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<br />. <br /> <br />along. the lower reaches of the Colorado. .Over a large portion of the <br /> <br />w <br />ao <br />N <br />W <br /> <br />lower valleys 50 to 60 inches is an overall average for evaporation. <br /> <br />. <br /> <br />Physiography. The drainage basin of the Colorado River is about <br /> <br />250,000 square miles. The Colorado River is l,440 miles long and its <br /> <br />. <br /> <br />drainage basin extends into five physiographic provinces. lts headwaters <br /> <br />originate in the Southern and Middle Rocky Mountains and the river flows <br /> <br />through the Wyoming Basin, The Colorado Plateau, and the Basin and <br /> <br />. <br /> <br />Range province in its lower reaches. More than half of the drainage ba- <br /> <br />sin is contained in the Colorado Plateau. This plateau was uplifted and <br /> <br />tilted northeast in geologic time, forming a temporary block of the river. <br /> <br />. <br /> <br />The Colorado River, where it leaves the Colorado Plateau, formed the <br /> <br />Grand Canyon as it cut across the rim of the plateau. <br /> <br />. <br /> <br />For that portion of the river which rises in the Southern Rocky <br /> <br />Mountains much of the area is higher than lO, 000 feet in altitude with <br /> <br />peaks reaching more than l4, 000 feet. Much of the Colorado Plateau is <br /> <br />. <br /> <br />between 5,000 and 7,000 feet in altitude and the river crosses this pro- <br /> <br />vince in deep canyons where it exits in the Grand Canyon. In the Basin <br /> <br />. <br /> <br />and Range province the river is below 2,000 feet in altitude. <br /> <br />In the Wyoming Basin, the relief along the Green River, the chief <br /> <br />tributary of the Colorado, is relatively minor and in places the valley <br /> <br />. <br /> <br />bottoms are wide. ln contrast, where the river flows through the middle <br /> <br />and southern Rocky Mountains the valleys are steep sided, generally <br /> <br />narrow am 2,000 to 3,000 feet deep where they cross the mountain <br /> <br />. <br /> <br />4 <br /> <br />. <br />