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<br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br />Figure 3. Pre- and post-impoundment patterns of discharge in the Colorado River <br />mainstream in Grand Canyon, downstream from Glen Canyon Dam. <br /> <br />tributary to the Colorado (Fig. 1), originates in <br />highlands of Arizona and New Mexico. The Rio <br />Yaqui in Mexico similarly passes from the northern <br />Sierra Madre Occidental through hot desert lowlands <br />to the sea. <br />These rivers were characterized by remarkable <br />variation in discharge (Fig. 3). Floods from spring <br />snowmelt in the north and both during regional <br />winter rains and late summer monsoons in the <br />south, are followed by mere trickles under the <br />intense evaporation and minimal precipitation <br />during early summer and autumn droughts. Down- <br />cutting of canyons and transport of tremendous <br />volumes of sediments are the rule. Canyons alternate <br />with reaches flowing through broader floodplains, <br />and diversity is high (Fig. 4). Where floodplains are <br />wide, gallery forests and woodlands of cottonwood, <br />willow, and other trees formerly lined desert <br />watercourses; extensive marshes occupied their <br />backwaters. Water tables were only a few feet <br /> <br />beneath the surface in even the driest desert basins, <br />and seepage maintained rivers, or at least filled pool <br />in protected canyons during major droughts. <br />The situation changed dramatically with <br />intervention of technological humans. Now, floods <br />alternating with intermittency in drought are an <br />exception rather than the rule (Fig. 3). Rivers are <br />dammed before they leave the mountains. Flood <br />waters and sediments are caught in reservoirs, and <br />water is released as needed for irrigation, power <br />generation, and domestic use. Low flow occurs when <br />humans deem it so; dams can be closed and rivers <br />turned off like a kitchen tap. <br />Far more surface water exists today than before, <br />but it is in quiet reservoirs markedly different from <br />the originally turbulent streams (Fig. 5). Canals <br />instead of streams, lined with concrete and chain-linl <br />fence rather than riparian trees, descend from- <br />reservoirs to and through the lowlands (Fig. 6). <br />Sediment carried downstream in flood is no longer <br /> <br />3 <br />