While, however, the Homolobi group of ruins is the most southerly to which I have been able to affix a Hopi name, others still more to the southward are claimed by certain of their traditions.[8] The Hopi likewise regard as homes of their ancestors certain habitations, now in ruins, near San Francisco mountains. In a report on his exploration of Zuñi and Little Colorado rivers in 1852, Captain L. Sitgreaves called attention to several interesting ruins, one of which was not far from the "cascades" of the latter river. After ascending the plateau, which he found covered with volcanic detritus, he discovered that "all the prominent points" were "occupied by the ruins of stone houses, which were in some instances three stories in height. They are evidently," he says, "the remains of a large town, as they occurred at intervals for an extent of eight or nine miles, and the ground was thickly strewn with fragments of pottery in all directions."
In 1884 a portion of Colonel James Stevenson's expedition, under F. D. Bickford, examined the cliff houses in Walnut canyon, and in 1886 Major J. W. Powell and Colonel Stevenson found scattered ruins north of San Francisco mountains having one, two, or three rooms, each "built of basaltic cinders and blocks of lava." These explorers likewise reported ruins of extensive dwellings in the same region made of sandstone and limestone. At about 25 miles north of the mountains mentioned they discovered a small volcanic cone of cinders and basalt, which was formerly the site of a village or pueblo built around a crater, and estimated that this little pueblo contained 60 or 70 rooms, with a plaza occupying one-third of an acre of surface.[9]
Twelve miles eastward from San Francisco mountains they found another cinder cone resembling a dome, and on its southern slope, in a coherent cinder mass, were many chambers, of which one hundred and fifty are said to have been excavated. They mention the existence on the summit of this cone of a plaza inclosed by a rude wall of volcanic cinders, with a carefully leveled floor. The former inhabitants of these rooms apparently lived in underground chambers hewn from the volcanic formation. Eighteen miles farther eastward was another ruined village built about the crater of a volcanic cone. Several villages were discovered in this locality and many natural caves which had been utilized as dwellings by inclosing them in front with walls of volcanic rocks and cinders. These cavate rooms were arranged tier above tier in a very irregular way.
At this place three distinct kinds of ruins were found—cliff villages, cave dwellings, and pueblos. Eight miles southeastward from Flagstaff, in Oak creek canyon, a cliff house of several hundred rooms was discovered. It was concluded that all these ruins were abandoned at a comparatively recent date, or not more than three or four centuries ago, and the Havasupai Indians of Cataract canyon were regarded as descendants of the former inhabitants of these villages. The situation of some of these ruins and the published descriptions would indicate that some of them were similar to those described and figured by Sitgreaves,[10] to which reference has already been made.
In 1896 two amateur explorers, George Campbell and Everett Howell, of Flagstaff, reported that they had found, about eighteen miles from that place, several well-preserved cliff towns and a remarkable tunnel excavation. The whole region in the immediate neighborhood of San Francisco mountains appears, therefore, to have been populated in ancient times by an agricultural people, and legends ascribe some of these ruins to ancestors of the Hopi Indians.
There are several ruins due south of Tusayan which have not been investigated, but which would furnish important contributions to a study of Hopi migrations. Near Saint Johns, Arizona, likewise, there are ruins of considerable size, possibly referable to the Cibolan series; and south of Holbrook, which lies about due south of Walpi, there are ruins, the pottery from which I have examined and found to be of the black-and-white ware typical of the Cliff people. Perhaps, however, no ruined pueblo presents more interesting problems than the magnificent Pueblo Grande or Kintiel, about 20 miles north of Navaho Springs. This large ruin, lying between the Cibolan and Tusayan groups, has been referred to both of these provinces, and would, if properly excavated, shed much light on the archeology of the two provinces.[11] Kinnazinde lies not far from Kintiel.
The ruins reported from Tonto Basin, of which little is known, may later be found to be connected with early migrations of those Hopi clans which claim southern origin. From what I can judge by the present appearance of ruins just north of the Mogollon mountains, in a direct line between Tonto Basin and the present Tusayan towns, there is nothing to show the age of these ruined villages, and it is quite likely that they may have been inhabited in the middle of the sixteenth century. While it is commonly agreed that the province of "Totonteac," which figures extensively in certain early Spanish narratives, was the same as Tusayan, the linguistic similarity of the word to "tonto" has been suggested by others. In the troublesome years between 1860 and 1870 the Hopi, decimated by disease and harried by nomads, sent delegates to Prescott asking to be removed to Tonto Basin, and it is not improbable that in making this reasonable request they simply wished to return to a place which they associated with their ancestors, who had been driven out by the Apache. Totonteac[12] is ordinarily thought to be the same as Tusayan, but it may have included some of the southern pueblos now in ruins west of Zuñi.
Having determined that the line of Verde ruins was continued into the Red-rock country, it was desirable to see how the latter compared with those nearer Tusayan. This necessitated reexamination of many ruins in Verde valley, which was my aim during the most of June. I followed this valley from the cavate dwellings near Squaw mountain past the great ruin in the neighborhood of Old Camp Verde, the unique Montezuma Well, to the base of the Red-rocks. Throughout this region I saw, as had been expected, no change in the character of the ruins great enough to indicate that they originally were inhabited by peoples racially different. Stopped from further advance by a barrier of rugged cliffs, I turned westward along their base until I found similar ruins, which were named Palatki and Honanki. Having satisfied myself that there was good evidence that the numbers of ancient people were as great here as at any point in the Verde valley and that their culture was similar, I continued the work with an examination of the ruins north of the Red-rocks, where there is substantial evidence that these were likewise of the same general character.
The last two months of the summer, July and August, 1895, were devoted to explorations of two Tusayan ruins, called Awatobi and Sikyatki. In this work, apparently unconnected with that already outlined, I still had in mind the light to be shed on the problem of Tusayan origin. The question which presented itself was: How are these ruins related to the modern pueblos? Awatobi was a historic ruin, destroyed in 1700, and therefore somewhat influenced by the Spaniards. Many of the survivors became amalgamated with pueblos still inhabited. Its kinship with the surviving villagers was clear. Sikyatki, however, was overthrown in prehistoric times, and at its destruction part of its people went to Awatobi. Its culture was prehistoric. The discovery of what these two ruins teach, by bringing prehistoric Tusayan culture down to the present time and comparing them with the ruins of Verde valley and southern Arizona, is of great archeological interest.
While engaged in preparing this report, having in fact written most of it, I received Mr Cosmos Mindeleff's valuable article on the Verde ruins,[13] in which special attention is given to the cavate lodges and villages of this interesting valley. This contribution anticipates many of my observations on these two groups of aboriginal habitations, and renders it unnecessary to describe them in the detailed manner I had planned. I shall therefore touch but briefly on these ruins, paying special attention to the cliff houses of Verde valley, situated in the Red-rock country. This variety of dwelling was overlooked in both Mearns' and Mindeleff's classifications, from the fact that it seems to be confined to the region of the valley characterized by the red-rock formation, which appears not to have been explored by them. The close resemblance of these cliff houses to those of the region north of Tusayan is instructive, in view of the ground, well taken, I believe, by Mr Mindeleff, that there is a close likeness between the Verde ruins and those farther north, especially in Tusayan.