The Cliff Ruins of Canyon de Chelly, Arizona: Sixteenth Annual Report of the Bureau of Ethnology to the Secretary of the Smithsonian Institution, 1894-95, Government Printing Office, Washington, 1897, pages 73-198Mindeleff, Cosmos
History
The Cliff Ruins of Canyon de Chelly, Arizona: Sixteenth Annual Report of the Bureau of Ethnology to the Secretary of the Smithsonian Institution, 1894-95, Government Printing Office, Washington, 1897, pages 73-198
Mindeleff, Cosmos
Arizona -- Antiquities; Chelly, Canyon de (Ariz.); Cliff-dwellings -- Arizona; Pueblo Indians -- Antiquities
These conclusions are not based on a study of the ruins in Canyon de
Chelly alone, which illustrate only one phase of the subject, but of all
the pueblo remains, or rather of the remains so far as they are now
known. They imply a rather sparsely settled country, occupied by a
comparatively small number of tribes and subtribes, moving from place to
place under the influence of various motives, some of which we know,
others we can only surmise. It was a slow but practically constant
migratory movement with no definite end or direction in view. The course
of this movement in a geographical way does not as yet reveal a
preponderance in any one direction; tribes and subtribes moved from east
to west and from west to east, from north to south and from south to
north, and many were irregular in their course, but the movements, so
far as they can now be discerned, were all within a circumscribed area.
There is no evidence of any movement from without into the pueblo group,
unless the close relation of the Hopi (Moki) language to the other
Shoshonean dialects be such evidence, and none of a movement from within
this area out of it, although such movements must have taken place, at
least in the early history of the region. It must be borne in mind in
this discussion that while we can assign approximate boundaries to the
ancient pueblo region on the north, east, and west, no limit can as yet
be fixed on the south. The arid country southward of Gila river and
northward of the Mexican boundary would be a great obstacle to a
movement either north or south, but little as we know about that region
we do know that it was not an insurmountable obstacle. The Casas Grandes
of Janos, in Chihuahua, closely resemble the type of ruins on the Gila
river, in Arizona, of which the best example we now have is the
well-known Casa Grande ruin. We know that there are cliff ruins in the
Sierra Madre, but beyond this we know little. Concerning the immense
region which stretches from Gila river to the valley of Mexico, over
1300 miles in length, we know practically nothing.
In that portion of the pueblo region lying within the United States
migratory movements have, as a rule, been confined to very small areas,
each linguistic family moving within its own circumscribed region. Some
instances of movement away from the home region have taken place even in
historic times, as, for example, the migration of a considerable band of
Tewas from the Rio Grande to Tusayan, where they now are, and moreover,
this movement probably occurred en masse and over a considerable
distance; but there is little doubt that the usual procedure was
different.
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