Aboriginal Remains in Verde Valley, Arizona / Thirteenth Annual Report of the Bureau of Ethnology to the Secretary of the Smithsonian Institution, 1891-92, Government Printing Office, Washington, 1896, pages 179-262

ABORIGINAL REMAINS

IN

VERDE VALLEY, ARIZONA

BY

COSMOS MINDELEFF

CONTENTS

ILLUSTRATIONS

Plate X. Map Showing Distribution of Ruins
and Location of Area Treated
with Reference to Ancient Pueblo Region.
larger view (705 × 973 pix)
high-resolution version for printing(300dpi, 2818 × 3888 pix)

ABORIGINAL REMAINS IN VERDE VALLEY, ARIZONA

By Cosmos Mindeleff

INTRODUCTION.

THE REGION AND ITS LITERATURE.

The region described in the following pages comprises the valley of the Rio Verde, in Arizona, from Verde, in eastern central Yavapai county, to the confluence with Salt river, in Maricopa county.

The written history of the region treated extends back only a few years. Since the aboriginal inhabitants abandoned it, or were driven from it, the hostile Apache and Walapai roamed over it without hindrance or opposition, and so late as twenty-five years ago, when the modern settlement of the region commenced, ordinary pursuits were almost impossible. Some of the pioneer settlers are still in possession, and are occupying the ground they took up at the time when the rifle was more necessary for successful agriculture than the plow.

The first notice of this region is derived from the report of Espejo, who visited some “mines” north and east of the present site of Prescott early in 1583; in 1598 Farfan and Quesada of Oñate’s expedition visited probably the same locality from Tusayan, and in 1604 Oñate crossed the country a little way north of the present Prescott, in one of his journeys in search of mineral wealth. Nothing seems to have come of these expeditions, however, and the remoteness of the region from the highways of travel and its rough and forbidding character caused it to remain unknown for over two centuries. It was not until the active prospecting for gold and silver accompanying the American invasion and conquest began that the country again became known. Valuable mines were discovered east and south of the site of Prescott, some of them as early as 1836; but it was not until after 1860 that any considerable amount of work was done, and the mining development of this region, now one of the best known in Arizona, may be said to date from about 1865. Camp Verde was first established in 1861, at a point on the northern side of Beaver creek, but was not regularly occupied until 1866. In 1871 it was removed to its present location, about a mile south of the previous site. It was abandoned as a military post in 1891, and gradually lost the military element of the name.

Concerning the archeologic remains of the Rio Verde valley almost nothing is known. In the early history of Arizona the Verde was known as Rio San Francisco, and vague rumors of large and important ruins were current among trappers and prospectors. The Pacific railway reports, published in 1856, mention these ruins on the authority of the guide to Lieut. Whipple’s party, Leroux by name. Other notices are found here and there in various books of exploration and travel published during the next two decades, but no systematic examination of the region was made and the accounts are hardly more than a mention. In 1878 Dr. W. J. Hoffman, at that time connected with the Hayden Survey, published descriptions of the so-called Montezuma well and of a large cliff ruin on Beaver creek, the latter accompanied by an illustration.1 The descriptions are slight and do not touch the region herein discussed.

The first publication of importance to the present inquiry is a short paper by Dr. E. A. Mearns, U.S. Army, in the Popular Science Monthly for October, 1890. Dr. Mearns was stationed for some years at Camp Verde, and improved the opportunity afforded by numerous hunting expeditions and tours of duty to acquaint himself with the aboriginal remains of the Verde valley. He published a map showing the distribution of remains in that region, described several ruins in detail, and illustrated some pieces of pottery, etc., found by him. The article is unfortunately very short, so short that it is hardly more than an introduction to the wide field it covers; it is to be hoped that Dr. Mearns will utilize the material he has and publish a more comprehensive report.

The remains in the valley of Rio Verde derive an additional interest from their position in the ancient pueblo region. On the one hand they are near the southwestern limit of that region, and on the other hand they occupy an intermediate position between the ruins of the Gila and Salt river valleys and those of the northern districts. The limits of the ancient pueblo region have not yet been defined, and the accompanying map (plate X) is only preliminary. It illustrates the limited extent of our knowledge of the ancient pueblo region as well as the distribution of ruins within that region, so far as they are known; and the exceptional abundance of ruins noted on certain portions of the map means only that those parts are better known than others. Notwithstanding its incompleteness, it is the best available and is published in the hope that it will serve as a nucleus to which further data may be added until a complete map is produced.

The ruins in the Gila valley, including those along Salt river, are less known than those farther northward, but we know that there is a marked difference between the type exemplified by the well-known Casa Grande, near Florence, Arizona, and that of which the best specimens (notably the Chaco ruins) are found in the San Juan basin. This difference may be due only to a different environment, necessitating a change in material employed and consequent on this a change in methods, although it seems to the writer that the difference is perhaps too great to be accounted for in this way. Be the cause what it may, there is no doubt that there is a difference; and it is reasonable to expect that in the regions lying between the southern earth-constructed and the northern stone structures, intermediate types might be found which would connect them. The valley of Rio Verde occupies such an intermediate position geographically, but the architectural remains found in it belong to the northern type; so we must look elsewhere for connecting links. The most important ruin in the lower Verde region occurs near its southern end, and more distinctly resembles the northern ruins than the ruins in the northern part of that region.

Although the examination of this region failed to connect the northern and southern types of house structure, the peculiar conditions here are exceptionally valuable to the study of the principles and methods of pueblo building. Here remains of large villages with elaborate and complex ground plan, indicating a long period of occupancy, are found, and within a short distance there are ruins of small villages with very simple ground plan, both produced under the same environment; and comparative study of the two may indicate some of the principles which govern the growth of villages and whose result can be seen in the ground plans. Here also there is an exceptional development of cavate lodges, and corresponding to this development an almost entire absence of cliff dwellings. From the large amount of data here a fairly complete idea of this phase of pueblo life may be obtained. This region is not equal to the Gila valley in data for the study of horticultural methods practiced among the ancient Pueblos, but there is enough to show that the inhabitants relied principally and, perhaps, exclusively on horticulture for means of subsistence, and that their knowledge of horticultural methods was almost, if not quite, equal to that of their southern neighbors. The environment here was not nearly so favorable to that method of life as farther southward, not even so favorable as in some northern districts, and in consequence more primitive appliances and ruder methods prevailed. Added to these advantages for study there is the further one that nowhere within this region are there any traces of other than purely aboriginal work; no adobe walls, no chimneys, no constructive expedients other than those which may be reasonably set down as aboriginal; and, finally, the region is still so little occupied by modern settlers that, with the exception of the vicinity of Verde, the remains have been practically undisturbed. A complete picture of aboriginal life during the occupancy of the lower Verde valley would be a picture of pueblo life pursued in the face of great difficulties, and with an environment so unfavorable that had the occupation extended over an indefinite period of time it would still have been impossible to develop the great structures which resulted from the settlements in Chaco canyon.

It is not known what particular branch of the pueblo-building tribes formerly made their home in the lower Verde valley, but the character of the masonry, the rough methods employed, and the character of the remains suggest the Tusayan. It has been already stated that the archeologic affinities of this region are northern and do not conform to any type now found in the south; and it is known that some of the Tusayan gentes—the water people—came from the south. The following tradition, which, though not very definite, is of interest in this connection, was obtained by the late A. M. Stephen, for many years a resident near the Tusayan villages in Arizona, who, aside from his competence for that work, had every facility for obtaining data of this kind. The tradition was dictated by Anawita, chief of the Pat-ki-nyûmû (Water house gentes) and is as follows:

We did not come direct to this region (Tusayan)—we had no fixed intention as to where we should go.

We are the Pat-ki-nyû-mû, and we dwelt in the Pa-lát-kwa-bĭ (Red Land) where the kwá-ni (agave) grows high and plentiful; perhaps it was in the region the Americans call Gila valley, but of that I am not certain. It was far south of here, and a large river flowed past our village, which was large, and the houses were high, and a strange thing happened there.

Our people were not living peaceably at that time; we were quarreling among ourselves, over huts and other things I have heard, but who can tell what caused their quarrels? There was a famous hunter of our people, and he cut off the tips from the antlers of the deer which he killed and [wore them for a necklace?] he always carried them. He lay down in a hollow in the court of the village, as if he had died, but our people doubted this; they thought he was only shamming death, yet they covered him up with earth. Next day his extended hand protruded, the four fingers erect, and the first day after that one finger disappeared [was doubled up?]; each day a finger disappeared, until on the fourth day his hand was no longer visible.

The old people thought that he dug down to the under world with the horn tips.

On the fifth day water spouted up from the hole where his hand had been and it spread over everywhere. On the sixth day Pá-lü-lü-koña (the Serpent deity) protruded from this hole and lifted his head high above the water and looked around in every direction. All of the lower land was covered and many were drowned, but most of our people had fled to some knolls not far from the village and which were not yet submerged.

When the old men saw Pá-lü-lü-koña they asked him what he wanted, because they knew he had caused this flood; and Pá-lü-lü-koña said, “I want you to give me a youth and a maiden.”

The elders consulted, and then selected the handsomest youth and fairest maid and arrayed them in their finest apparel, the youth with a white kilt and paroquet plume, and the maid with a fine blue tunic and white mantle. These children wept and besought their parents not to send them to Pá-lü-lü-koña, but an old chief said, “You must go; do not be afraid; I will guide you.” And he led them toward the village court and stood at the edge of the water, but sent the children wading in toward Pá-lü-lü-koña, and when they reached the center of the court where Pá-lü-lü-koña was the deity and the children disappeared. The water then rushed down after them, through a great cavity, and the earth quaked and many houses tumbled down, and from this cavity a great mound of dark rock protruded. This rock mound was glossy and of all colors; it was beautiful, and, as I have been told, it still remains there.