That the cavate lodges are simple "horticultural outlooks" is an important suggestion, but one might question whether they were conveniently placed for that purpose. So far as overlooking the opposite plain (which had undoubtedly been cultivated in ancient times) is concerned, the position of some of them may be regarded good for that purpose, but certainly not so commanding as that of the hill or mesa above, where well-marked ruins still exist.

The position of the cavate dwellings is a disadvantageous one to reach any cultivated fields if defenders were necessary. When the Tusayan Indian today moves to his _kisi_ or summer brush house shelter he practically camps in his corn or near it, in easy reach to drive away crows, or build wind-breaks to shelter the tender sprouts; but to go to their cornfields the inhabitants of the cavate dwellings I have described were forced to cross a river before the farm was reached.

That these cavate dwellings were lookouts none can deny, but I incline to a belief that this does not tell the whole story if we limit them to such use. It is not wholly clear to me that they were not likewise an asylum for refuge, possibly not inhabited continuously, but a very welcome retreat when the agriculturist was sorely pressed by enemies.

Following the a.n.a.logy of a Hopi custom of building temporary booths near their fields, may we not suppose that the former inhabitants of Verde valley may have erected similar shelters in their cornfields during summer months, retiring to the cavate dwellings and the mesa tops in winter? All available evidence would indicate that the cavate dwellings were permanent habitations.[19]

There are several square ruins on top of the mesa above the cavate dwellings. The walls of these were ma.s.sive, but they are now very much broken down, and the adobe plastering is so eroded from the masonry that I regard them of considerable antiquity. They do not differ from other similar ruins, so common elsewhere in New Mexico and Arizona, and are identical with others in the Verde region. I visited several of these ruins, but made no excavations in them, nor added any new data to our knowledge of this type of aboriginal buildings. The pottery picked up on the surface resembles that of the ruins of the Little Colorado and Gila.

The dwellings which I have mentioned above are said[20] to be duplicated at many other points in the watershed of the Verde, and many undescribed ruins of this nature were reported to me by ranchmen.

I do not regard them as older than the adjacent ruins on the mesa above or the plains below them, much less as productions of people of different stages of culture, for everything about them suggests contemporaneous occupancy.

From what little I saw of the village sites on the Verde I believe that Mindeleff is correct in considering that these ruins represent a comparatively late period of pueblo architecture. The character of the cliff houses of the Red-rocks shows no very great antiquity of occupancy. While it is not possible to give any approximate date when they were inhabited, their general appearance indicates that they are not more than two centuries old. There is, however, no reference to them in the early Spanish history of the Southwest.

[Ill.u.s.tration: BUREAU OF AMERICAN ETHNOLOGY

SEVENTEENTH ANNUAL REPORT PL. XCIII

BOWLDER WITH PICTOGRAPHS NEAR WOOD'S RANCH]

Few pictographs were found in the immediate neighborhood of the cavate dwellings; indeed the rock in their vicinity is too soft to preserve for any considerable time any great number of these rock etchings.

Examples of ancient paleography were, however, discovered a short distance higher up the river on malpais rock, which is harder and less rapidly eroded. A half-buried bowlder (plate XCIII) near Wood's ranch was found to be covered with the well-known spirals with zigzag attachments, horned animals resembling antelopes, growing corn, rain clouds, and similar figures. These pictographs occur on a black, superficial layer of lava rock, or upon lighter stone with a malpais layer, which had been pecked through, showing a lighter color beneath.

There is little doubt that many examples of aboriginal pictography exist in this neighborhood, which would reward exploration with interesting data. The Verde pictographs can not be distinguished, so far as designs are concerned, from many found elsewhere in Colorado, Utah, New Mexico, and Arizona.

An instructive pictograph, different from any which I have elsewhere seen, was discovered on the upturned side of a bowlder not far from Hance's ranch, near the road from Camp Verde to the cavate dwellings.

The bowlder upon which they occur lies on top of a low hill, to the left of the road, near the river. It consists of a rectangular network of lines, with attached key extensions, crooks, and triangles, all pecked in the surface. This daedalus of lines arises from grooves, which originate in two small, rounded depressions in the rock, near which is depicted the figure of a mountain lion. The whole pictograph is 3-1/2 feet square, and legible in all its parts.

The intent of the ancient scribe is not wholly clear, but it has been suggested that he sought to represent the nexus of irrigating ditches in the plain below. It might have been intended as a chart of the neighboring fields of corn, and it is highly suggestive, if we adopt either of these explanations or interpretations, that a figure of the mountain lion is found near the depressions, which may provisionally be regarded as representing ancient reservoirs. Among the Tusayan Indians the mountain lion is looked on as a guardian of cultivated fields, which he is said to protect, and his stone image is sometimes placed there for the same purpose.

In the vicinity of the pictograph last described other bowlders, of which there are many, were found to be covered with smaller rock etchings in no respect characteristic, and there is a remnant of an ancient shrine a few yards away from the bowlder upon which they occur.

MONTEZUMA WELL

One of the most interesting sites of ancient habitation in Verde valley is known as Montezuma Well, and it is remarkable how little attention has been paid to it by archeologists.[21] Dr Mearns, in his article on the ancient dwellings of Verde valley, does not mention the well, and Mindeleff simply refers to the brief description by Dr Hoffman in 1877. These ruins are worthy of more study than I was able to give them, for like many other travelers I remained but a short time in the neighborhood. It is possible, however, that some of my hurried observations at this point may be worthy of record.

Montezuma Well (plate XCIV) is an irregular, circular depression, closely resembling a volcanic crater, but evidently, as Dr Hoffman well points out, due to erosion rather than to volcanic agencies. As one approaches it from a neighboring ranch the road ascends a low elevation, and when on top the visitor finds that the crater occupies the whole interior of the hill. The exact dimensions I did not accurately determine, but the longest diameter of the excavation is estimated at about 400 feet; its depth possibly 70 feet. On the eastern side this depression is separated from Beaver creek by a precipitous wall which can not be scaled from that side. At the time of my visit there was considerable water in the "well," which was reported to be very deep, but did not cover the whole bottom. It is possible to descend to the water at one point on the eastern side, where a trail leads to the water's edge.

There appears to be a subterranean waterway under the eastern rim of the well, and the water from the spring rushes through this pa.s.sage into Beaver creek. At the time of my visit this outflow was very considerable, and in the rainy season it must be much greater. The well is never dry, and is supplied by perennial subterranean springs rather than by surface drainage.

The geological agency which has been potent in giving the remarkable crater-like form to Montezuma Well was correctly recognized by Dr Hoffman[22] and others as the solvent or erosive power of the spring.

There is no evidence of volcanic formation in the neighborhood, and the surrounding rocks are limestones and sandstones. Not far from Navaho springs there is a similar circular depression, called Jacob's Well, but which was dry when visited by me. This may later be found to have been formed in a similar way. At several places in Arizona there are formations of like geological character.

[Ill.u.s.tration: BUREAU OF AMERICAN ETHNOLOGY

SEVENTEENTH ANNUAL REPORT PL. XCIV

MONTEZUMA WELL]

The walls of Montezuma Well are so nearly perpendicular that descent to the edge of the water is difficult save by a single trail which follows the detritus to a cave on one side. In this cave, the roof of which is not much higher than the water level, there are fragments of masonry, as if structures of some kind had formerly been erected in it. I have regarded this cave rather as a place of religious rites than of former habitation, possibly a place of retreat for ancient priests when praying for rain or moisture, or a shrine for the deposit of prayer offerings to rain or water G.o.ds.

Several isolated cliff dwellings are built at different levels in the sides of the cliffs. One of the best of these is diametrically opposite the cave mentioned above, a few feet below the rim of the depression. While this house was entered with little difficulty, there were others which I did not venture to visit.

The accompanying ill.u.s.tration (plate XCV) gives an idea of the general appearance of one of these cliff houses of Montezuma Well. It is built under an overhanging archway of rock in a deep recess, with masonry on three sides. The openings are shown, one of which overlooks the spring; the other is an entrance at one side. The face of masonry on the front is not plastered, and if it was formerly rough cast the mud has been worn away, leaving the stones exposed. The side wall, which has been less exposed to the elements, still retains the plastering, which is likewise found on the inner walls where it is quite smooth in places.

The number of cliff rooms in the walls of the well is small and their capacity, if used as dwellings, very limited. There are, however, ruins of pueblos of some size on the edge of the well.

One of the largest of these, shown in the accompanying ill.u.s.tration (plate XCVI), is situated on the neck of land separating the well from the valley of Beaver creek. This pueblo was rectangular in form, of considerable size, built of stones, and although at present almost demolished, shows perfectly the walls of former rooms. Fragments of ancient pottery would seem to indicate that the people who once inhabited this pueblo were in no respect different from other sedentary occupants of Verde valley. From their housetops they had a wide view over the creek on one side and the spring on the other, defending, by the site of their village, the one trail by which descent to the well was possible.

The remarkable geological character of Montezuma Well, and the spring within it, would have profoundly impressed itself on the folklore of any people of agricultural bent who lived in its neighborhood after emigrating to more arid lands. About a month after my visit to this remarkable spring I described the place to some of the old priests at Walpi and showed them sketches of the ruins. These priests seemed to have legendary knowledge of a place somewhat like it where they said the Great Plumed Snake had one of his numerous houses. They reminded me of a legend they had formerly related to me of how the Snake arose from a great cavity or depression in the ground, and how, they had heard, water boiled out of that hole into a neighboring river. The Hopi have personal knowledge of Montezuma Well, for many of their number have visited Verde valley, and they claim the ruins there as the homes of their ancestors. It would not be strange, therefore, if this marvelous crater was regarded by them as a house of Palulukon, their mythic Plumed Serpent.

Practically little is known of the pictography of this part of the Verde valley people, although it has an important bearing on the distribution of the cliff dwellers of the Southwest. There is evidence of at least two kinds of petroglyphs, indicative of two distinct peoples. One of these was of the Apache Mohave; the other, the agriculturists who built the cliff homes and villages of the plain.

Those of the latter are almost identical with the work of the Pueblo peoples in the cliff dweller stage, from southern Utah and Colorado to the Mexican boundary. It is not a difficult task to distinguish the pictography of these two peoples, wherever found. The pictographs of the latter are generally pecked into the rock with a sharpened implement, probably of stone, while those of the former are usually scratched or painted on the surface of the rocks. Their main differences, however, are found in the character of the designs and the objects represented. This difference can be described only by considering individual rock drawings, but the practiced eye may readily distinguish the two kinds at a glance. The pictographs which are pecked in the cliff are, as a rule, older than those which are drawn or scratched, and resemble more closely those widely spread in the Pueblo area, for if the cliff-house people ever made painted pictographs, as there is every reason to believe they did, time has long ago obliterated them.

The pictured rocks (plate XCVII) near Cliff's ranch, on Beaver creek, four miles from Montezuma Well, have a great variety of objects depicted upon them. These rocks, which rise from the left bank of the creek opposite Cliff's ranch, bear over a hundred different rock pictures, figures of which are seen in the accompanying ill.u.s.tration.

The rock surface is a layer of black malpais, through which the totem signatures have been pecked, showing the light stone beneath, and thus rendering them very conspicuous. Among these pictographs many familiar forms are recognizable, among them being the crane or blue heron, bears' and badgers' paws, turtles, snakes, antelopes, earth symbols, spirals, and meanders.

Among these many totems there was an unusual pictograph in the form of the figure 8, above which was a bear's paw accompanied by a human figure so common in southwestern rock etchings. A square figure with interior parallel squares extending to the center is also found, as elsewhere, in cliff-dweller pictography.

[Ill.u.s.tration: BUREAU OF AMERICAN ETHNOLOGY

SEVENTEENTH ANNUAL REPORT PL. XCV

CLIFF HOUSE, MONTEZUMA WELL]

CLIFF HOUSES OF THE RED-ROCKS

After the road from old Camp Verde to Flagstaff pa.s.ses a deserted cabin at Beaver Head, it winds up a steep hill of lava or malpais to the top of the Mogollones. If, instead of ascending this hill, one turns to the left, taking an obscure road across the river bed, which is full of rough lava blocks, and in June, when I traveled its course, was without water, he soon finds himself penetrating a rugged country with bright-red cliffs on his right (plate XCVIII). Continuing through great parks and plains he finally descends to the well-wooded valley of Oak creek, an affluent of Rio Verde. Here he finds evidences of aboriginal occupancy on all sides--ruins of buildings, fortified hilltops, pictographs, and irrigating ditches--testifying that there was at one time a considerable population in this valley. The fields of the ancient inhabitants have now given place to many excellent ranches, one of the most flourishing of which is not far from a lofty b.u.t.te of red rock called the Court-house, which from its great size is a conspicuous object for miles around. In many of these canyons there are evidences of a former population, but the country is as yet almost unexplored; there are many difficult places to pa.s.s, yet once near the base of the rocks a way can be picked from the mouth of one canyon to another. It does not take long to discover that this now uninhabited region contains, like that along the Verde and its tributaries, many ancient dwellings, for there is scarcely a single canyon leading into these red cliffs in which evidences of former human habitations are not found in the form of ruins. There is little doubt that these unfrequented canyons have many and extensive cliff houses, the existence of which has thus far escaped the explorer. The sandstone of which they are composed is much eroded into caves with overhanging roofs, forming admirable sites for cliff houses as distinguished from cavate dwellings like those we have described. They are the only described ruins of a type hitherto thought to be unrepresented in the valley of the Verde.[23]

In our excursion into the Red-rock country we were obliged to make our own wagon road, as no vehicle had ever penetrated the rugged canyons visited by us. It was necessary to carry our drinking water with us from Oak creek, which fact impeded our progress and limited the time available in our reconnoissance. There was, however, in the pool near the ruins of Honanki enough water for our horses, and at the time we were there a limited amount of gra.s.s for fodder was found. I was told that later in the season both forage and water are abundant, so that these prime necessities being met, there is no reason why successful archeological investigations may not be successfully conducted in this part of the Verde region.

The limited population of this portion of the country rendered it difficult to get laborers at the time I made my reconnoissance, so that it would be advisable for one who expects to excavate the ruins in this region to take with him workmen from the settled portions of the valley.

RUINS NEAR SCHuRMANN'S RANCH

The valley of Oak creek, near Court-house b.u.t.te, especially in the vicinity of Schurmann's ranch, is dotted with fortifications, mounds indicative of ruins, and like evidences of aboriginal occupancy. There is undoubted proof that the former occupants of this plain constructed elaborate irrigating ditches, and that the waters of Oak creek were diverted from the stream and conducted over the adjoining valleys.

There are several fortified hills in this locality. One of the best of these defensive works crowned a symmetrical mountain near Schurmann's house. The top of this mesa is practically inaccessible from any but the southern side, and was found to have a flat surface covered with scattered cacti and scrub cedar, among which were walls of houses nowhere rising more than two feet. The summit is perhaps 200 feet above the valley, and the ground plan of the former habitations extends over an area 100 feet in length, practically occupying the whole of the summit. Although fragments of pottery are scarce, and other evidences of long habitation difficult to find, the house walls give every evidence of being extremely ancient, and most of the rooms are filled with red soil out of which grow trees of considerable age.

Descending from this ruin-capped mesa, I noticed on the first terrace the remains of a roundhouse, or lookout, in the middle of which a cedar tree had taken root and was growing vigorously. Although the walls of this structure do not rise above the level of the ground, there is no doubt that they are the remains of either a lookout or circular tower formerly situated at this point.

Many similar ruins are found throughout this vicinity, yet but little more is known of them than that they antedate the advent of white men.

The majority of them were defensive works, built by the house dwellers, and their frequency would indicate either considerable population or long occupancy. Although many of those on the hilltops differ somewhat from the habitations in the valleys, I think there is little doubt that both were built by the same people.[24] There are likewise many caves in this region, which seem to have been camping places, for their walls are covered with soot and their floors strewn with charred mescal, evidences, probably, of Apache occupancy. This whole section of country was a stronghold of this ferocious tribe within the last few decades, which may account for the modern appearance of many of the evidences of aboriginal habitation.

[Ill.u.s.tration: BUREAU OF AMERICAN ETHNOLOGY

SEVENTEENTH ANNUAL REPORT PL. XCVI

RUIN ON THE BRINK OF MONTEZUMA WELL]