Cave Regions of the Ozarks and Black Hills | Page 6

spar. A very clear stream of water issues out. West of the Gasconade, on Clifty Creek, is a remarkable Natural Bridge which I have elsewhere described in Geological Survey of Missouri, 1855-71, page 16."
"Mr. Meek speaks of a large and interesting cave on Tavern Creek, in Miller County. Dr. Shumard estimates a cave on Bryant's Fork, in Ozark County, to be a mile and a half long."
This description of Dr. Shumard's is in the Geological Survey of Missouri, 1855-71, page 196, where he says:
"The entrance is thirty-five feet wide and thirty feet high, and is situated at the foot of a perpendicular cliff, and far above the water-level of Bryant. Just within the entrance it expands to sixty or seventy feet, with a height of about fifty feet; and this part of the cave has been used by the citizens of the county as a place for holding camp-meeting. I estimated its length at not far short of one mile and a half. The main passage is in general quite spacious, the roof elevated, and the floor tolerably level, but often wet and miry. For some distance beyond the entrance there is not much to attract attention; but as we proceed, at the far extremity the chambers are quite as picturesque as the most noted of the well-known Mammoth Cave. The ceilings, sides and floor are adorned with a multitude of stalactites and stalagmites arranged in fanciful combinations, and assuming a variety of fantastic and beautiful forms."
Many of these caves contain niter, which occurs as a mineral and not as evidence of former animal occupation, it being found in the form of effervescenses on the walls. Dr. Shumard mentions several of this character in Pulaski County, the most noted being Niter Cave, in the Third Magnesian Limestone, with a wide entrance thirty feet above the level of the Gasconade. On page 201, he also gives a charming description of one of the immense springs that are numerous in this region and that I have never seen elsewhere. He says:
"Ozark County is bountifully supplied with springs of the finest water, and some of them of remarkably large size. The largest one is situated near the North Fork, in T. 24, R. 11 W., Sec. 32, and is known under the name of the Double Spring. It issues from near the base of a bluff of Sandstone and Magnesian Limestone, a few feet above the level of the North Fork. This spring discharges an immense volume of water, which is divided by a huge mass of Sandstone into two streams, with swift currents flowing in opposite directions to join the North Fork about one hundred and fifty yards distant from the spring. I estimated the width of these streams at not less than fifty yards. They are separated from the North Fork by a pretty wooded island one hundred yards long. The upper stream affords a good mill-site. I am informed that the quantity of water discharged by this magnificent spring is not materially diminished during the dryest seasons of the year. The temperature of the water measured at the edge of the spring, was found to be 56��; the temperature of the air at the same time, 59��. Other springs of considerable magnitude occur in various portions of the county, giving rise to beautiful and limpid streams."
The descriptions of the Natural Bridge and Friede's cave, near Rolla, previously referred to as being on page 16 of the same volume, are as follows:
"On Clifty Creek found the chert bed of Sec. 21-5 occurring about sixty feet from the top of the Third Magnesian Limestone, with a road passing over its upper surface, presenting it very favorably for observation. It seemed here to be broken by vertical cracks into large rhomboidal blocks. Further up this creek in a wild and secluded spot, observed a Natural Bridge with six feet of this chert bed at its base, and Silicious Magnesian Limestone above. The span of this bridge is about thirty feet, an elevation of opening about fifteen feet above the water, the thickness of the rock above is about twelve feet, and width on top about fifteen feet. Two small streams come together, one from the west and another from the south-west. A point of the bluff on the south-west fork spans the northern fork, and terminates about sixty feet beyond in a sharp point; a few large masses of rock lie near the termination of the promontory, and fifty feet beyond, the bluffs of the opposite hills rise abruptly from the bottoms. The bluffs, both above and below, are very precipitous, the middle and lower beds of the Third Magnesian Limestone forming perpendicular escarpments, frequently studded with cedar, some occurring on top of the bridge. A perfectly clear stream of water courses through