Three or four candles sufficed to give us light.
The air was heavy and very warm, and, after staying in it for two
hours, it was necessary to come to the surface to breathe. After
extracting the bones from the lower pocket, and when no more clay
remained, we successively dug out the upper ones and threw the earth
to the bottom of the well.

On the 20th of December, 1884, my excavating was finished. To-day the
Oubliettes of Gargas are obstructed with the clay that it was
impossible to carry elsewhere. The animals that I thus collected in
the well were the following: The great bear (in abundance), the little
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