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constant from late Agust to early November, with a flow of 13.3 <br />gpm. Ttie flow increased to 24.8 gpm in mid-November and decreased <br />to 18.8 gpm in thelate part of November avid early Part of <br />I <br />December.. <br />I <br />NPDES site 002 (No Name Gulch) recorded a high flow of 445.1 <br />gpro and overall averai~e flow of 85.7 gpro during ':he period (Figure <br />C-2). The high flow observed was most likely dice to snow melt or <br />D-pit pumping during the last part of February z~nd the first part <br />of March. Discharges varied throughout the pe~•iod, showing some <br />of the variability that can be attributed to the precipitation <br />events. <br />The Coyote Dam Seep, below NPDES site 005, showed a constant <br />discharge of 4.7 gpm from July 1 through October 19 until the • <br />recorder was pulled (Figure C-3). <br />Flow data recorded for NPDES site 003 (East Buzzard Gulch) <br />from mid-July to mid-August documents no flow dc.ring this period. <br />NPDES site 006 (W. Buzzard Gulch) recorded a high flow of <br />379.1 gpm during 1991. Figure C-4 presents the i`lows versus time. <br />Low flows dominate the plot with an average flow during the period <br />of 7.4 gpm. Flow at the 10YR/24HR flume Coyote site was not <br />observed during 1991 after Spring melt-out. <br />r1 <br />u <br />a-2 <br />