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<br />. <br />be used to compare the present condition of the Colorado River. Man's im- <br /> <br />Table 6. Estimate of Habitat Change Due to Major Reservoir <br />Construction in Principal Reaches of the Colorado <br />River Basin <br /> <br />pact on the environmental characteristics of the Colorado River Basin can <br /> <br />be categorized into three broadly defined areas: (1) effects caused by <br /> <br />water resource management diversions and consumptive uses (dams. hydro- <br /> <br /> <br />Mil es <br /> <br />electric power. flow control. inter- and intra-basin diversions); (2) ef- <br /> <br />Reservoir <br />length <br /> <br />fects of various economic activities and land uses; and (3) effects of <br /> <br />River <br />length <br /> <br />introducing alien floral and faunal species and of other changes in the <br /> <br />1~440 <br /> <br />Colorado-Mainstream <br />(Mexican border to headwaters) <br />Laguna Dam <br />Imperial Dam <br />Lake Havasu <br />Lake Mo jave <br />Lake Mead <br />Lake Powell <br /> <br />5 <br />30 <br />80 <br />65 <br />105 <br />175 <br /> <br />biotic community. <br /> <br />Water Management. Because of reservoir development in the basin, <br /> <br />particularly Flaming Gorge and Glen Canyon Dam (Lake Powell). the varia- <br /> <br />ble flows and velocities of the river have been sharply altered through <br /> <br />Green River <br />Flaming Gorge <br />Fontenelle <br /> <br />50 <br />15 <br /> <br />inundation of river reaches and flow alteration by reservoir releases <br /> <br />(see table 6). The consequences of constructing the present dams have <br /> <br />Gunnison <br />Blue Mesa Reservoir and <br />Morrow Point Reservoir <br /> <br />40 <br /> <br />been to reduce the silt-carrying capacity of the rivers. reduce flows <br /> <br />downstream. increase salt concentrations (from increased evaporation), <br /> <br />San Juan <br />Navajo Reservoir <br /> <br />35 <br /> <br />change the types and quantities of biota residing in the river. and change <br /> <br />Gila <br /> <br />recreational potential (amount of use as well as type of use). <br /> <br />Painted Rock <br />San carlos <br />Roosevelt <br />Horse Shoe <br />Barlett <br />Lake Pleasant <br /> <br />25 <br />25 <br />30 <br />10 <br />15 <br />10 <br />715 <br /> <br />Stream reaches below dams are affected by a variety of phenomena <br /> <br />which result from the way water is released in the operation of the reser- <br /> <br />voir. The releases from upper basin reservoirs tend to be extremely cold <br /> <br />Total <br /> <br />because the water comes from the lower strata of the reservoir. For ex- <br /> <br />500 <br /> <br />130 <br /> <br />.. <br />~ <br />.. <br />.. <br />~ <br />~ <br />I <br /> <br />370 <br /> <br />~ <br />0( <br />e <br />I <br /> <br />805 <br /> <br />.. <br />- <br />... <br />... <br />... <br />.. <br />> <br />... <br />,.. <br />0( <br /> <br />3.245 <br /> <br />ample. below Flaming Gorge Reservoir, these releases have resulted in a <br /> <br />Note: <br /> <br />700 <br />320b= 0.22; 22% of major reaches of river system dammed. <br /> <br />shift from native fishes to a trout fishery because of the reduced silt <br /> <br />load and because the water is too cold to support other types of fish. <br /> <br />. <br />