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
The horticultural conditions here, while essentially the same as those
of the whole pueblo region, present some peculiar features. Except for a
few modern examples there are no traces of irrigating works, and the
Navaho work can not be regarded as a success. The village builders
probably did not require irrigation for the successful cultivation of
their crops, and under the ordinary Indian methods of planting and
cultivation a failure to harvest a good crop was probably rare. After
the Harvest season it is the practice of the Navaho to abandon the
canyon for the winter, driving their flocks and carrying the season's
produce to more open localities in the neighboring valleys. The canyon
is not a desirable place of residence in the winter to a people who live
in the saddle and have large flocks of sheep and goats, but there is no
evidence that the old inhabitants followed the Navaho practice.
During most of the year there is no water in the lower 10 miles of the
canyons, where most of the cultivable land is situated. The autumn rains
in the mountains, which occur late in July or early in August, sometimes
send down a little stream, which, however, generally lasts but a few
days and fails to reach the mouth of the canyon. Late in October, or
early in November, a small amount comes down and is fairly permanent
through the winter and spring. The stream bed is even more tortuous than
the canyon it occupies, often washing the cliffs on one side, then
passing directly across the bottom and returning again to the same side,
the stream bed being many times wider than the stream, which constantly
shifts its channel. In December it becomes very cold and so much of the
stream is in shade during a large part of the day that much of the water
becomes frozen and, as it were, held in place. In the warm parts of the
day, and in the sunshine, the ice is melted, the stream resumes its
flow, and so gradually pushes its way farther and farther down the
canyon. But some sections, less exposed to warmth than others, retain
their ice during the day. These points are flooded by the water from
above, which is again frozen during the night and again flooded the next
day, and so on. In a short time great fields of smooth ice are formed,
which render travel on horseback very difficult and even dangerous.
This, and the scant grazing afforded by the bottom lands in winter,
doubtless is the cause of the annual migration of the Navaho; but these
conditions would not materially affect a people living in the canyon who
did not possess or were but scantily supplied with horses and sheep. The
stream when it is flowing is seldom more than a foot deep, generally
only a few inches, except in times of flood, when it becomes a raging
torrent, carrying everything before it. Hence irrigation would be
impracticable, even if its principles were known, nor is it essential
here to successful horticulture.
Public-domain text, read in full here on John Shaqi.
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