CONCLUSIONS

Geographically the Mimbres Valley is the northern extension of the

drainage area of the large interior plateau, the lowest level of which

is occupied by Palomas, Guzman, and other so-called lakes. The Casas

Grandes, Mimbres, and other rivers contribute their scanty waters to

these lakes, which have no outlets into the sea. As a rule the thirsty

sands along the course of the river drink up the surplus waters of

the Mimbres or cause them to sink beneath the surface, to reappear

when the configuration of lower clay or rock formations forces them

from subterranean courses. Considering the similarity in climatic and

geographical conditions in the northern and southern ends of this

plateau, we would expect to find cultural likenesses in the prehistoric

inhabitants of the Mimbres and Casas Grandes valleys, but such is not

the case. The absence of relief decoration combined with painting, so

common in the pottery from the Casas Grandes region, separates the

Mimbres ware from that found far to the south.[58]

There are evidences that the course of the Mimbres River through

Antelope Plain has from time to time changed considerably, and although

a section of its bed now lies east of the Florida Mountains, the river

probably formerly made its way to the west of the same in its course to

Mexico. Modifications or changes in the bed of this river have had in

the past much to do with the shifting of population and obliteration

of prehistoric sites, either by washing them away entirely or burying

them out of sight or deeply below the surface. This concealment of

evidences of prehistoric occupancy has also been aided by frequent

sandstorms, when considerable quantities of soil have been transported

from place to place and deposited on walls or covered implements lying

on the surface of the ground. It is also possible that there has been

a slow change of climate, causing a desiccation which may have been so

widespread that the inhabitants of the plain were driven up river into

the hills where water was more abundant, but it is well to remember

that abandoned settlements or ruins exist on the banks of the Mimbres

where there is still abundant water, as well as in the plain which is

dry.

The depth of the present water level, as shown by drilling for wells,

varies in different places in the valley, but in the neighborhood of

the hills there are many springs. The configuration of the surface

of the hard clay strata lying beneath the soil here and there often

forces the water to rise to the surface, and ruins occur at points

where at present there are no signs of surface water, although at the

time they were inhabited there may have been more water.[59] Whether or

not this water was brought to certain ruins by a system of artificial

irrigation, the canals of which have been obliterated, we cannot say,

but there is only scanty evidence that the climate here, as elsewhere,

has radically changed since man occupied the valley.[60]

Although there is a remote likeness between the terraced house or

pueblo community of northern New Mexico[61] and the prehistoric houses

of the Lower Mimbres, its closest resemblance is to an antecedent type,

for it is possible that the terraced pueblo culture in the Rio Grande

Valley was preceded by another. This earlier type of habitation of

the Mimbres Valley was like the fragile-walled house of the natives

inhabiting a large part of Arizona and New Mexico before the Puebloan,

and we have evidence that this older style of building was scattered

over the present Pueblo area. There is no evidence of a terraced

dwelling or pueblo more than one story high in the Mimbres or the

inland basin in which it lies. In other words the ruins of the Mimbres

may be regarded as older than true pueblo ruins, resembling an earlier

type of dwelling that antedated, in the Rio Grande Valley, the terraced

houses.

The author does not find any architectural features in the remains

of the prehistoric habitations of the Mimbres Valley suggesting

Casa Grande compounds, or those massive buildings with encircling

walls which are characteristic of the plains of the Gila. Although

the walls of the Casas Grandes, in Chihuahua, are constructed in

the same way and out of material like those of Casa Grande on the

Gila, the architectural feature, an encircling wall of the latter,

has not yet been recognized on the Sierra Madre plateau.[62] Objects

found in the Gila ruins are somewhat different in form from those of

Chihuahua, while pottery from the Gila Valley ruins and that from the

inland plateau in northern Chihuahua is markedly different, with very

divergent symbolism. Not only do forms of stone implements of a shape

unknown in southern Arizona occur in southern New Mexico, but also

the methods of disposal of the dead differed among the two people.

The latter practised inhumation only, the other both cremation and

inhumation. The aborigines of the Mimbres Valley placed a bowl over

the head or face of the dead, a practice which, so far as known, does

not appear to have been so commonly in vogue in inhumation of the

prehistoric people of the Lower Gila plains.

The conventional geometric symbols on prehistoric Mimbres pottery are

readily distinguished from those on ware from Tulerosa, a tributary

of the San Francisco. The most significant feature of the Mimbres

pottery is that fifty per cent of the figures on it represent men or

animals, while out of a hundred bowls from the Gila not more than two

or three are ornamented with zoic designs. As we know comparatively

nothing of the pottery of the sources of the Upper Gila and that part

of its course which lies between the Tulerosa and the Mimbres, we can

at present venture very little information on ceramic relations, but

similarities or mixtures would naturally be expected, due to contact or

overlapping, the type of the one valley overlaying that of the other or

mingling with it.

The sources of the Upper Salt, the largest tributary of the Gila, lie

far from the Mimbres, and close relationship in the pottery of the

ancient people inhabiting its banks is not found or expected. It is

not known whether the pottery from the Upper Salt and that from the

Upper Gila is similar, for our museums have no extensive collections

from the latter region from which to make comparisons and draw

conclusions. We know practically nothing of the prehistoric culture of

the Upper Gila.

The aborigines of the Mimbres, like those of some of the former

dwellers in Pajarito Park in New Mexico, practised a modified form of

urn burial, but the latter rarely decorated their pottery with figures

of animals. As compared with known Pueblo ceramics, the Mimbres pottery

appears to be more closely allied to ancient Keresan than to old Tewan.

Judging from what remains, the houses architecturally had little in

common with true pueblos.[63] There are no evidences of circular

subterranean kivas with pilasters, ventilators, deflectors, and niches,

as in northern New Mexico, although there is a fairly large proportion

of subterranean rooms or pit dwellings which may have been their

prototypes. Architecturally the prehistoric habitations of the Mimbres

Valley represent an old house form widely distributed in the Pueblo

region or that antedating the pueblo or terraced-house type before the

kiva had developed.

There are not sufficient data at hand to determine satisfactorily the

kinship of the prehistoric inhabitants of Mimbres Valley, but as far as

may be judged by pottery symbols it may be supposed that their culture

resembled that of other sedentary people of New Mexico and Arizona in

early times, as well as that of peoples of Chihuahua. It appears to the

author that there are so many cultural similarities among the sedentary

people which inhabited the Sierra Madre plateau, of which the Antelope

Plain of Mimbres Valley is only a northern extension, that we may

regard their culture as closely related. A specialized high development

of this inland culture took place along the Casas Grandes River,

culminating in Chihuahua. The Mimbres Valley was inhabited by people

somewhat less developed in culture.

Although the ancients of the Mimbres were related on the one side to

the Pueblos of New Mexico and on the other to more southern people,

that relationship existed between the ancestors of the same rather than

with modern Pueblos, and reached back to a time before the terraced

communal house type originated. This type of house arose in northern

New Mexico and spreading from this center extended down the San Juan

as far as the Hopi, while modifications are also found in certain

ruins on the Gila and Little Colorado, which, like Zuñi, it profoundly

influenced, but its influence never reached as far as the Lower Mimbres.

A comparison of the limited archeological material from the Mimbres

with that from other localities in the Southwest suggests a provisional

hypothesis that the prehistoric culture of this valley was not modified

by terraced architecture nor greatly affected by that of the Lower Gila

type, both of which evolved independently and locally, but belonged to

an older type with which it had much in common.

[Illustration: PL. 1

FIG. 1.—WOMAN DANCER. BLACK AND WHITE WARE. 12 BY 6 INCHES. OSBORN

RUIN.

FIG. 2.—DANCING FIGURE. RED DECORATION. DIAMETER 5 INCHES. OSBORN

RUIN.]

[Illustration: PL. 2

FIG. 1. TWO WOLVES. BLACK AND WHITE WARE. 11 BY 5½ INCHES. OSBORN

RUIN.

FIG. 2. MOUNTAIN SHEEP. BLACK AND WHITE WARE. 11 BY 5½ INCHES.

OSBORN RUIN.]

[Illustration: PL. 3

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