Aboriginal Remains In Verde Valley, Arizona Part 1

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 Onate's expedition visited probably the same locality from Tusayan, and in 1604 Onate 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 ill.u.s.tration.[1] The descriptions are slight and do not touch the region herein discussed.

[Footnote 1: Tenth Ann. Rep. U.S. Geol. Survey for 1876 (Washington, 1878), p. 477.]

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 ill.u.s.trated 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 ill.u.s.trates 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.

[Ill.u.s.tration: Plate XI.

MAP OF THE VALLEY OF THE RIO VERDE.]

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 princ.i.p.ally 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-nyumu (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-nyu-mu, and we dwelt in the Pa-lat-kwa-bi (Red Land) where the kwa-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 Pa-lu-lu-kona (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 Pa-lu-lu-kona they asked him what he wanted, because they knew he had caused this flood; and Pa-lu-lu-kona 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 Pa-lu-lu-kona, 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 Pa-lu-lu-kona, and when they reached the center of the court where Pa-lu-lu-kona 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.

[Ill.u.s.tration: Plate XII.

GROUND PLAN OF RUIN NEAR MOUTH OF LIMESTONE CREEK.

RIO VERDE : ARIZONA]

The White Mountain Apache have told me that they know a place in the south where old houses surround a great rock, and the land in the vicinity is wet and boggy.

We traveled northward from Palat-kwabi and continued to travel just as long as any strength was left in the people--as long as they had breath. During these journeys we would halt only for one day at a time. Then our chief planted corn in the morning and the pa-to-la-tei (dragon fly) came and hovered over the stalks and by noon the corn was ripe; before sunset it was quite dry and the stalks fell over, and whichever way they pointed in that direction we traveled.

When anyone became ill, or when children fretted and cried, or the young people became homesick, the Co-i-yal Katcina (a youth and a maiden) came and danced before them; then the sick got well, children laughed, and sad ones became cheerful.

We would continue to travel until everyone was thoroughly worn out, then we would halt and build houses and plant, remaining perhaps many years.

One of these places where we lived is not far from San Carlos, in a valley, and another is on a mesa near a spring called Coyote Water by the Apache. * * *

When we came to the valley of the Little Colorado, south of where Winslow now is, we built houses and lived there; and then we crossed to the northern side of the valley and built houses at h.o.m.olobi.

This was a good place for a time, but a plague of flies came and bit the suckling children, causing many of them to die, so we left there and traveled to Ci-pa (near k.u.ma spring).

Finally we found the Hopi, some going to each of the villages except Awatobi; none went there.

PHYSICAL DESCRIPTION OF THE COUNTRY.

The Rio Verde is throughout its length a mountain stream. Rising in the mountains and plateaus bounding two great connected valleys northwest of Prescott, known as Big Chino valley and Williamson valley, both over 4,000 feet above the sea, it discharges into Salt river about 10 miles south of McDowell and about 25 miles east of Phoenix, at an elevation of less than 1,800 feet above the sea. The fall from Verde to McDowell, a distance of about 65 miles, is about 1,500 feet The whole course of the river is but little over 150 miles. The small streams which form the river unite on the eastern side of Big Chino valley and flow thence in a southerly and easterly direction until some 12 miles north of Verde the waterway approaches the edge of the volcanic formation known on the maps as the Colorado plateau, or Black mesa, and locally as "the rim." Here the river is sharply deflected southward, and flows thence in a direction almost due south to its mouth. This part of the river is hemmed in on both sides by high mountain chains and broken every few hundred yards by rapids and "riffles."

Its rapid fall would make the river valuable for irrigation if there were tillable land to irrigate; but on the west the river is hugged closely by a mountain chain whose crest, rising over 6,000 feet above the sea, is sometimes less than 2 miles from the river, and whose steep and rugged sides descend in an almost unbroken slope to the river bottom. The eastern side of the river is also closely confined, though not so closely as the western, by a chain of mountains known as the Mazatzal range. The crest of this chain is generally over 10 miles from the river, and the intervening stretch, unlike the other side, which comes down to the river in practically a single slope, is broken into long promontories and foothills, and sometimes, where the larger tributaries come in, into well-defined terraces. Except at its head the princ.i.p.al tributaries of the Verde come from the east, those on the west, which are almost as numerous, being generally small and insignificant.

Most of the modern settlements of the Rio Verde are along the upper portion of its course. Prescott is situated on Granite creek, one of the sources of the river, and along other tributaries, as far down as the southern end of the great valley in whose center Verde is located, there are many scattered settlements; but from that point to McDowell there are hardly a dozen houses all told. This region is most rugged and forbidding. There are no roads and few trails, and the latter are feebly marked and little used. The few permanent inhabitants of the region are mostly "cow men," and the settlements, except at one point, are shanties known as "cow camps." There are hundreds of square miles of territory here which are never visited by white men, except by "cow-boys" during the spring and autumn round-ups.

Scattered at irregular intervals along both sides of the river are many benches and terraces of alluvium, varying in width from a few feet to several miles, and comprising all the cultivable land in the valley of the river. Since the Verde is a mountain stream with a great fall, its power of erosion is very great, and its channel changes frequently; in some places several times in a single winter season. Benches and terraces are often formed or cut away within a few days, and no portion of the river banks is free from these changes until continued erosion has lowered the bed to such a degree that that portion is beyond the reach of high water. When this occurs the bench or terrace, being formed of rich alluvium, soon becomes covered with gra.s.s, and later with mesquite and "cat-claw" bushes, interspersed with such cottonwood trees as may have survived the period when the terrace was but little above the river level. Cottonwoods, with an occasional willow, form the arborescent growth of the valley of the Verde proper, although on some of the princ.i.p.al tributaries and at a little distance from the river groves of other kinds of trees are found. All these trees, however, are confined to the immediate vicinity of the river and those of its tributaries which carry water during most of the year; and as the mountains which hem in the valley on the east and west are not high enough to support great pines such as characterize the plateau country on the north and east, the aspect of the country, even a short distance away from the river bottom, is arid and forbidding in the extreme.

[Ill.u.s.tration: Plate XIII.

MAIN COURT, RUIN NEAR LIMESTONE CREEK.]

Within the last few years the character of the river and of the country adjacent to it has materially changed, and inferences drawn from present conditions may be erroneous. This change is the direct result of the recent stocking of the country with cattle. More cattle have been brought into the country than in its natural state it will support. One of the results of this overstocking is a very high death rate among the cattle; another and more important result is that the gra.s.ses and other vegetation have no chance to seed or mature, being cropped off close to the ground almost as soon as they appear. As a result of this, many of the river terraces and little valleys among the foothills, once celebrated for luxuriant gra.s.s, are now bare, and would hardly afford sustenance to a single cow for a week. In place of strong gra.s.ses these places are now covered for a few weeks in spring with a growth of a plant known as "filaree," which, owing to the rapid maturing of its seeds (in a month or less), seems to be the only plant not completely destroyed by the cattle, although the latter are very fond of it and eat it freely, both green and when dried on the ground. As a further effect of the abundance of cattle and the scarcity of food for them, the young willows, which, even so late as ten years ago, formed one of the characteristic features of the river and its banks, growing thickly in the bed of the stream, and often forming impenetrable jungles on its banks, are now rarely seen.

Owing to the character of the country it drains, the Rio Verde always must have been subject to freshets and overflows at the time of the spring rains, but until quite recently the obstructions to the rapid collection of water offered by thickly growing gra.s.s and bushes prevented destructive floods, except, perhaps, on exceptional occasions.

Now, however, the flood of each year is more disastrous than that of the preceding year, and in the flood of February, 1891, the culminating point of intensity and destructiveness was reached. On this occasion the water rose in some places over 20 feet, with a corresponding broadening in other places, and flowed with such velocity that for several weeks it was impossible to cross the river. As a result of these floods, the gra.s.sy banks that once distinguished the river are now but little more than a tradition, while the older terraces, which under normal circ.u.mstances would now be safe, are being cut away more and more each year. In several localities near Verde, where there are cavate lodges, located originally with especial reference to an adjacent area of tillable land, the terraces have been completely cut away, and the cliffs in which the cavate lodges occur are washed by the river during high water.

DISTRIBUTION AND CLa.s.sIFICATION OF RUINS.

All the modern settlements of the lower portion of the Verde valley are located on terraces or benches, and such localities were also regarded favorably by the ancient builders, for almost invariably where a modern settlement is observed traces of a former one will also be found. The former inhabitants of this region were an agricultural people, and their villages were always located either on or immediately adjacent to some area of tillable soil. This is true even of the cavate lodges, which are often supposed to have been located solely with reference to facility of defense. Owing to the character of the country, most of the tillable land is found on the eastern side of the river, and as a consequence most of the remains of the former inhabitants are found there also, though they are by no means confined to that side. These remains are quite abundant in the vicinity of Verde, and less so between that point and the mouth of the river. The causes which have induced American settlement in the large area of bottom land about Verde doubtless also induced the aboriginal settlement of the same region, although, owing to the different systems of agriculture pursued by the two peoples, the American settlements are always made on the bottom lands themselves, while the aboriginal settlements are almost always located on high ground overlooking the bottoms. Perched on the hills overlooking these bottoms, and sometimes located on the lower levels, there was once a number of large and important villages, while in the regions on the south, where the tillable areas are as a rule very much smaller, the settlements were, with one exception, small and generally insignificant.

The region treated in these pages is that portion of the valley of Rio Verde comprised between its mouth and Verde, or Beaver creek, on the north. It was entered by the writer from the south; it is not proposed, however, to follow a strict geographic order of treatment, but, on the contrary, so far as practicable, to follow an arrangement by types.

The domiciliary ruins of this region fall easily into three general cla.s.ses, to which may be added a fourth, comprising irrigating ditches and works, the first cla.s.s having two subcla.s.ses. They are as follows: