Part 23

A rock shelter not more than 15 feet wide and 10 feet deep is near the top of the bluff overlooking the Gasconade, almost opposite the mouth of Big Piney. It contains a quantity of ashes, but as it was frequently resorted to by bushwhackers during the Civil War, and is still much used by trappers and hunters who camp in it, these are probably not due to Indians.

ASH CAVE

So near to the county line that there is some uncertainty as to whether it lies in Pulaski or Phelps County is Ash Cave in a bluff over Baker's Lake, an artificial pond, 4 miles west of Arlington. The cave is small, and notwithstanding its name it contains no ashes or other remains of occupancy. The great number of large rocks on the floor makes examination impossible.

CLEMMENS CREEK CAVE (27)

At the head of a ravine opening into Clemmens Creek, about 4 miles south of Dixon, near the Piquet orchards, is a cavern with an entrance 55 feet wide and 40 feet high. The depth is 110 feet to loose rocks and clay, partly from the sides and roof, partly washed in through side caves and crevices. There is a small amount of cave earth along one wall, but it is damp, moldy, and covered with a growth of minute green fungus. Most of the floor, however, is of clay strewn with loose rocks and swept over by water at times.

There is no refuse, and the cave was never fit for habitation.

CAMDEN COUNTY

ALONG THE NIANGUA RIVER (28)

It is widely known that many caverns exist along the Niangua River and its tributaries, in Camden County, especially in the vicinity of Hahatonka, or, as it is locally termed, "Tonky." This is one of the show places of Missouri. The name includes a post office; a store; a school; an immense spring coming out at the foot of a cliff; the creek formed by this spring; a lake of several hundred acres, made by damming the creek; a picturesque ruined mill with the usual accessories of such a building; numerous caves; and a magnificent, but unfinished, residence crowning one of the hills. This has already called for an expenditure of half a million dollars; and at least double that sum, additional, will be required to complete it in accordance with the original plans. Whether it be due to the national appreciation of architectural beauty or the national appreciation of ability to do things in a large way, the palace seems to impress most visitors more than the remarkable combination of natural features.

The principal caves in the vicinity have distinctive names, as "Onyx" (there being two thus called), "Robbers'," "River" (this because there is a stream in it which can be crossed only in a boat), "Bridal," etc. Others are named for the owners of the land, or from some peculiarity, as "Dry," "Bunch," "Morgan," "Arnholdt." Many are not deemed of sufficient importance to have specific titles.

All those named were visited, as well as a number of the others.

A detailed description is not necessary. Not one of these caverns has ever been occupied unless as a temporary shelter. Some are flooded at intervals, either from the outside or by interior drainage; some have very restricted entrances and are dark at the front; some have rock floors or muddy bottoms; some can be entered only by clambering over talus to an opening at the bottom, or near the bottom, of a sink hole. Some shallow cavities, which under different conditions would be available as rock shelters, are in places difficult of access, remote from water, or otherwise unsuitable.

Some of these caverns have wonderful deposits on ceilings, walls, and floors, rivaling in beauty and ornate patterns those of the most famous caves of the country; and if they were easily accessible or could be conveniently explored, would attract hosts of visitors. One in particular, the "Bridal Cave," so called from a mass of stalactite material fully 10 feet from side to side at the top, which hangs in delicate translucent loops and folds and convolutions, equals Luray or Wyandotte for beauty, though not for extent.

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It was reported that two walled graves stand on a "bald" on the farm of Will Robert Eidson, on the divide between the Niangua and the Little Niangua Rivers, about 4 miles north of Roach post office. They were described as "rocks laid up in a regular wall about 4 feet high, and about 30 steps square, and filled up inside with rocks." A visit to the site disclosed two ordinary cairns, made by throwing weathered limestone boulders into a rounded heap. Both piles have been scattered, and as they now exist one is about 25 feet, the other about 30 feet across. Such exaggerated, misleading descriptions are common, and result in much fruitless investigation.

Several caves are reported in the vicinity of Toronto, in Camden and Miller Counties; especially the Cokely Cave, 4 miles from Brumley on the Linn Creek road. From the descriptions given by informants, none of them appear to be suitable for habitation.

Many cairns exist on the ridges in this region, especially on high points overlooking valleys. All of them were built up with chert or limestone blocks, and all are more or less torn up. So far as could be learned there is no sign of a wall in any of them.

In the present state of knowledge, Camden County offers no inducement for archeological research.

A FOSSIL CAVE (29)

The geological deposits in this region comprise three principal formations which are named in the State report as the Jefferson City limestone, the Roubidoux sandstone, and the Gasconade limestone. It is in the last (which is the lowest) that caverns are found.

In various places erosion, either internal or superficial, or both, has formed crevices or sink holes through which the disintegrated sandstone finds its way into caverns below, where it accumulates and hardens until more resistant than when in its original condition.

Further erosion has in several places carried away the limestone from around these intrusive masses, allowing them to project above the present surface. Sometimes, where the sand piled up, they resemble haystacks; but usually they are of indefinite form, having spread out on the floor of the cavern, as such material will do in a shallow stream.

An interesting example of this action is the "Standing Rock," 4 miles west of Linn Creek, the county seat. Here was formerly a large cave with an eastward trend until near the mouth, when it turned sharply southward, the opening being in the direction of a little stream. The lower end of this cave became solidly filled with sand, and the water found an outlet farther back. All the limestone which formed the roof and walls of the middle portion of the cave is gone, a narrow ravine marking its course. The sandstone obstruction held its place, and now extends directly across the ridge between the two ravines. Its surface is an exact cast of the interior of the cave which it filled, and nodules of chert, remaining when the limestone dissolved, are still imbedded in its surface. The line of demarkation between the limestone matrix, where this still exists in part, and the siliceous filling is as distinct as that between the stone and brick in a building. The loose cave earth shows plainly under the sandstone near the former mouth of the cavern. Plan and section are shown in figures 20 and 21.

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MILLER COUNTY

WRIGHT CAVE (30)

A mile and a half west of Brumley, near Glaize Creek, is Wright, or Brumley, Cave. The entrance is 15 feet high and 40 feet wide. At 20 feet from the mouth the width contracts to 20 feet. The depth is 120 feet in daylight to a stalagmite floor. Dry cave earth extends for 35 feet from the entrance, at which distance it reaches tough, sticky clay; this continues to the stalagmite. Above the clay are growing stalactites.

In front of the entrance were a few flint chips, but no indications of pottery or shell. A small implement, shown in figure 22, was found which is of interest because it was worked to a sharp point at one end of a narrow drill, while the other end widened into a squared form with a straight base which was dulled and polished from use as a cutting tool; the entire surface was polished from long service. An object of this kind would be highly suitable for mending moccasins and leggins. Finding this and nothing else strengthens the probability that this cave was used as a temporary camping place, but was never permanently occupied.