View to the northwest with
Blacktail Canyon slightly below the center while Forster Canyon enters
from the left edge. The South Rim stretches across the top edge with
Fossil Canyon near the center, and reaches out toward Great Thumb Point
at the upper right.
The Tapeats Sandstone and Bright Angel Shale layers are
once again next to the river, as the Precambrian layers have not been
exposed here yet. The Colorado River straightens out for a few miles
and serenely marches down Conquistador Aisle - bordered on both sides
by massive cliffs of Redwall/Muav Limestone.
The Kaibab/Toroweap/Coconino complex still forms the cliff
at the rim, but the broad flat Esplanade Sandstone surface is becoming
more prevalent. The Esplanade surface defines what was here before the
Colorado River overflowed the Kaibab Plateau about 5.4 million years
ago. Earlier in the Miocene, the Hualapai drainage system had eroded
broad canyons down to the Esplanade surface. By 6 million years ago
this area looked like many other areas in the southwestern U.S. that
are characterized by broad valleys that are bounded by steep canyon
walls rising abruptly up to flat-topped mesas. When the river started
flowing through here about 5.4 million years ago, it quickly eroded
downward to cut the inner canyon.
View to the northeast with
Fossil Canyon and Great Thumb Point on the left (South Rim) side of the
river. A piece of the Powell Plateau (North Rim) can be seen in the
upper right corner. 128 Mile Canyon is not exactly noteworthy, but it
joins the right hand side of the river just after it bends back
slightly to the right.
Fossil Canyon is aptly named. The Bright Angel Shale in
this area has many fossils over 500 million years old.
This part of the river (that section that flows
northeastward) is also interesting as it is flowing into rising strata
layers. (Also rising surface topography if you disallow the canyon.) At
one time it was thought that a "pirate stream" eroding from the west
side of the Kaibab Plateau captured an ancestral Colorado River that
existed to the east of the plateau. However, this would require the
headwall erosion of the "pirate stream" to actually work its way back
downhill through this section. This is of course impossible which is
one of the reasons we can confidently say there was no "pirate
stream".
Return to river miles 112 to 120
Continue to river
miles 128 to 136
Return to the
Index Page for the Grand Canyon Tour
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