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ceiling, and the floor is muddy and rocky. The drainage from 3 or 4 acres of hillside flows over the arch of the entrance and logs 6 inches in diameter are carried into it by the surface floods. LOCK'S CAVE.--This is a mile east of Rowlett's Station, near the top of a ridge, and lying nearly parallel with its crest. It affords another instance of a cave which has come to light only after a portion of its roof has fallen in. The detritus entirely conceals the opening at one end. The other end is entered by going down the fallen rocks over a slope of 15 or 20 feet, which leads to a bottom strewn with rocks. In such cases there can be nothing under the loose material, because the cave had no entrance until this had fallen in. GARVIN CAVE.--This cavern, which is 3 miles southeast of Munfordville, has an opening at the bottom of a sink hole, requiring a rope or ladder for descent. HARLOW CAVE.--This is 31/2 miles southeast of Munfordville. It is a very large cave, apparently, as the slope down the debris is more than 40 feet high, to a rocky shelf, beyond which the descent was followed some yards without finding any indications that a level bottom was near. It is another illustration of the fallen roof. WYNNE'S CAVE.--Three miles south of Rowlett's Station is a large sink hole. Stones thrown into the vertical shaft at the bottom can be heard striking the sides for three or four seconds before coming to rest. WASH. ROWLETT CAVE.--On "the old Lewis Martin place," 11/2 miles west of Rowlett's Station, a section of roof, 20 or 25 feet across, has dropped into a deep cavity. The sides are still insecure. The descent to a spring under what appears to be the original roof is somewhat more than 40 feet. The ceiling is not more than 6 feet high. STEFFY'S CAVE.--Four miles southwest of Munfordville between 200 and 300 feet in length of the roof of a high and wide cave has fallen in. Ice remains in this cave until May or later every year. JOEL BUCKNER'S CAVE.--About 10 miles northeast of Munfordville is a large cave with the entrance on a hillside. The roof has evidently extended several rods farther out than at present. The front part of the cavern is wide and high, but is now nearly filled with debris. The roof slopes at about the same angle as loose material within, there being not more than 3 feet of space between the two at any place nearer than 30 feet from the present mouth. Rocks thrown back showed the same unif
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