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
From here we pass to the "Chamber de Norcutt," which would be considered
a very handsome room if it had no superiors: and the same can be said of
Union College, in which, however, is the Fan Rock to claim special
notice; an immense piece of fallen box work shaped like a lady's fan
half opened.
An imposing vestibule leads into the extensive but rather dreary
Catacombs, from which we crawled through a little hole into the M.W.A.
Hall, emerging at the top of a steep but not high slope covered with the
smooth yellow crust of calcite encountered at other places, and in
trying to make a dexterous turn so as to go down feet first, the
descent was accomplished with uncalculated suddenness and an unsought
but liberal collection of bruises. This, however, was not a happening of
the unexpected and could have no attention amid scenes of wonder and
beauty, and we were close to the Geysers. From a scientific point of
view this is the most important portion of the cave, for here is an
indisputable proof that the water in the cave was hot and that it was
subject to geyser action. The surrounding region is covered with the
crust already described, and at the top of a gentle elevation is thrown
up in the unmistakable form of geyser cones; there being two near
together on the surface described, with a third visible through one of
these on a slightly lower level, this one being a new discovery, as it
had escaped observation until we called attention to it.
These small cones show that after the degree of heat and the volume of
water had become reduced to the merest fraction of their former
greatness, they continued their accustomed work here in the depth of the
earth long after the once grand old geyser had ceased to show an outward
sign of life. When the water finally became so reduced even here that
the steam could no longer force it through, or to these latest vents,
the last rising vapors fringed their edges with a beautiful snow-white
border of crystallized carbonate of lime as fine and soft as a band of
swan's down, which it resembles. In the pure, still atmosphere of the
eighth level, almost five hundred feet beneath the entrance, this silent
proof of ancient action will endure for the admiration and instruction
of many generations yet to come. Few mortals will ever be honored with
memorials so lasting or so convincing of vanished power.
Proceeding on the journey the next chamber is the A.O.U.W. Hall, a
large, irregular room, by the rise of which a return to the seventh
level is accomplished; and the next entered is the Tabernacle, not at
all resembling the last, although a similar description would be
correct.
Now is reached what many consider the cave's greatest charm, The Pearly
Gates. And marvelously beautiful it certainly is.
Public-domain text, read in full here on John Shaqi.
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