Cave Regions of the Ozarks and Black Hills eBook

This eBook from the Gutenberg Project consists of approximately 189 pages of information about Cave Regions of the Ozarks and Black Hills.

Cave Regions of the Ozarks and Black Hills eBook

This eBook from the Gutenberg Project consists of approximately 189 pages of information about Cave Regions of the Ozarks and Black Hills.

The old mill was the scene of great activity in former times, but was closed on account of an unfortunate accident and for years has had no other duty than simply to serve as a portion of the landscape.

Just beyond, the canon makes a curving bend, the road dwindles to a narrow path and we behold the most beautiful scene imaginable.

The canon has come to an end and is shut in by a graceful curve of the high, perpendicular grey walls that are crowned with trees and shrubs, and decked below with a thick carpet of bright green moss.  In this basin, which is nearly one hundred feet across, Greer Spring plunges up from beneath through an opening nine feet in diameter, in the midst of a pool of water six feet deep, and having an unvarying temperature of forty-nine degrees throughout the year.  This water is so perfectly clear that not the least pebble is obscured from view, and the color scheme is most marvelous.

[Illustration:  Greer Spring.  Page 88.]

Where the great spring forces its way to the surface, the water is a deep, brilliant blue with white caps, and its falling weight keeps clear of moss a large spot of fine, pure, white sandstone, while all the balance appears a vivid green from the moss that thrives beneath the moving water; and surrounding these are the handsome, foliage-decked grey walls.  The edges of the basin are thickly strewn with fallen rocks deeply covered with moss, in which small ferns are growing, and on these gay stepping stones we crossed to the head-wall of the canon to find ourselves at the open mouth of a cave from which flows a clear, shallow stream to join the waters of the Spring in that wonderful basin.  The entrance to the cave is an arch about fifteen feet wide and twelve feet high, with the clear, shallow stream spreading over the clean rock floor from side to side.  Here now was presented a difficulty.  Truly the cave was not quite dry.  The water was about ten inches deep, and my boots in Thayer.  Contrary to advice, however, my nephew had brought his, and with a boy’s kindness loaned them while he made the trip with bare feet and rolled up trousers.

A short distance within, the cave widens and the floor of the extension being somewhat higher, is dry, but the roof drops so low over it that the water-course is an easier route of travel; and this soon widens into a lake above which the ceiling rises in a broad dome less than twenty feet in height, and hung with heavy masses of dripstone draperies of varying length, from five to seven feet; and all the ceilings are fringed at various heights with stalactites of every size and age, some being a clear, colorless onyx, while others proclaim their great age in the fact that they have so deteriorated that the onyx texture is either partly or completely lost, and what was once a pure drip crystal has returned to a common, porous, dull-colored limestone so soft that portions can be rubbed to powder in the hand.

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Project Gutenberg
Cave Regions of the Ozarks and Black Hills from Project Gutenberg. Public domain.