Cave Regions of the Ozarks and Black Hills by Luella Agnes Owen
page 119 of 173 (68%)
page 119 of 173 (68%)
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being coated over and cemented together with calcite crystal.
From the Glacier down to the lowest level of the cave by another route than that taken for the ascent, there is abundant evidence that at one time this portion of the cave was subject to excessively violent activity, and if studied with a view to the penetration of the principle of geyser action, offers many interesting and valuable suggestions that can be added to and expanded into definite theories in connection with the balance of the cave; all important requirements are clearly shown. At a short distance from the Glacier is a small circular dome, called the Picture Gallery, which evidently was shaped by water forced up from below. The descent from here takes us into the St. Louis Tunnel, a long rough passage leading down into the great Cathedral, by the still descending irregularities of which we finally reach the Garden of Eden, the objective point of a favorite tourist route, but usually approached from the opposite direction. It is a large chamber of very irregular shape, with an extremely uneven ceiling, dipping nearly to the floor and rising suddenly to distant heights, while every portion of all the varied surfaces glitters with a mass of frost work in every form it is known to have assumed; the banks of orange buds in different stages of expansion being exceptionally handsome. A portion of this wonderful room especially admired is Cupid's Alcove, where the frost is tinged with a pinkish flush from the brilliant paint clay captured in minute particles by the vapors. The whole room is a marvel of loveliness, but unfortunately visitors have wrought such noticeable damage that wire screening must be placed before the general admittance of large parties can be resumed. Passing out and down to a lower level, by way of Jacob's Well, we find |
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