Durango Bill's
Grand Canyon 3-D Tour
Glen Canyon from Page, AZ to
Lees Ferry, AZ (15.5 river miles)
This first picture
is a view looking southwest from Lake Powell (lower edge),
which is the upstream reservoir above Glen Canyon Dam. The
major highway is US 89 with the town of Page, AZ occupying the
lower left quadrant of the picture.
The early Jurassic Navajo Sandstone dominates
surface rock in this area. 200 million years ago, climate
conditions here were similar to modern-day Egypt. River
systems flowing north from southern Arizona and westward from
Texas carried silt and sand into much of northern Arizona and
southern Utah just as the modern Nile River carries silt and
sand northward from central Africa to Egypt. (Latest evidence
as of September 2003 indicates a large portion of this sand
originated in the present Appalachian Mountains.) During dry
periods, the rivers would shrink, and as the latest silt layer
dried, winds would blow the sand into dunes - just like the
modern Sahara Desert.
The annual process was repeated for millions of
years with the dunes accumulating to over 1,000 feet in
thickness. They were converted into sandstone rock when they
were subsequently buried by thousands of feet of other
sediments. However, if you have a chance to examine the Navajo
Sandstone, traces of these ancient sand dunes can be readily
seen.
In the last 5 million years erosion by the
Colorado River has uncovered the Navajo. The daily heating and
cooling from the sun (expansion followed by contraction)
weakens whatever surface layer is exposed. Then, when the
legendary thunderstorms and flash floods finally arrive, they
wash another thin layer down to the Colorado River, which in
turn transports the sand and silt to its delta in the Gulf of
California.
The second picture
(centered a few miles southwest of picture 1 and still looking
southwest) illustrates entrenched meanders in the Colorado
River. These meanders developed shortly after the Colorado
River found its new route across the Kaibab Plateau about 5.4
million years ago. This area was part of the flat silt plain
that had backed up behind the Colorado's old course across the
rising Wasatch Ranges. When the Colorado switched to its
current path, it was still crossing the flat silt plain. The
river developed meanders similar to meanders seen in the
current Mississippi River. Then, as the Colorado River cut
down through the Kaibab Plateau, canyon cutting worked its way
back upstream. In classical fashion, the river cut downward
into the old sandstone layers and became trapped in its former
meandering course.
The third
picture shows the extreme southwest end of Glen Canyon.
Lees Ferry (the put-in location for Grand Canyon raft
trips) is located where the river becomes completely
visible again. In the distance highway US 89A crosses the
river over Navajo Bridge. To the right the Paria River
enters from the right edge. The Paria Plateau is just
above it.
Surface rock in the foreground is still the
Navajo Sandstone. The red/orange/reddish-brown Triassic
Age Moenave Formation is found in the lower parts of the
canyon and forms the brilliant cliffs just to the
northeast of Lees Ferry.
Continue
to
Grand Canyon - River Miles 0 to 8
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the Index Page for the Grand Canyon Tour
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