Chapter 9

Near the rear of the cave erosion of the lower part of the eastern wall formed a rudely triangular recess or cavity 30 feet long by 7 feet deep at the widest part. The upper margin of this was below the surface of the ashes, so that its existence was not suspected until these had been removed from in front of it. The roof was 5 feet above the rock bottom, the entire space being filled with loose material. The upper 2 feet of this was clean ashes in which were great quantities of refuse, so much that it had all the appearance of a general dumping ground. Below this depth, patches of fine dark earth were mingled with the ashes and refuse. The latter continually decreased in quantity, until at a foot above the bottom they ceased altogether, the lower portion of the deposit consisting of nothing but earth. The pure ashes were slightly damp; and the moisture increased with the depth until at a foot above the bottom the earth was saturated and could no longer be removed with tools.

The refuse in the ashes consisted of animal bones, entire or in fragments; broken flints and pottery; mussel and snail shells; and numerous wrought objects. These continued, though in smaller amount, where the ashes were mingled with earth, though bones and shells were soft owing to the moisture, and could be removed only in fragments. Among them were the flint shown at a in plate 28, and the hematite ax, at a, plate 29. The latter was at the lowest level to which the ashes extended; perhaps its weight caused it to settle below the place at which it originally lay.

Near the middle of this chamber, 2 feet from the rear wall, lying at the bottom of the mixed ashes and earth, were 12 entire and 3 broken leaf-shaped blades; they were not closely piled, or arranged in any order, but seem to have been hastily or carelessly laid or thrown on a small space. Another was found a foot away. They are shown in plate 25.

Here and there among the refuse were found the upper jaw, with left orbit, of a young person; a fragment of an occiput, perhaps belonging with the above though not lying near it; fragments of the skull of a young child; half of an ulna of a child probably 12 years old; a small fragment of the lower jaw of an adult with one molar remaining in it, which has been burned until black. These fragments were all in such position and condition as to show they were not carried in by animals; were not disinterred from graves and placed here; were not in any way accidentally present; but had been gathered up with the refuse and thrown in as a part of it. The broken or burned condition of these, as well as of other human bones found at random among the ashes of the main cave, are presumptive evidence that dwellers here sometimes devoured the flesh of human beings; and the fact that a majority of such bones are those of children indicates that it was not eaten through a belief that the valor and skill of an enemy could be thus absorbed by the victor, but that it was used as food, like the flesh of any other animal. Such conclusion may not be justified; but the facts are not readily accounted for otherwise, except on the equally repulsive hypothesis that the inmates of the cave were brutally indifferent to the bodies or skeletal remains of their fellows.

Omitting this question from consideration, however, there is still ample evidence that the inhabitants of Miller's Cave were in a low state of savagery, or, if the phrase be preferred, in a very primitive stage of culture. There was a remarkable paucity of articles used as ornaments or for personal decoration, and the few that were found were simple and crude, being only rubbed stones or rough pieces of bones which were possibly intended for beads or pendants. The pottery, while strong and serviceable, was plain in form and devoid of any ornamentation or design except that a few pieces showed impressions such as would be made by scratching or pressing with the end of a small stick or bone. Nearly all of it was cord-marked, though some was smooth, one red piece appearing almost glazed. It varied much in thickness, hardness, and color. Most of it was dark gray, some red, occasionally a piece yellowish or nearly white; due to the different clays of which it was made. So far as observed it was tempered with shell. The shards were small, as if when a pot was broken the fragments were still further demolished. The curvature showed there was a wide range in size, from about a pint to 2 gallons or more.

Their mortars were natural blocks or slabs of sandstone, such as may be picked up by thousands in the immediate neighborhood, and showed no alteration of form beyond ordinary wear except that the rough faces of a few were pecked, apparently with a pointed flint tool, to make them less irregular. Some were flat and smooth from use with a muller or grinding stone; most of them were worked or hollowed on only one face; a few showed depressions on both sides; one had a few hemispherical indentations near the margin, like those observed in cup-stones.

Only one pestle was dressed into any of the forms which we are accustomed to associate with the name, and this was a truncated cone with rounded top, shown at b in plate 29. All the others were cobblestones from ravines or the river shore. A few had undergone no change in form; most of them were battered on the perimeter; a few had pitted sides; some had been used as pestles, mullers, or grinding stones until the surface was more or less smooth. All such stones are classed as "pestles," for convenience; they could have also been used as hammers, bone crushers, and in various other ways.

In all, 73 mortars were found; counting only those stones which bore marks of use as such. The largest one was at the bottom of the ashes, near the doorway. There were more than 100 pestles which bore evidence of much use; and probably as many more on which there was little or no sign of wear. As the cavern was not of sufficient size to provide living quarters for many families at any one time--10 or 12 at the most--the large number of these utensils may imply that the inmates would not use an object which had previously belonged to some one else.

Among the flint implements there was a wide range in the character of stone, the shape, and the degree of finish, although the variation in size was quite limited. Very few of them may be classed as either large or small. The longest, shown at a in plate 28, measured 5½ inches; few were more than 4 or less than 2 inches. Tapering stems predominated. The principal forms are shown in plates 26-28. Only three arrowheads were found; but this was to be expected, as arrows would be used only out of doors. One of these of clear, fine-grained pink and white chert, shown at b in plate 28, so far surpasses in delicate finish any other specimen secured that it is probably exotic. The large number of cores, blocks, spalls, and flakes shows that many implements were made and repaired here. But, while a few specimens showed that their fabricators were masters of the chipping art, most of them were roughly finished. Some which are so little altered from the original form of the rough flake or spall that they would be classed as "rejects" if found about a flint workshop have a smoothness or "hand polish" which denotes much service. There is the possibility, of course, that hunting or traveling parties from some other part of the country may have availed themselves of the shelter, either when it was temporarily unoccupied, or as guests of those living in it; and that these, also, may have left some small articles when they departed. However this may have been, all the objects from the top to the bottom of the deposits, in dry ashes or in sticky mud, in crevices or branch caverns, on the red clay, the barren muck, or the bedrock--all, if we may except the few flints of superior workmanship--are identical in general character: That is to say, any object from any part of the deposited material had its practical duplicate at various other points on different levels.

Only three grooved axes and three pestles were found. They are shown in plate 29, along with a cobblestone used as a pestle.

The cave was especially rich in objects wrought from bone and antler. A few of these are shown in plates 30-36 and figure 15.

Plate 36 illustrates four stages in the manufacture of skivers. It shows that instead of being always rubbed down from its natural form the bone was sometimes split by blows of a stone hammer until complete, subsequent smoothing probably resulting from use, as shown by the implement at c. When skivers were broken, the ends were dressed down for other uses; as observed in the upper row of plate 32.

Shell spoons, knives, and scrapers were abundant. Some are shown in plate 37, along with perforated pottery disks and the bowl of a spoon made from the frontal bone of a deer.

Figure 16 represents the only adz or gouge form implement found. It is made of gray chert, the edge highly polished. In figure 17 is shown a broken clay pipe, identical in form and material with that in figure 14.

The red clay which had formed the floor of the excavated area from the mouth of the cavern to well past the central portion suddenly dipped to the north and to the east shortly before reaching the corner of the west wall. Attempts to follow it downward were frustrated by black earth, which when dug with pick or shovel assumed the consistency of "hog-wallow mud."

For a space of 4 or 5 feet inside the doorway, whose floor was about 3 feet higher than the average surface level in the cave, the ashes were not more than a foot thick, the clay rising to this extent. It spread out fan shape, with a continuous slope for several yards in every direction, thus making an easy grade for entrance and exit.

There are three ways in which this condition could have been brought about.

First, the aborigines may have constructed a graded way; though it is not at all likely they would have piled the clay so far to each side.

Secondly, it may have washed through the doorway from the outer cave when the main outlet of the latter in the face of the bluff toward D (fig. 13) was obstructed in some way. This is improbable.

Thirdly, it may be due to material deposited in the eddy or swirl created by the corner of the west wall whenever a large volume of drainage water flowed from the westward in the main cave and was sharply deflected toward the south when it struck the east wall. This is no doubt the correct explanation.

Whether or not these floods had any part in piling up the clay at the doorway, beyond doubt it was to them that the clay, gravel, and sand resting upon the floor of the main cave owe their origin. To them is likewise due the dark earth overlying the clay at the rear and covering the floor of the recess in the east wall. Clearly, there was at one time in the cave's history a current at intervals, which carried mud and small rocks from the interior of the cave, or from the outside surface through sink holes, and left at least a part of it where the velocity of the stream was checked. Later, much of this water found other drainage channels, and the coarser matter could no longer be carried into the cave; but at times of unusually heavy precipitation enough of the torrent followed the old course to bring in the dark earth. The last is due to top soil containing a large amount of humus from decaying vegetation. Finally, no more water came this way except as seepage, which is the condition at present.

The pool at the rear may be entirely empty in dry seasons; and after heavy rains may contain a depth of 2 feet. This water now has a greasy looking scum and a sour, unpleasant odor.

The cave was inhabited before the water had entirely ceased to flow through it; this is proven by the alternation of refuse and silt in the recess under the east wall. Kitchen waste would be thrown here, and when the water rose sediment would cover it. There was then dry ground near the doorway; and the water in the pool, having an outlet toward the east, through the crevice, was fit for use, except, perhaps, when turbid.

On the rear slope, 18 feet from the water, the excavation was carried to the level of the bottom of the pool. The lower 2 feet was mud, and at the bottom water oozed in. Scattered through this muddy earth was much charcoal in small fragments; and for a short distance it also occurred for a few inches below the surface of the red clay. This charcoal was carried in by the water at the same time as the earth with which it was associated, and must be due to fires on the hill outside. At any rate, it did not come from any fires made within the cavern. No refuse or worked objects of any kind were found in this black earth, except in the recess in the east wall, as described, and in the upper portion immediately under the ashes. Such as existed outside the recess may have become mixed in the same way; that is, by being thrown on the top as it existed at the moment and being later covered by the water; or it may have worked in from the ashes above. Nor was there much refuse in the ashes on the rear slope, although these were quite regularly stratified.

To entirely remove the rocks and clay and expose in a satisfactory manner the bedrock floor would require months of labor, the use of mechanical appliances, and complete drainage to the rear wall through the mouth of the cave.

Without attempting to make a detailed list, there may be given a summary of the objects shipped to the National Museum:

12 skulls, most of them more or less broken. 10 partial skeletons, including those of children. 8 fragments of skulls from different individuals not included in the above. 74 objects of shell. 711 worked flint objects; knives, scrapers, cores, etc. 10 grooved axes, tomahawks, and flint hammers. 10 mortars. 40 pestles, stone hammers, rubbing stones, etc. 413 wrought objects of bone and stag horn. 2 clay pipes. 1 box of pottery fragments. A number of small objects, not classified.

There were left in the cavern several hundred broken flints; more than 60 mortars; probably 200 stones used as pestles, hammers, etc., and several large wagonloads of shell, bone, and broken pottery.

There is no way in which the age of the deposits in either the Miller or the Sells Cave can be determined. The accumulation of ashes in the one and of talus at the front of the other would certainly imply the lapse of several centuries, perhaps a thousand years of continuous occupation. Intermittent habitation would lengthen this period.

RAMSEY'S CAVE

Ramsey's Cave, better known as Freeman's Cave, is in a bluff on the right bank of Big Piney River, 3 miles below Miller's Cave. It is about 150 feet above the level of the stream and the same below the summit of the hill behind it. Within a hundred yards to east and west are shallow ravines by which access is fairly easy to a ledge nearly on the same level as the cave; this is wide enough for one person to traverse, but in most places too narrow for two abreast. The talus in front is rough and steep but a crooked path with no difficult grades can be made to the water.

Chambers on each side near the entrance, which are accessible only by means of a ladder, provide excellent living quarters and command approach from any direction, even along the foot of the cliff on either side.

The entrance, which faces southwest, is a symmetrical arch 75 feet wide and 20 feet high.

Bedrock shows just in front, covered with loose material washed over the cliff. The floor ascends and the roof descends toward the rear, until at 70 feet they approach within 6 feet of each other; beyond this the cave is choked with fallen rocks and with earth and gravel probably from a sink hole some distance back on top of the hill.

Refuse shows about the entrance and for 40 feet toward the rear, where earth from the interior has worked down over it. The surface is strewn with rocks, large and small, so that excavations are possible only in small areas. Several holes were dug at intervals between the front and the rear; a considerable amount of ashes was found over the middle portion, thrown from still farther back. Very little was found in them. The rock bottom slopes upward slightly and was covered in some places with clay and gravel, on which lay the ashes and other refuse; these were nowhere more than 3 feet deep, and usually much thinner.

The place was so difficult to work in and the returns were so scanty that systematic investigation did not seem warranted, and the work was not extended. The only objects secured were a bone perforator, part of another one, a snail shell, apparently a bead, a very small piece of sandstone used as a grinder or polisher for bones, a fragment of worked mussel shell, and nine rough flints. There were also a few small fragments of pottery.

A man living near the cave reported that a few years ago he was digging in a narrow space between the east wall and a large fallen rock. He came upon the feet of two skeletons and took out the lower leg bones. Being assured by a friend that these were not bones of Indians because they were not "red," and so must be remains of white people, he replaced them and threw the earth back on them. He was certain the spot had never since been disturbed; but in this he was mistaken, for investigation revealed a pile of human bones lying in confusion, in which the frames of two individuals, as he had said, were mingled; but no trace of the skull or jaw of either. Evidently some one had come afterwards in search of the skulls. The femur of the larger individual was just 19 inches long; the other frame was much smaller; but all other bones were in such fragmentary condition they could not be measured.

There is a rock shelter a short distance down the river from the Ramsey Cave and in the same ledge. It is 45 feet long, 15 feet deep, and 8 feet high in front, the roof coming down to the floor at the rear. There is nothing to show that it was ever used, even as a camping place.

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A fourth of a mile above this cave is another from which flows a never-failing spring. There is a pile of ashes near the front, containing some refuse, but these mark only the site of an occasional camp, as the place could not be occupied in wet weather.

GRAHAM CAVE

On Graham's land, high up in a bluff facing Big Piney, opposite the mouth of Spring Creek, is a small cave difficult to reach and not suitable for occupancy.

PILLMAN'S OR SPRING CREEK, CAVE (25)

At the mouth of Spring Creek, on land of John Pillman, near the top of the bluff, is a cave with an entrance 30 feet wide and 30 feet high. A steep rock ledge at the front offers an impassable obstacle to any stock except goats. The front chamber is well lighted for a distance of 80 feet, where it makes a turn. Bedrock is exposed near the entrance and rises toward the rear, showing here and there through the covering of earth, which is not more than 2 feet deep anywhere. Water cracks appear even in the highest spots, proving the floor to be saturated at times. There is considerable refuse inside the cave, but none in front, and it is reported that human skeletons have been found in it. If so they must have been on a ledge or in a crevice. Plate 2, a, shows the hill, from the west; plate 2, b, the entrance to the cave.

Two large cairns stood on top of the bluff above the cave. So far as can be determined in their dilapidated condition, there seems to have been a row of stones inclosing a definite area, but it is impossible to ascertain with certainty whether this was the case.

On a lower ridge, to the north, are three similar but smaller cairns. These are constructed entirely of sandstone slabs, and there was plainly some sort of system used in placing them; but, as in the case of the first, it can not now be determined whether there was a continuous wall, and, if so, whether it was more than one stone high.

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A village site is reported in the river bottom on David Thomas's farm on the Big Piney, near Moab.

There were cairns, now totally destroyed, at two places on the ridge over which passes the road from Devil's Elbow to Spring Creek.

WOODLAND HOLLOW CAVE

A minor ravine, known as Woodland Hollow, opens into a small unnamed creek a mile above its junction with Big Piney River at the Devil's Elbow. In the west slope of this ravine is a large cave, named from its location. Through the middle part the floor is muddy; along the wall on the left, dry cave earth, with a width of 20 to 30 feet, extends for 70 feet from the entrance, its surface 4 feet above the level of the wet floor. A smaller amount of dry earth lies along the opposite wall. The sides of the cavern recede at the bottom, the dry earth passing under them. No estimate can be made as to the total depth of the deposits. At the mouth of a ground-hog burrow were two bone perforators, potsherds, fragments of bones, and pieces of worked flint, including two knives, which had been thrown out by the animal. Two mortar stones were found on the margin of the dry earth.

The cave belongs to Philip Becker, of St. Louis, who peremptorily refused to allow any examination whatever to be made; the only case in the whole region where cheerful permission was not given for any amount of excavation desired.

Three cairns, all demolished, stood on the Stuart property, half a mile from Woodland Cave.

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There is a cairn on top of Lost Hill, half a mile south of Blue, or Shanghai, Spring on Big Piney.

WALLED GRAVES AT DEVIL'S ELBOW (26)

Three miles above the point at which it passes out of the hills into the bottom lands on its way to the Gasconade, the Big Piney River doubles on itself with an abrupt curve, which raftsmen have named "The Devil's Elbow." For more than a mile above and below this bend the stream flows in opposite directions in nearly parallel east and west channels around the foot of a spur from the high land to the west.

Into the Elbow, on its outer curve, three ravines from the east and southeast open within a fourth of a mile. They form the boundaries of two very narrow ridges or "hog-backs," which terminate in precipitous slopes near the river. For some distance back from the points the limestone bedrock crops out, a slight accumulation of earth in the crevices supporting a scanty covering of weeds but being insufficient to permit the growth of trees or bushes; hence the term "balds" by which they are locally known. The ridges have a gradual and nearly uniform slope toward the summit of the hill, which lies half a mile to the eastward. The sandstone capping the hill appears within a few hundred feet and is covered with an abundant growth. On the upland are many large trees.