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 works of the great mine are wonderful, and visitors welcome to
examine whatever they find interesting; any questions they wish to ask
are graciously answered, although every one is busy. This is not a
special favor to the exceptional few, but the courtesy shown to all.
Visitors are also welcome to descend into the mine, but as an attendant
is necessary on account of dangers to be avoided, a permit must be
obtained at the office.
Several other caves have been discovered in the Black Hills, the largest
of which is the Davenport Cave at Sturgis. Very little exploration has
yet been done in it, but indications are said to be that it will take
rank among the large ones.
At Galena, a new mining town of golden promise, there is reported to be
an Ice Cave, where ice forms at all seasons, and during the warm weather
is a source of comfort and pleasure to the miners.
In the evening, as train time for continuing the homeward journey
approached, the snow storm which began gently early in the afternoon,
grew steadily more severe. A carriage to the depot was not to be had, as
every vehicle in town had gone to the funeral of an old-timer in the
Hills and the return delayed by the storm. The situation could not be
regarded as a special pleasure, but cave hunters learn to accept
whatever is and be thankful for the general average. At the last moment,
however, a team was driven up and permission given us to make use of it.
It proved to be the private conveyance of the hotel proprietor, and the
young boy who accompanied us, his son.
Our train was on time, and the ride through the Hills to their southern
limit, in the falling snow, was wonderfully beautiful; but the storm
continued for many days and was one of the most severe on record.
Those persons who have been so unfortunate as to permit themselves to
accept a ready made opinion of dangers and roughness to be met with in
the more newly settled regions, might find a tour of the Hills doubly
interesting by making a supplementary study of "The Living Age," which
cannot be so correctly viewed from a distance as is sometimes supposed,
since the specimens exhibited are not always a true average of the
strata they are supposed to represent.
CHAPTER XVI.
CONCLUSION.
Public-domain text, read in full here on John Shaqi.
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