The Mentor: Reclaiming the Desert, Vol. 6, Num. 17, Serial No. 165, October 15, 1918 — John Shaqi
The Mentor: Reclaiming the Desert, Vol. 6, Num. 17, Serial No. 165, October 15, 1918Blanchard, C. J. (Clarence John)
History
The Mentor: Reclaiming the Desert, Vol. 6, Num. 17, Serial No. 165, October 15, 1918
Blanchard, C. J. (Clarence John)
Desert reclamation -- Southwest, New; Desert resources development -- Southwest, New; Irrigation -- Southest, New
As to water supply, the desert belongs in two regions, arid and
semi-arid. West of the Missouri and extending to the foot of the Rocky
Mountains, is a vast area of foothills and gently sloping, grassy
prairies, which constitute a large part of the semi-arid or sub-humid
region of the United States. This broad belt, stretching from Mexico
northward into Canada, has no clear-cut boundary separating it from
the humid region on the east or the arid region on the west, owing to
the variance of the mean annual precipitation in many localities. A
convenient and easily marked line for the eastern boundary of the arid
region is one closely following the hundred and third meridian. On the
north it bends away from the meridian toward the west, and on the south
tends eastward north of the Rio Grande. On the west the arid region
extends to the Pacific Coast in extreme southern California, but from
Monterey north there is a narrow belt of semi-arid and humid country
bordering the Pacific Ocean. The Coast Range is humid, especially in
Oregon and Washington, where the rainfall is as heavy as in any other
part of the United States.
[Illustration: FORTY BUSHELS OF WHEAT PER ACRE
Shoshone Project, Wyoming. This was desert land in 1915]
The true desert, wherein the production of crops is wholly dependent
upon the artificial application of water, lies for the most part west
of the Rocky Mountains. Its estimated area, 900,000 square miles,
is probably slightly greater than that of the semi-arid region. An
accurate determination of the relative size of each, however, is not
possible until a comprehensive hydrographic survey has been completed.
Contrary to popular opinion, this region is not a vast wilderness,
desolate and unpromising. Between the mountain ranges lie many
beautiful valleys, through which flow numerous streams fed by melting
snows. Utah and Nevada contain large areas of sage-brush desert,
comprising what is known as the Great Basin, which has no outlet to
the sea, and is doomed to aridity by reason of the absence of living
streams. Millions of acres of desert now inhabited by the coyote and
the rattlesnake await only the coming of the engineer to wake to
teeming fecundity.
In one important respect the arid and semi-arid regions are alike, and
that is in the character of the streams. Almost without exception the
rivers of the West are erratic and “flashy” in flow, are subject to
long periods of drought and sudden and destructive floods. The full
utilization of these streams for irrigation and power necessitates
storage. In the control of floods, engineers have found their greatest
problem, and one whose solution has taxed the skill, imagination and
daring of twentieth-century genius.
[Illustration: WHEAT ON SHOSHONE PROJECT, WYOMING
This land was desert in 1908]
_National Irrigation_
Public-domain text, read in full here on John Shaqi.
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