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<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 />