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Canyons of the Colorado by J. W. Powell
page 51 of 264 (19%)
to the plateau, I found that a great storm had swept the land, and the
dry arroyos of the day before were the channels of a thousand streams of
tawny water, born of the ocean of vapor which had invaded the land
before my vision.

Below the Pink Cliffs another irregular zone of plateaus is found,
stretching out to the margin of the Gray Cliffs. The Gray Cliffs are
composed of a homogeneous sandstone which in some places weathers gray,
but in others is as white as virgin snow. On the top of these cliffs
hills and sand-dunes are found, but everywhere on the Gray Cliff margin
the rocks are carved in fantastic forms; not in buttes and towers and
pinnacles, but in great rounded bosses of rock.

The Virgen River heads back in the Pink Cliffs of the Markagunt Plateau
and with its tributaries crosses one of these plateaus above the Gray
Cliffs, carving a labyrinth of deep gorges. This is known as the Colob
Plateau. Above, there is a vast landscape of naked, white and gray
sandstone, billowing in fantastic bosses. On the margins of the canyons
these are rounded off into great vertical walls, and at the bottom of
every winding canyon a beautiful stream of water is found running over
quicksands. Sometimes the streams in their curving have cut under the
rocks, and overhanging cliffs of towering altitudes are seen; and somber
chambers are found between buttresses that uphold the walls. Among the
Indians this is known as the "Rock Rovers' Land," and is peopled by
mythic beings of uncanny traits.

Below the Gray Cliffs another zone of plateaus is found, separated by
the north-and-south faults and divided from the Colob series by the Gray
Cliffs and demarcated from the plateaus to the south by the Vermilion
Cliffs. The Vermilion Cliffs that face the south are of surpassing
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