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• <br />Consumptive Uses and Losses 5 <br />Lesser structures downstream include Senator Wash, Laguna, Headgate Rock, Palo Verde, <br />Imperial, and Morelos Dams. Senator Wash and Laguna Dams provide very limited <br />amounts of reregulation capacity, while the others are used principally for diversions. <br />Diversions below Lake Mead for agriculture, municipal and industrial, power, export, <br />and other purposes are of the magnitude of six million acre -feet annually. A portion of these <br />diversions is satisfied from upstream return flows. Yuma and Lake Havasu City <br />in Arizona and Needles and Blythe in California are the major cities along the main stem <br />below Lake Mead. Current irrigated lands adjacent to the main stem are estimated to cover <br />approximately 275,000 acres. <br />Tributary Area Above Lake Mead, Arizona - Nevada -Utah <br />Development away from the Colorado River main stem is limited by the availability of water <br />and the rugged terrain. <br />Most of the irrigated lands in this area are located in the lower reach of the Virgin River and <br />Las Vegas Valley in Nevada, on Kanab Creek in Arizona and Utah. Reporting period <br />irrigated land averaged approximately 12,500 acres. <br />North Las Vegas, Las Vegas, Henderson, and Boulder City in Nevada, are the leading cities <br />in the area. <br />0 Tributary Area Below Lake Mead, Arizona <br />As discussed above, development away from the Colorado River main stem is limited by the <br />availability of water and the rugged terrain. <br />Most of the irrigated lands in this area are located in the lower portions of the Gila and Bill <br />Williams Rivers in Arizona. Kingman and Williams in Arizona, are the leading cities. <br />Little Colorado River, Arizona -New Mexico <br />The Little Colorado River drainage area occupies a large part of northern Arizona and <br />a portion of west - central New Mexico. It originates on the north slopes of the White <br />Mountains about 20 miles above Springerville, Arizona. The river has a main stem length of <br />about 356 miles and joins the Colorado River on the east boundary of Grand Canyon <br />National Park about 78 miles downstream from Glen Canyon Dam. <br />A series of saline springs near the mouth of the Little Colorado River produces an estimated <br />160,000 acre -feet of water annually. The U.S. Geological Survey (USGS) gauging station <br />near Cameron, Arizona, is located on the Navajo Indian Reservation about 45 miles <br />upstream from the mouth. Streamflow is undependable and erratic and <br />is subject to flash floods of considerable magnitude. Flow at the gauging station during <br />the 1996 -2000 period varied from 16,990 acre -feet in 1996 to 138,000 acre -feet in 1998. <br />Only minor development of the ground water has occurred because of low yields and poor <br />quality. Excessive erosion and sediment deposition plague the area. <br />