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
One peculiarity of this great journey was that the box work, so abundant
in other portions of the cave, was here conspicuously absent.
THE CRYSTAL PALACE.
Another route in Wind Cave is that to the Crystal Palace which, although
the shortest, is the one most seldom taken by visitors, because of a
certain amount of difficulty and discomfort being unavoidable. Only a
portion of the great stairway below the entrance is descended, when we
abandon it and climb into a hole in the side-wall of the narrow passage,
from which point to the end of the trip our feet prove to be merely
encumbrances.
The space crawled into and through widens sufficiently in several places
to form chambers of good size, but the height of the ceiling is nowhere
more than three feet and most of it only two or even less. The rough
rock floor is partly carpeted with patches of loose moist clay, which is
the means of our becoming as grimy as tramps, and its source is readily
accounted for by an examination of the ceiling. This is easily made
while resting one skinned elbow at the expense of the other. The word
"abraded" is inadequate where anything approaching real cave study is
attempted.
The box work of the ceiling has almost entirely lost its
crystallization, and is as ready to crumble as the enclosed clay, which
is still retained because it had not yet reached the necessary point of
deterioration to be carried out before the great volume of water,
required for that service, retired from this high level of the cave.
When finally reached, the Crystal Palace proved worthy of the effort,
its decoration being entirely of dripstone and very beautiful, although
on too small a scale to be compared with similar work in many caves: it
is merely an attractive "extra" in Wind Cave, and not one of the
important attractions that give the Cave the rank that may have a few
equals but no superiors.
The first room is scarcely more than twelve feet in either direction and
not quite six feet high. The glassy ceiling is thickly studded with
small stalactites from two to eighteen inches in length, and mostly of
the hollow "pipe stem" variety, from which the surplus drip rests in
white masses on the clean floor around a central bowl of good clear
water.
Down the middle of the wall directly opposite the entrance a rushing
little white cascade has congealed, and on either side just under the
ceiling is a hollowed-out nook closely set with short stalactites and
small columns, all pure white.
Near by but not connected is another room too well filled to permit an
entrance, but a portion of the wall having been carried out a
satisfactory view is not denied. Here the floor rises to within three
feet of the ceiling, and the deposit is much heavier, so that many fine
columns rise from bases that spread and meet or overlap. If the cave had
no greater claim to notice than these small drip rooms, it would still
be worthy of a visit.
Public-domain text, read in full here on John Shaqi.
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