Cave Regions of the Ozarks and Black Hills by Luella Agnes Owen
page 71 of 173 (41%)
page 71 of 173 (41%)
![]() | ![]() |
|
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. Picking the way carefully as the depth of the lovely lake increased, we followed the sound of falling water and peered into the dark distance in a vain effort to see it, yet expecting to reach that special object of interest by keeping to the shallower parts of the lake. These expectations were shattered suddenly when the boots filled with water, and that called to mind the fact that twenty-three miles and a chilly night lay between us and dry clothing; so we returned to the outside world and rested on the rocks where Captain Greer and our young driver waited for us. The cave has never been fully explored, and probably we penetrated farther than others have ever done, as the owner knew nothing of the falling water we so distinctly heard and were surely very near. The view from the rocks is wonderfully beautiful and includes both the entrance to the cave, with its flowing stream, and the receiving basin with its bounding stream. But it was growing late in the afternoon, and there was another cave whose entrance was in the perpendicular wall above the end of the path by which we had come. This entrance could be reached by a dilapidated ladder; assisted by a forked pole and supplied with candles and matches, my nephew and I achieved the ascent with not much trouble. Here we found what is, no doubt, one of the oldest caves |
|