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Eagle River Inventory and Assessment
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Eagle River Inventory and Assessment
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Last modified
1/27/2010 11:11:04 AM
Creation date
6/5/2008 4:20:32 PM
Metadata
Fields
Template:
Watershed Protection
Document ID
hr_0003a
County
Eagle
Pitkin
Stream Name
Eagle River
Basin
Colorado Mainstem
Sub-Basin
Eagle 14010003
Water Division
5
Title
Eagle River Inventory and Assessment
Date
8/1/2005
Prepared For
Eagle River Watershed Council
Prepared By
Colorado State University
Watershed Pro - Doc Type
Planning Report
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Gore Creek between the Black Gore confluence and the Eagle River is estimated at 7% and 35%, respectively. <br />Similar patterns exist in the Eagle main stem, particularly between Minturn and Edwards where basin <br />topography, development practicality, and human desires to be near the water place disproportionate <br />development pressures in alluvial valleys, Results of an analysis of the imperviousness of developed areas (an <br />often-cited indicator of stream health) revealed comparable trends. Future development will continue <br />increasing imperviousness as the population of Eagle County approaches anticipated growth of 75% <br />(Colorado Division of Local Government, 2003) over the next 25 years. These patterns are perhaps not <br />surprising but nonetheless underscore the added challenges surrounding management of impervious surfaces, <br />stormwater, and riparian zones in mountainous watersheds with rapidly growing population centers focused <br />in and near ecologically critical zones. <br />ES.4.2 Water Use <br />C~~su~nptiv~ us~ accounts for a~p~oximat~ly 10 ~o ~ 5% of t~~ E~~~~ ~v~r's av~~a~~ an~ual yi~~~ <br />of 410,000 ~c~~ ~~~t a~ t~e Gypsum ~~~e~ 7C~~ ~~eat~st co~su~n~tive use i~ t~e bas~m ~esu~ts ~rorn <br />tr~ns~ou~tain exp~r~s which account for GO% of con~~mp~iv~ ~s~~ Irrigation is the second largest <br />consumptive use at approximately 32%. Domestic/municipal and reservoir evaporation uses are estimated at <br />3% and 4%, respectively. From 1985 to 1995, a shift from irrigation consumptive use to domestic <br />consumptive use was apparent, as was a 54% decrease in irrigation consumptive use. <br />ES.4.3 Hydrology <br />Although the flow regime of the Eagle main stem is more intact than some other rivers of comparable <br />size on the western slope of Colorado, reservoirs and diversions have influenced the flow regime of several <br />segments in the basin. We performed a detailed analysis of current and historical flow regime characteristics <br />at 351ocations in the Eagle River watershed. We have included numerous metrics describing the magnitude, <br />frequency, duration, timing, and rate of change of streamflows at these gaging sites in the main report. <br />Changes in flow regime are most pronounced in Homestake Creek below Homestake Reservoir and in <br />the upper Eagle River below the Wurtz and Columbine Ditches. The combined effects of these flow <br />modifications are transmitted below the confluence of Homestake Creek and the Eagle River through the <br />Eagle Mine site and Minturn, The relative hydrologic effects of these modifications diminish in a step-like <br />fashion as the Eagle main stem accumulates tributary inflows. Reductions in peak flows have both <br />geomorphic and ecological implications discussed in the Edgle River Inventory dnd Assessment. In general, the <br />analysis and description of several ecologically relevant flow attributes performed in this study provide a <br />framework for managing flows with a better understanding of historical variability. <br />Despite distinct shifts in peak flow magnitudes in the upper Eagle and Homestake Creek, differences in <br />pre- and post-alteration low flow regimes are much more subtle, Although there are detectable changes in low <br />flows in the upper Eagle and Homestake Creek, it appears that the most detectable changes in the low flow <br />regime of the Eagle River are associated with a reduction in irrigation return flows and the timing of low flow <br />minima. Thus, it appears that there has been a historical sequence in which baseflows were originally <br />supported by greater overbank flooding during snowmelt, then altered by irrigation diversions, return flows, <br />and peak flow reductions, and most recently reduced by a shift from irrigation to domestic/municipal uses. <br />The net effect of these changes over the last half century is a reduction in low flows in the main stem Eagle in <br />the late summer and fall months when greater irrigation returns formerly supported higher baseflows, <br />ES.4.4 Instream Flows <br />Instream flows rights have been established by Colorado law to "preserve the natural environment to a <br />reasonable degree," In the Eagle River watershed, instream flow rights have priority dates ranging from 1975 <br />Eagle River Inventory and Assessment v <br />
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