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 519-744Fewkes, Jesse Walter
History
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
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
SEVENTEENTH ANNUAL REPORT PL. XCII
ENTRANCES TO CAVATE RUINS]
Whether the rock had recesses in it before the caves were enlarged
would seem to be answered in the affirmative, for similar caves
without evidences of habitations were observed. These, however, are as
a rule small, and wherever available the larger caverns have been
appropriated and enlarged by stone implements, as shown by the pecking
on the walls. The enlargement of these caverns, however, would not be
a difficult task, for the rock is very soft and easily worked.
Entering one of these cavate rooms the visitor finds himself in a dark
chamber, as a rule with side openings or passageways into adjoining
rooms. Broad lateral banquettes are prominent features in the most
complicated caves, and there are many recesses and small closets or
cists.
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