<br />..Erincipal crops are alfalfa, cotton, barley, watermelons, cantaloupes, lettuce and pasture. The crop
<br />~alue in 1952 was $13,000,000 plus $7,500,000 for livestock. The raising of livestock is increasing in
<br />;}1nportance. .
<br />
<br />N The reinforced concrete structure, now known as the old intake, was built in 1908, the floor ele-
<br />'vation is 274.0. The structure was widened to eight 6-foot gates in 1917. ~he new intake structure
<br />CWith five 8-foot gates and floor elevation of 278,0 was constructed in 1945 in conjunction with the
<br />temporary rock weir. The District has 269 miles of canals and 108 miles of drains. The amount spent
<br />on construction of works by the District and its predecessors from 1908 to 1953 was approximately
<br />$5,900,000.
<br />
<br />The Colorado River Indian Reservation continues along the river for approximately 52 miles
<br />mostly in Arizona, but embraces some land in California. The reservation contains approximately
<br />243,000 acres of which 100,000 acres of valley land in Arizona are considered irrigable. Approxi-
<br />mately 36,000 acres, in the northern part of this valley near the town of Parker, are now under irri-
<br />gation.
<br />
<br />DIVERSION:
<br />
<br />The water surface of the Colorado River at the Palo Verde Intake was of such elevation that
<br />the District could and did satisfactorily irrigate all cultivated land within approximately 90% of its
<br />gross valley area from 1908 to 1935 when the construction of Hoover Dam changed the regimen of
<br />the stream, It is also well to note that the district could and did satisfactorily irrigate during this
<br />period all cultivated land within 94.2 percent of that area considered feasible for gravity diversion.
<br />The gross area of the valley is 104,500 acres. There are 5200 acres near the intake that were never
<br />considered feasible for gravity irrigation. This area went into cultivation in 1941 and pumps from
<br />elevation 286,3. A second area of 5800 gross acres is the area which caused irrigation difficulty in
<br />1928 to 1934; this is 5.8 percent of the gross area considered feasible for gravity irrigation.
<br />
<br />The average daily elevation of the river at Palo Verde intake from 1909 (when the gauge was
<br />established) to February 1935 (when Hoover Dam was closed was 285,9. To irrigate that por-
<br />tion of the district considered feasible for gravity irrigation (99,300 acres) requires an intake
<br />canal elevation of 286,3. However, elevation 286.3 is necessary only for 5800 acres or 5.8 percent
<br />of the area. Approximately 94.2 percent can be irrigated from an intake canal elevation of 282,3.
<br />In the 26 years from January 3, 1909 to February 1, 1935 the river was below 282.3 for only 232
<br />days or 2.44 percent of the time, hence the Palo Verde Irrigation District feels that its obligation to-
<br />ward the cost of a solution to the diversion problem is the obligation of this 5800-acre area only,
<br />
<br />About 1927, some changes were made by the District in the river channel along the valley to
<br />improve flood protection, thereby lowering the water surface at the intake. In 1928, pumps were in-
<br />stalled on Main Canal to give a lift of less than two feet for irrigation of a 1,400-acre portion of
<br />the previously mentioned 5800-acre area in the north end of the valley. In 1931, another pump was
<br />installed at the lower end of the settling basin to pump into Duplicate Main Canal (high level). These
<br />pumps were operated until about 1934 when normal changes in the river raised the water surface so
<br />that the pumps were no longer needed.
<br />
<br />Hoover Dam was closed in February 1935. Silt carried by the river upstream from that point
<br />was impounded by the dam. The clear water from Hoover Dam exerted a scouring or degrading
<br />effect upon the bed of the stream. Engineers call this retrogression. In other words, the silt in the
<br />stream bed below the dam moves on downstream but can not be replaced by silt from upstream. This
<br />causes the stream bed to lower, thus lowering the water surface. The effect of retrogression was
<br />not immediately evident because of intervening distance (214 miles), nor was it felt following the
<br />closure of Parker Dam (59 miles upstream) in November 1938. But upon closure of Headgate Rock
<br />Dam (44 miles upstream) in March 1942 the effect was almost i=ediate. In 1943 the district in-
<br />stalled pumps within its canal system to provide water for the high lands and in 1944 Congress auth-
<br />orized construction of the temporary rock weir (First Deficiency Appropriation Act 1944, 58
<br />Stat. 150, 157), with an appropriation of $250,000, to maintain the water surface of the river at an
<br />elevation such that the district could divert its needs by gravity. The weir was completed in
<br />June 1945,
<br />
<br />Also in 1945, the Secretary of Interior requested the Bureaus of Reclamation and Indian Af-
<br />fairs to make a survey and investigation and to submit a joint report on a permanent solution to the
<br />Palo Verde diversion problem. This report was submitted March 26,1947, and covered four pos-
<br />sible plans:
<br />
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