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Canyons of the Colorado by J. W. Powell
page 18 of 264 (06%)
block of the upper side being lifted several thousand feet above the
valley region. Through the fissure lavas poured out, and in many places
the escarpment is concealed by sheets of lava. The canyons in these lava
beds are often of great interest.

On the plateau a number of volcanic mountains are found, and black
cinder cones are scattered in profusion. Through the forest lands are
many beautiful prairies and glades that in midsummer are decked with
gorgeous wild flowers. The rains of the region give source to few
perennial streams, but intermittent streams have carved deep gorges in
the plateau, so that it is divided into many blocks. The upper surface,
although forest-clad and covered with beautiful grasses, is almost
destitute of water. A few springs are found, but they are far apart, and
some of the volcanic craters hold lakelets. The limestone and basaltic
rocks sometimes hold pools of water; and where the basins are deep the
waters are perennial. Such pools are known as "water pockets."

This is the great timber region of Arizona. Not many years ago it was a
vast park for elk, deer, and antelope, and bears and mountain lions were
abundant. This is the last home of the wild turkey in the United States,
for they are still found here in great numbers. San Francisco Peak is
the highest of these volcanic mountains, and about it are grouped in an
irregular way many volcanic cones, one of which presents some remarkable
characteristics. A portion of the cone is of bright reddish cinders,
while the adjacent rocks are of black basalt. The contrast in the
colors is so great that on viewing the mountain from a distance the red
cinders seem to be on fire. From this circumstance the cone has been
named Sunset Peak. When distant from it ten or twenty miles it is hard
to believe that the effect is produced by contrasting colors, for the
peak seems to glow with a light of its own.
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