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Owen, Luella Agnes, 1852-1932

"Cave Regions of the Ozarks and Black Hills"

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.


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