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
Rainy Chamber is the room in which the bones of the three-toed horse,
already referred to, were found, but their presence has not yet been
explained; therefore the case is open to conjecture and several
theories may be advanced and their values considered. The first question
when such a discovery is made, is whether the living animal was possibly
a cave-dweller; which, as the horse was not, is quickly disposed of and
attention turned to the next, the possibility of a carniverous animal
having carried his prey into the dark recesses of the cave in order that
the enjoyment of his dinner might be undisturbed. This theory is equally
unavailable by reason of the topographical features presented. If the
present natural entrance to the cave were the only way into this room
from the outside, the distance was too great and beset with many
difficulties; besides which the final passage is too small to admit an
animal of sufficient size to carry any considerable portion of even a
very small horse. But if at that period the room had direct
communication with the outside through an opening since closed, the
shape of the walls indicate that it must have been a pot-hole in the
roof, and through this an animal could have entered by falling, which
the horse and others may have done. But it seems most probable that the
remains were carried in by the water through such a hole before it was
closed at the beginning of the Quaternary period, when the erosion of
the Hills was most active.
Rainy Chamber also contains a large and beautiful assortment of the
small polished and coated pebbles called cave pearls.
Public-domain text, read in full here on John Shaqi.
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