The Romance of the Colorado River : $b The Story of its Discovery in 1840, with an Account of the Later Explorations, and with Special Reference to the Voyages of Powell through the Line of the Great Canyons — John Shaqi
The Romance of the Colorado River : $b The Story of its Discovery in 1840, with an Account of the Later Explorations, and with Special Reference to the Voyages of Powell through the Line of the Great CanyonsDellenbaugh, Frederick Samuel
History
The Romance of the Colorado River : $b The Story of its Discovery in 1840, with an Account of the Later Explorations, and with Special Reference to the Voyages of Powell through the Line of the Great Canyons
Dellenbaugh, Frederick Samuel
Colorado River (Colo.-Mexico) -- Description and travel; Colorado River (Colo.-Mexico) -- Discovery and exploration; Colorado River Valley (Colo.-Mexico) -- Description and travel; Colorado River Valley (Colo.-Mexico) -- Discovery and exploration; Grand Canyon (Ariz.) -- Description and travel; Gran
Its name is derived from a wonderful echo
of ten words returned from the smooth wall seen in the cut on page 203.
It is only a mile long with walls of 600 feet. At its head enter the
Yampa River and Canyon, which mark the foot of Lodore, the most
striking gorge, next to the Grand Canyon, on the whole river. Lodore is
only 20 miles long, but it is 20 miles of concentrated water-power
energy and grandeur, the fall being about 400 feet, the walls 2700.
Never for a moment does it relax its assault, and the voyager on its
restless, relentless tide, especially at high water, is kept on the
alert. The waters indeed come rushing down with fearful impetuosity,
recalling to Powell the poem of Southey, on the Lodore _he_ knew, hence
the name. The beginning of the gorge is at the foot of Brown’s Park
through what is called the Gate of Lodore, an abrupt gash in the Uinta
Mountains 2000 feet deep. In viewing this entrance the ordinary
spectator is at a loss to comprehend how the stream could have begun
its attack upon this precipitous ridge. The theory that the river was
there before the upheaval formed the mountain does not entirely
satisfy, for it would seem in that case that the canyon walls would
long ago have become much more broken down than they are. But the walls
have a strikingly fresh look, as if formed recently, compared with the
time of the original upheaval. It seems possible that there may have
been in this region some great lake which lifted the waters up to the
top of the ridge to begin their work of corrasion. Such lakes did
exist; but lack of space forbids the further pursuit of this discussion
here.
[9] The character of the Grand River is similar to that of the Green,
but the canyons above the mouth of the Dolores are not so long nor so
deep. The river also carries less water.
Pinnacles in Split Mountain Canyon. Pinnacles in Split Mountain Canyon.
Photograph by E.O. BEAMAN, U.S. Colo. Riv. Exp.
Head of the Canyon of Lodore just inside the “Gate”. Head of the Canyon
of Lodore just inside the “Gate”.
Walls 2500 feet high; river 300 feet wide.
Photograph by E.O. BEAMAN, U.S. Colo. Riv. Exp.
Pot-hole in Intermittent Water Course, Glen Canyon. Pot-hole in
Intermittent Water Course, Glen Canyon.
Homogeneous sandstone. These holes are often 10 to 15 feet deep, with
the stones which ground them lying in the bottom.
Photograph by J. FENNEMORE, U.S. Colo. Riv. Exp.
Public-domain text, read in full here on John Shaqi.
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