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
The box work in Crystal Cave is not of such great abundance as to demand
special attention, but is very beautiful, and one variety deserves
particular mention. These boxes have been formed in dark red sandstone,
and after being emptied of their original contents, have been completely
filled with colorless calcite crystals, and over this is spread an outer
surface of the same crystals tinted a brilliant flame color by red
paint-clay having been taken in solution by the crystal forming waters.
A specimen of this was a temptation too great to be resisted even in the
owner's absence.
Some of the box work is of such size that a single box may have a
capacity equal to that of a bushel measure, but it is less beautiful
than the smaller forms.
On the following morning we left Piedmont, and having a desire for
greater personal knowledge of the Hills, took the same train which had
taken us to the cave, and traveled to its western terminus, Lead City.
The interesting scenery makes this a desirable trip for any one visiting
the Hills, but its beauty is chiefly massed at the ends, the middle
distance being over gradually rising ground, which is without a
counterpart of the rocky canon left behind or more than a suggestion of
the high hills yet to come. The special charm of this portion was the
magnificent pine forest which covered it until three years ago, when it
was swept by a terrible fire, from which the settlers escaped with only
their lives; and even that would have been impossible if the railroad
company had not kept refuge trains waiting for them just ahead of the
flames. The prominent geological feature here is the porphyry dikes,
which are becoming more numerous and more prominent, and in many places
resemble a conspicuous group near Harney Peak, called The Needles. These
dykes are of special interest in connection with a study of the caves,
since they are probably of simultaneous origin.
The same volcanic movements that caused the violent upheaval of the
whole region, and thrust up molten masses through the strata to form a
central core to the Hills, must also have rent the nearby regions with
fissures through which probably much gas escaped, and having been
further opened and then adorned, now demand our attention as caves of
unique and curious beauty.
The approach to Lead is over the hill-tops with a magnificent distant
view, and the first glimpses of that young city famous for having as a
center the Homestake mine, the largest gold mine in the world, are
charming. It is situated far down in a valley among the high hills and
spreads some distance up the surrounding slopes.
Public-domain text, read in full here on John Shaqi.
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