Your National Parks, with Detailed Information for TouristsMills, Enos A.
Philosophy
Your National Parks, with Detailed Information for Tourists
Mills, Enos A.
National parks and reserves -- Canada; National parks and reserves -- United States; West (U.S.) -- Guidebooks
Well may the Cañon of the Colorado be called the greatest inanimate
wonder in the world. Written in the exposed and remaining rock-strata
through which the river has cut its way is a wonderful story of the
past, a marvelous and splendid romance. At an enormously remote time
the Grand Cañon plateau rose from the primeval sea. After long
exposure and great weathering it sank back, remained submerged for
ages, and thousands of feet of strata were deposited upon it. Again it
emerged, was exposed "a million years and a day," during which æon
thousands of feet of strata were eroded away. Again it went down into
the sea, and upon it were piled thousands of feet of additional
strata. A fourth time it rose slowly above the water. As this plateau
was rising, its surface was acted upon by the elements. The part of
the plateau surrounding the Grand Cañon proper was the scene of
repeated volcanic action and earthquake disturbance. Here the strata
have been subjected to repeated faultings, heavings, tiltings, and
lava-flows. This uplift imprisoned an enormous Eocene lake that
occupied much of what is now the Colorado River basin. This lake the
river drained. The drainage was quite probably caused by the fact that
the eastern part of the territory was uplifted higher than the
western. The drainage-system of the Colorado River, as we now know it,
began at that time to take on form and its waters started to cut the
cañon. This crude outline covers cycling ages, and probably represents
millions of years.
Through several thousand years the plateau slowly rose, and all this
time the river was gradually cutting its way down into it. Finally the
plateau ceased to rise and long remained at a standstill. After
cutting down to its first base level, the river had so little fall
that its waters, overladen with débris, ceased deepening the channel.
The widening of the cañon went steadily on. Again the plateau slowly
rose, perhaps two thousand feet. This uplift increased the fall of the
river and again set it to deepening its channel, a work it is still
doing.
The waters of the Colorado River are heavily laden with sediment.
During the ages it has transported an inconceivable bulk of eroded
material to the ocean. Much of this has come from its three hundred
thousand square miles of mountainous drainage basin and all the
material which formerly occupied the vast spaces of its numerous
cañons. Continual caving of the walls compels the river to spend most
of its time and energy in breaking up this débris and carrying it
forward to the sea. This condition has existed for thousands of years.
Public-domain text, read in full here on John Shaqi.
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