Prev | Current Page 181 | Next

Owen, Luella Agnes, 1852-1932

"Cave Regions of the Ozarks and Black Hills"

On these crystals the pop-corn is being
formed, and specimens can be seen in all stages of development, from the
beginning to an approximate degree of finish; and whatever the position
it occupies on the receiving surface, either on top, underneath, or on a
side exposure, it always maintains the same relative position as growing
plants on the mundane sphere. The water falling on the upper surface in
scattering drops forms myriads of minute stalagmites; on side positions
the falling drop first strikes the point exposed to its line of descent
and then spreads. The scant moisture slowly makes its way down sloping
sides and shelving edges, leaving on each small irregularity a tiny
portion of its volume, to deposit an infinitely small charge of solid
substance, and the balance finally hangs in moisture less than drops on
the growing grains of the under surface.
Pop-corn, therefore, is the globular aragonite of the stalagmitic
variety. A small specimen from Rainy Chamber, placed beside one of the
same color from Wind Cave, shows them to be absolutely alike.
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.


Pages:
169 170 171 172 173 174 175 176 177 178 179 180 181 182 183 184 185 186 187 188 189 190 191 192 193