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Canyons of the Colorado by J. W. Powell
page 24 of 264 (09%)

A hundred miles to the northwest of the Zuni pueblo are the seven
pueblos of Tusayan: Oraibi, Shumopavi, Shupaulovi, Mashongnavi,
Sichumovi, Walpi, and llano. These towns are built on high cliffs. The
people speak a language radically different from that of the Zuni, but,
with the exception of that of the inhabitants of Hano, closely allied to
that of the Utes. The people of Hano are Tewans, whose ancestors moved
from the Rio Grande to Tusayan during the great Pueblo revolt against
Spanish authority in 1680-96.

Between the Little Colorado and the Rio San Juan there is a vast system
of plateaus, mesas, and buttes, volcanic mountains, volcanic cones, and
volcanic cinder cones. Some of the plateaus are forest-clad and have
perennial waters and are gemmed with lakelets. The mesas are sometimes
treeless, but are often covered with low, straggling, gnarled cedars and
pifions, trees that are intermediate in size between the bushes of sage
in the desert and the forest trees of the elevated regions. On the
western margin of this district the great Navajo Mountain stands, on the
brink of Glen Canyon, and from its summit many of the stupendous gorges
of the Colorado River can be seen. Central in the region stand the
Carrizo Mountains, the Lukachukai Mountains, the Tunitcha Mountains, and
the Chusca Mountains, which in fact constitute one system, extending
from north to south in the order named. These are really plateaus
crowned with volcanic peaks.

But the district we are now describing, which stretches from the Little
Colorado to the San Juan, is best characterized by its canyons. The
whole region is a labyrinth of gorges. On the west the Navajo Creek and
its tributaries run in profound chasms. Farther south the Moencopie with
its tributaries is a labyrinth of gorges; and all the streams that run
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