The foreground in this view
to the west illustrates how Unkar Creek’s debris fan deflects the
Colorado River. Unkar Creek originates off the North Rim (right) and
drains the easily eroded Dox Formation. The large amount of debris that
it deposits pushes the river to the left out of its normal course.
In relatively recent times, some of these debris flows
have created small dams at Unkar Delta. The river would then back up
and deposit a lot river gravel upstream from these dams before it could
cut back down to its original level. Remnants of these old river gravel
deposits are still visible along both sides of the river for half a
dozen miles back upstream.
A
few miles further downstream the up-to-the-west tilt of the Grand
Canyon Supergroup brings the much harder Shinumo Quartzite above ground
level to form a cliff just before the river turns westward.
The small segment of the South Rim visible in the upper
left corner is Shoshone Point (a few miles east of Grand Canyon
Village), while Wotans Throne, Cape Royal, and a small section of the
Walhalla Plateau (North Rim) can be seen in the upper right corner.
The river gradient continues steeper in the western Dox
area than it was east of the Butte Fault. Then, the steepest river
gradient in the entire Grand Canyon is encountered in the area around
Hance Rapid after the sharp bend in the river toward the west-northwest.
View to the west-northwest.
In the foreground the Colorado River turns a corner and plunges down
Hance Rapid with the average river gradient in this section (about 18
ft/mi) the steepest in the Grand Canyon. The steep gradient is a result
of three different factors. First, the debris fan from Red Canyon
(enters from left edge) would normally create a rapid. Next, this area
is on the west (downhill) side of the axis of the Kaibab Plateau.
Finally, the river is crossing from the hard Shinumo Quartzite to the
more easily eroded underlying Hakatai Shale.
As part of the Grand Canyon Supergroup, the Hakatai Shale
also tilts upward to the west and forms a small upward tilting slope in
the right side of the canyon just below Hance Rapid. Then at the
river's leftmost position in the picture, the Bass Limestone and Vishnu
Schist are encountered and the river enters Upper Granite Gorge.
River mile 80 is reached where the river turns slightly
further to the right before disappearing from view. Cottonwood Creek
enters from the left just after this bend to the right.
Return to
river miles 64 to 72
Continue to river
miles 80 to 88
Return to the
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