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<br />1-& <br />C) <br />(:0 <br />o <br /> <br />'" <br />OQ.f <br />l!" -Sl, <br />., <br /> <br />2 <br />1840) <br /> <br />,~ <br />0' <br />{7001 ~~e <br />1 "Vi" <br />3 <br />(890) <br />Dillon Reseruoir <br />124001 4 <br /> <br />EXPLANATION <br /> <br />~ 1 SAMPLING SITE AND NUMBER <br />ITABLE 2 AND FIGURE 31 <br />17001 SALT LOAD, IN TONS PER YEAR <br /> <br />, <br />. <br />o <br />ii: <br /> <br />11l,20m 5 <br /> Green Mountain <br /> ReserlJolr <br />('1,200) 6 <br />~ <br />"' <br />(11,2001 1 <br /> <br />Figure 5.--Drainage system and salt load: Blue River subbasin. <br /> <br />most of the subbasin. No historical data were available for comparison with <br />sample data. <br /> <br />The Blue River subbasin (site 7) discharged an adjusted estimated annual <br />base flow of 188 ft3/s and a salt load of 11,200 tons (fig. 5). The <br />adjustment factors for Dillon Reservoir and Green Mountain Reservoir resulted <br />in an increase of 27 ft3/s above the measured base flow and a salt load of <br />6,400 ton/yr less than measured salt loads. This adjustment was applied to <br />all affected downstream sites. <br /> <br />Ea~le River <br /> <br />The Eagle River subbasin includes the drainage area of the Eagle River <br />and tributaries upstream from the confluence with the Colorado River. <br />Cambrian and Ordovician limestones and dolomites crop out in the headwaters <br />region west of the Eagle River and upstream from Avon" Colo. Pennsylvanian <br />and Permian sandstones, limestones, dolomites, and shale crop out in the <br />headwaters east of the Eagle River upstream from Avon. Downstream from Avon, <br />there are large areas of the Eagle Valley Evaporite, which contain thick salt <br />beds. In addition, localized deposits of pre-Tertiary conglomerates, <br />sandstones, and shales crop out in this reach. <br /> <br />22 <br />