Titan of Chasms: The Grand Canyon of Arizona — John Shaqi
Titan of Chasms: The Grand Canyon of ArizonaPowell, John Wesley
History
Titan of Chasms: The Grand Canyon of Arizona
Powell, John Wesley
Grand Canyon (Ariz.)
To the west of the Kanab Plateau are the Uinkaret Mountains—an immense
group of volcanic cones upon a plateau. Some of these cones stand very
near the brink of the Grand Canyon and from one of them a flood of
basalt was poured into the canyon itself. Not long ago geologically, but
rather long when reckoned in years of human history, this flood of lava
rolled down the canyon for more than _fifty miles_, filling it to the
depth of _two_ or _three hundred feet_ and diverting the course of the
river against one or the other of its banks. Many of the cones are of
red cinder, while sometimes the lava is piled up into huge mountains
which are covered with forest. To the west of the Uinkaret Mountains
spreads the great Shiwits Plateau, crowned by Mount Dellenbough.
Past the south end of these plateaus runs the Colorado River; southward
through Marble Canyon and in the Grand Canyon, then northwestward past
the Kaibab and Shinumo Canyon, then southwestward past the Kanab
Plateau, Uinkaret Mountains to the southernmost point of the Shiwits
Plateau, and then northwestward to the Grand Wash Cliffs. Its distance
in this course is little more than 300 miles—but the 300 miles of river
are set on every side with cliffs, buttes, towers, pinnacles,
amphitheaters, caves, and terraces, exquisitely storm-carved and painted
in an endless variety of colors.
The plateau to the south of the Grand Canyon, which we need not describe
in parts, is largely covered with a gigantic forest. There are many
volcanic mountains and many treeless valleys. In the high forest there
are beautiful glades with little stretches of meadow which are spread in
summer with a parterre of flowers of many colors. This upper region is
the garden of the world. When I was first there bear, deer, antelope,
and wild turkeys abounded, but now they are becoming scarce. Widely
scattered throughout the plateau are small canyons, each one a few miles
in length and a few hundred feet in depth. Throughout their course
cliff-dweller ruins are found. In the highland glades and along the
valley, pueblo ruins are widely scattered, but the strangest sights of
all the things due to prehistoric man are the cave dwellings that are
dug in the tops of cinder cones and the villages that were built in the
caves of volcanic cliffs. If now I have succeeded in creating a picture
of the plateau I will attempt a brief description of the canyon.
[Illustration: Copyright, 1899, by H. G. Peabody.
Bissell Point and Colorado River.]
Marble Canyon
Public-domain text, read in full here on John Shaqi.
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