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
quality and hardness; and just above them is a ledge of fine blue
marble.
The next chamber is called the Bad Lands, on account of a certain
resemblance to that desolate region. The way into it is through the
Devil's Corkscrew, a most uninviting passage because it stands on end
and is about twelve feet deep with circular, perpendicular walls
discouragingly free of prominent irregularities; but careful study
reveals a few available crags and rough edges, by which the descent is
made. Fortunately the party decreased in size just within the entrance.
Climbing up into a hole in the wall of this room, with no little
difficulty, the Aerial Lake is the reward of a breathless upward
struggle, and a satisfying one. The Lake is very small, but under its
clear surface can be seen numerous growing deposits of calcite, while
the roof of onyx gleams with a mass of small white stalactites.
Returning again to the main route and traveling to the end of a short
passage we beheld the entrance to Red Hall, a piece of rope ladder
dangling half way down a perpendicular wall, the other half having no
help whatever. The way was clear so far as the length of the ladder, and
with trust in the future soon learned in cave work that distance was at
once passed, and sitting on the very narrow ledge to cogitate on the
possibility of further progress, Mr. Sidey solved the problem by
suggesting, rather doubtfully, that the easiest way would be to drop off
and allow him to interrupt the fall. This method had twice proved the
only means of advance in Wind Cave and can be termed rapid transit. The
walls of Red Hall are of stratified limestone variegated with patches of
red rock, and clay of the same gay hue. It is the highest chamber in the
cave and probably the largest. A hole in the wall at the floor level,
near the entrance to the passage beyond, gives a glimpse of the cave
river flowing on a slightly lower level, not over two feet below the
floor we stand on. The water is said to have a depth of fifteen feet,
and a rock thrown in gave back the sound of a splash into water not
shallow. Entering the passage already referred to, its dimensions
decreased to a crawl and then to a squeeze, so that most of its length
was taken in a very humble position, which permitted no regard to be
paid to the ample mud or little pools of water that must be serenely
dragged through as if carrying them away were an agreeable privilege.
Even a muddy passage ends in time, and at last we gained a standing
point and after a short climb were in Fairies' Palace, a marvel of
dainty beauty, and worthy of the distasteful trip just taken. We stood
in a narrow passage that divided the small chamber like the central
aisle of a cathedral, above which the white roof formed a Gothic arch
from which depended countless little stalactites and draperies, while on
either side, six feet above the passage, was a floor of onyx supporting
exquisite columns of which the highest are not more than three feet.
Public-domain text, read in full here on John Shaqi.
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