Cave Regions of the Ozarks and Black HillsOwen, Luella Agnes
Science
Cave Regions of the Ozarks and Black Hills
Owen, Luella Agnes
Caves -- Black Hills (S.D. and Wyo.); Caves -- Ozark Mountains
Where the great spring forces its way to the surface, the water is a
deep, brilliant blue with white caps, and its falling weight keeps clear
of moss a large spot of fine, pure, white sandstone, while all the
balance appears a vivid green from the moss that thrives beneath the
moving water; and surrounding these are the handsome, foliage-decked
grey walls. The edges of the basin are thickly strewn with fallen rocks
deeply covered with moss, in which small ferns are growing, and on these
gay stepping stones we crossed to the head-wall of the canon to find
ourselves at the open mouth of a cave from which flows a clear, shallow
stream to join the waters of the Spring in that wonderful basin. The
entrance to the cave is an arch about fifteen feet wide and twelve feet
high, with the clear, shallow stream spreading over the clean rock floor
from side to side. Here now was presented a difficulty. Truly the cave
was _not_ quite dry. The water was about ten inches deep, and my boots
in Thayer. Contrary to advice, however, my nephew had brought his, and
with a boy's kindness loaned them while he made the trip with bare feet
and rolled up trousers.
A short distance within, the cave widens and the floor of the extension
being somewhat higher, is dry, but the roof drops so low over it that
the water-course is an easier route of travel; and this soon widens
into a lake above which the ceiling rises in a broad dome less than
twenty feet in height, and hung with heavy masses of dripstone draperies
of varying length, from five to seven feet; and all the ceilings are
fringed at various heights with stalactites of every size and age, some
being a clear, colorless onyx, while others proclaim their great age in
the fact that they have so deteriorated that the onyx texture is either
partly or completely lost, and what was once a pure drip crystal has
returned to a common, porous, dull-colored limestone so soft that
portions can be rubbed to powder in the hand.
Picking the way carefully as the depth of the lovely lake increased, we
followed the sound of falling water and peered into the dark distance in
a vain effort to see it, yet expecting to reach that special object of
interest by keeping to the shallower parts of the lake. These
expectations were shattered suddenly when the boots filled with water,
and that called to mind the fact that twenty-three miles and a chilly
night lay between us and dry clothing; so we returned to the outside
world and rested on the rocks where Captain Greer and our young driver
waited for us. The cave has never been fully explored, and probably we
penetrated farther than others have ever done, as the owner knew
nothing of the falling water we so distinctly heard and were surely very
near.
Public-domain text, read in full here on John Shaqi.
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