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<br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />UESCRIPTIO~ OF BASl~ <br /> <br />E. Hydrology <br /> <br />~ The Colorado Riv~r begins ....here peaks rise more than 14,000 feet <br />o high in the northwest portion of Colorado's Rocky :-lountain ;<;at100al Park, <br />o ]0 miles northwl'st of Denver. It r!'I{,ilndcrs solJt.h~st for 040 miles througb <br />::.....~ the Upper Basin to Lee Ferry. The Green Riv~'r. its major tributary, <br />rises in ....estern ~yoming and discharges into the Colorado River in SQuth- <br />t..'i1stern Utah--7JO river miles south of its origin and 220 miles above <br />It:'e Ferry. The Green River drains 70 percent more area than the Colorado <br />River above their junction but produces only about three-fourths as much <br />water. The Gunnison and the San Juan are the other principal tributaries <br />of the Upper Colorado River. <br /> <br />The flo""s of the San Juan Rivl"r ar(' no.... controlled by tile :;avajo <br />Dam, the Green RiVer by Fontenellc and Flaming Gorge Dams, and the Gunn- <br />ison River by the Cur~canti Unil Dam~. Glen C..mvon n,lm is tlJt:~ only major <br />darn on the main stem of the Colorado ahovl:' Lee Ferry, but it .....ill permit <br />control of almost all flows leaving the l:pper Basin. <br /> <br />The flow at various points in streams in the COlorilda River Basin <br />for the 1941-72 period is ~iven in Tables 1 throu~h 17. The records <br />uf flo..... dt'pict the characteristic wide fluctuations from month-to-ronth <br />and the considerable variation from year-to-year. The storage reservoirs <br />no..... level out oomt> of the fluctuations in the r.:!.3ches b('low the dam. <br /> <br />The natur."Jl drainage area of thte' lower Colorado River belo.... Lee <br />Ferry and above Imperial Dam is about 75.100 square miles. This section <br />of the river is no.... larp:e.:ly controlled by" B('ries of stor."Jge ,lnd diver- <br />sion dams startinp: with Hoover Dam and. endinp: at Imperial Dam. <br /> <br />At the present time there is no significant stora~e on tile main <br />rivt:>r or on the tributaries between Glen Canyon Dam and Lake ~lead. The <br />intervening tributary inflo.... is erratic but amounts to almost enough <br />to offset the t'vaporation from Lake Mead. <br /> <br />Lake :1e."Jd provides most of the storage and regulation in the Lo....er <br />Colorado River Rasin with the \oGter bein~ stored for irri~ation and munic- <br />ip.al and industrial uses. ~eneration of el('ctrical po....er. and other he-ne- <br />ffcial uses. <br /> <br />Lake Hohave. the reservoir formed by Davis Dam. backs \oI(Her at high <br />stages about 67 miles upstream to the tailrace of Hoover Po....erplant. <br />Storage in Lake ~Iohave is used for some reregulation of releases from <br />Hoover Oa;:!. for meeting treaty requirements ....ith ~lexico. and for devel- <br />oping power head for the production of electrical eneq~y at Davis Power- <br />plan t. <br /> <br />13 <br /> <br />