CAVATE DWELLINGS--OAK CREEK]

The section of the cliff which was examined embraced the northern

series of these caves, extending from a promontory forming one side of

a blind or box canyon to nearly opposite our camp. Adjacent to this

series of rooms, but farther down the river, on the same side, there

are two narrow side canyons, in both of which are also numerous caves,

in all respects similar to the series we chose for examination. At

several points on the summit of the cliffs, above the caves, large

rectangular ruins, with fallen walls, were discovered; these ruins

are, however, in no respect peculiar, but closely resemble those

ordinarily found in a similar position throughout this region and

elsewhere in Arizona and New Mexico. From their proximity to the caves

it would seem that the cavate dwellings, and the pueblos on the

summits of the mesas in which they are found, had been inhabited by

one people; but better evidence that such is true is drawn from the

character of the architecture and the nature of the art remains common

to both.

Let us first consider the series of caves from a point opposite our

camp to the promontory which forms a pinnacle at the mouth of the

first of the two side caverns--a row of caves the entrances to which

are shown in the accompanying illustration (plate XCII). I have

lettered these rooms, as indicated by their entrances, _a_ to _l_,

beginning with the opening on the left.

The rock in which these caves have been hewn is very soft, and almost

white in color, save for a slightly reddish brown stratum just below

the line of entrances to the cavate chambers. Although, as a general

thing, the wall of the cliff is almost perpendicular, and the caves at

points inaccessible, entrance to the majority of them can be effected

by mounting the heaps of small stones forming the débris, which has

fallen even to the bed of the river at various places, and by

following a ledge which connects the line of entrances. The easiest

approach mounts a steep decline, not far from the promontory at the

lower level of the line, which conducts to a ledge running along in

front of the caves about 150 feet above the bed of the stream. Roughly

speaking, this ledge is about 100 feet below the summit of the cliff.

It was impossible to reach several of the rooms, and it is probable

that when the caves were inhabited access to any one of them was even

more difficult than at present.

Judging from the number of rooms, the cliffs on the left bank of the

Verde must have had a considerable population when inhabited. These

caverns, no doubt, swarmed with human beings, and their inaccessible

position furnished the inhabitants with a safe refuge from enemies, or

an advantageous outlook or observation shelter for their fields on the

opposite side of the stream. The soft rock of which the mesa is formed

is easily worked, and there are abundant evidences, from the marks of

tools employed, that the greater part of each cave was pecked out by

hand. Fragments of wood were very rarely seen in these cliff dugouts;

and although there is much adobe plastering, only in a few instances

were the mouths of the caves walled or a doorway of usual shape

present. The last room at the southern end, near the promontory at the

right of the entrance to a side canyon, has walls in front resembling

those of true cliff houses and pueblos in the Red-rock country farther

northward, as will be shown in subsequent pages.

This group of cavate dwellings, while a good example of the cavern

type of ruins, is so closely associated, both in geographical position

and in archeological remains, with other types in Verde valley, that

we are justified in referring them to one and the same people. The

number of these troglodytic dwelling places on the Verde is very

large; indeed the mesas may be said to be fairly honeycombed with

subterranean habitations. Confined as a general thing to the softer

strata of rock, which from its character was readily excavated, they

lie side by side at the same general level, and are entered from a

projecting ledge, formed by the top of the talus which follows the

level of their entrances.

[Illustration: FIG. 245--Plan of cavate dwelling on Rio Verde]

This ledge is easily accessible in certain places from the river bed,

where stones have fallen to the base of the cliff; but at most points

no approach is possible, and in their impregnable position the

inhabitants could easily defend themselves from hostile peoples.

[Illustration: BUREAU OF AMERICAN ETHNOLOGY

Archeological Expedition to Arizona in 1895 Seventeenth Annual Report of the Bureau of American Ethnology to the Secretary of the Smithsonian Institution, 1895-1896, Government Printing Office, Washington, 1898, pages 519-744 · 第 17 / 295 题