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<br /> <br /> <br />Figure 4. Left: Canyon-bound reaches alternating with more open sections in bends <br />characterize most desert rivers (San Juan River, photograph by U.S. Bureau of <br />Reclamation). Right: In wider, valley sections, meandering channels and sandbars are <br />common and riparian woodlands develop on floodplains (Gila River, New Mexico). <br /> <br /> <br /> <br />Figure 5. Left: Boulder Canyon reach of the Colorado River prior to Hoover Dam, <br />contrasted with; Right: the same reach after the dam was in place to form Lake <br />Mead, Arizona.Nevada (photographs provided by U.S. Bureau of Reclamation). <br /> <br /> <br />replaced from above, and unlined channels soon are <br />deeply incised. Arroyo cutting (Fig. 7) due to <br />watershed abuse such as overgrazing stimulates <br />further erosion, draining water tables to decrease <br />stability even more. Groundwater is pumped from <br />beneath the desert floor far faster than it is restored, <br />seepage into channels fails as water tables drop, and <br />streams cease to flow. Riparian vegetation disappears, <br /> <br />Figure 6. Imperial Dam, Arizona-California, a major diversion <br />on the lower Colorado River, from which canals supply <br />agricultural and domestic water for southern California <br />(photograph provided by U.S. Bureau of Reclamation). <br /> <br />4 <br />