PREHISTORIC VILLAGES, CASTLES, AND TOWERS OF SOUTHWESTERN COLORADO.
CLASSIFICATION.
(continued)
CLIFF-DWELLINGS
There are numerous cliff-houses in this district, but
while, as a rule, they are much smaller than the magnificent examples in
the Mesa Verde, they are built on the same architectural lines as their
more pretentious relatives. Both large and small have circular
subterranean kivas, similarly constructed to those of Spruce-tree House,
and have mural pilasters (to support a vaulted roof, now destroyed),
ventilators, and deflectors.
There are also many rooms in cliffs, possibly used
for storage or for some other unknown purposes, but too small for
habitations. It is significant that these are identical so far as their
size is concerned with the "ledge houses," near Spruce-tree House,
indicating similar or identical uses.
The kivas of cliff-dwellings of size in the region
considered have the same structural features as those of adjacent ruins,
but very little resemblance, save in site, to those of cliff-dwellings
in southern Arizona, as in the Sierra Ancha or Verde Valley, the
structure of which resembles adjacent pueblos.
The absence in the McElmo region of very large
cliff-houses is due partly but not wholly to geological conditions, the
immense caves of the Mesa Verde not being duplicated in the tributaries
of the McElmo but wherever caverns do occur, as in Sand Canyon, we
commonly find diminutive representatives. While differences in
geological features may account for the size of these prehistoric
buildings, the nature of the site or its size is not all
important. [1]
1Attention may be called to the fact that often we
find very commodious caves without correspondingly large cliff-houses,
even in the Mesa Verde.
Here and there one sees from the road through the
McElmo Canyon a few small cliff-houses, and if he penetrates some of the
tributaries, he finds many others. The canyon is dominated by the Ute
Mountain on the south, but on the north are numerous eroded cliffs in
which are many caves affording good opportunities for the construction
of cliff-houses.
These buildings do not differ save in size from the
cliff-houses of the Mesa Verde. Their kivas resemble the vaulted variety
and the masonry is identical.
Although the existence of cliff-dwellings in the
tributaries of the McElmo has long been known, the characteristic
circular kivas which occur in the Mesa Verde had not been recognized
previous to the present report.
The relative age of the pueblos and great towers and
the same structures in caves can not be decided by the data at hand, but
the indications are that they were contemporary.
On account of the similarity in structure of the
McElmo cliff-dwellings to those on Mesa Verde, only a few examples from
the former region are here considered. It may be worthy
of note that while McElmo cliff-dwellings are generally accompanied by
large open-air pueblos and towers or great houses on the cliffs above,
in the Mesa Verde open-air buildings [1] are generally situated
some distance from the cliff-dwellings.
1Sun Temple, however, is a seeming exception and
follows the McElmo rule of proximity; several large cliff-dwellings
occur under the cliff on which this mysterious building stands.
CLIFF-DWELLINGS IN SAND CANYON
Several small cliff-houses occur in Sand Canyon, one
of the northern tributaries of the McElmo. Stone Arch House, here
figured (pl. 6, a), so called from the eroded cliff (pl. 4, b)
near by. It is situated in the cliff, about a mile from where the
canyon enters the McElmo Canyon near Battle Rock. Abundant pinon trees
and a few scrubby cedars grow in the low mounds of the talus below the
ruin, near which, on top of a neighboring rock pinnacle, still stand the
well-constructed walls of a small house (pl. 4, a).
DOUBLE CLIFF-HOUSE
The formerly unnamed cliff-house shown in plate 8 [2] is
one of the best preserved in Sand Canyon. It consists of an upper and a
lower house, the former situated far back in the cave, the latter on a
projecting terrace below. Unfortunately it is impossible to introduce
an extended description of this building as it was not entered by the
author's party, but from a distance the walls exhibit fine masonry. It
is unique in having double buildings on different levels, an arrangement
not rare in a few examples of cliff-dwellings on the Mesa Verde. As
shown in plate 8, the character of the rock on which the lower house
stands is harder than that above in which the cave has been eroded. The
upper house is wholly protected by the roof [3] of the cave and occupies
its entire floor. The lower house shows from a distance at least two
rooms, the front wall of one having fallen.
2Taken from a point across the canyon, the only one
from which both houses can be included in the same photograph.
3For a good example of cliff-houses at different
levels, see Cliff-Dwellings in Fewkes Canyon, Mesa Verde National Park,
Holmes Anniversary Volume.
From a distance the walls of both the lower and the
upper house seem to be well preserved, although many of the component
stones have fallen to the base of the cliff.
SCAFFOLD IN SAND CANYON
One of the cliffs bordering Sand Canyon has an
inaccessible cave in which is an artificial platform or lookout shown in
plate 7, a. Although this structure is not as well preserved as the
scaffold in the neighborhood of Scaffold House in Laguna (Sosi) Canyon,
on the Navaho National Monument, it seems to have had a similar
purpose. It is constructed of logs reaching from one side of
the cave to the other supporting a floor of flat stones and adobe. Its
elevated situation would necessitate for entrance either holes cut in
the cliffs or ladders.
UNIT-TYPE HOUSES IN CAVES
In subsequent pages the author will describe a ruin
called the Unit-type House, situated in the open on the north rim of
Square Tower Canyon. A similar type of unit-type house is found in a
cave in Sand Canyon. The reader's attention may first be called to the
definition of a unit type, which is a building composed of a circular
kiva, with mural banquettes and pedestals supporting a vaulted roof,
with ventilator, reflector, and generally a ceremonial opening near a
central fire hole in the floor. This kiva (fig. 5) is generally embedded
in or surrounded by rectangular rooms. The
single-unit type has one kiva with several
surrounding rooms; the so-called pure type is composed of these units
united.

FIG. 5.Ground plan of Unit-type House in
cave.
In an almost inaccessible cave (pl. 5, b) in
Sand Canyon a few miles from the McElmo road near the scaffold already
mentioned there is a cliff ruin, so far as known the first described
single-unit house in a cave. It covers the whole floor of the cave (fig.
5) and its walls are considerably dilapidated, but the kiva shows this
instructive condition: The walls are double, one inside the other, with
two sets of pedestals, the outer of which are very much blackened with
smoke of constant fires; the inner fresh and untarnished, evidently of
late construction. A similar double-walled kiva known as "Kiva A" exists
in Spruce-tree House, as described in the author's account of that
ruin. [1] On the perpendicular wall of the precipice at the
right hand of the ruin in the cave above mentioned are several
pictographs shown in plate 7, c.
1Antiquities of the Mesa Verde National Park:
Spruce-tree House. Bull. 41, Bur. Amer. Ethn., 1909.
The rectangular rooms about the kiva are in places
excavated out of the cliffs, but show standing walls on the front. These
were not, however, constructed with the same care as those of the
kiva.
The cliff-house in Hackberry Canyon (pl. 9, a) is one
of the most instructive. It lies below Horseshoe House and appears to
be a second example of a unit-type kiva and surrounding rooms.
The cliff-dwelling in Ruin Canyon [1] visible
across the canyon from the Old Bluff City Road is well preserved. On the
rim of the canyon are piles of stone indicating a very large pueblo,
with surface circular depressions indicating unit-type houses.
1The name Ruin Canyon, often applied also to Square Tower Canyon, is
retained for this canyon.
CLIFF-HOUSES IN LOST CANYON
Lost Canyon, a southern tributary of the Dolores
River, contains instructive cliff-houses to which my attention was
called by Mr. Gordon Parker, superintendent of the Montezuma Forest
Reserve, who has kindly allowed me to use the accompanying photographs.
This cliff-house (pl. 10, a, b) belongs to the true Mesa Verde type and
shows comparatively good preservation of its walls, some of the beams
being in place. It is most easily approached from Mancos.
There are small cliff-houses in the same canyon not
far from Dolores, but these are smaller and their walls very poorly
preserved.
An interesting feature of these cliff-houses in Lost
Canyon is that they mark the northern horizon of cliff-dwellings of the
Mesa Verde type, having kivas similarly constructed.
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