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Surface waters draining from the sedimentary rock basins <br />associated with the coal deposits may yield higher TDS <br />concentration due to the greater amounts of soluble salts in <br />these rock types. Also, surface water quality in streams <br />draining the area varies on a seasonal basis. <br />The primary drainages in the Upper Yampa River Subbasin related <br />to coal mining activities include both small tributaries and <br />major tributaries. The major tributaries of interest are <br />Trout Creek, Fish Creek, and Oak Creek. These streams general <br />exhibit perennial flow. The small tributaries are <br />Foidel Creek, Middle Creek, and Grassy Creek. These streams <br />flow intermittently in response to snow melt and rainfall <br />events and exhibit no natural base flow (ground water component <br />of flow). Foidel Creek and Middle Creek below Foidel Creek <br />both now flow perennially as a result of underground mine <br />dewatering, and spoil spring discharges leaving the <br />Eckman Park/Foidel Creek Mine complex. <br />A11 disturbed area drainage from the Energy Mine No. 3 enters <br />Middle Creek, which flows north-northeast to Trout Creek and <br />ultimately into the Yampa River (Figure 21. <br />Water discharge and quality data (1975-19831 from U.S.G.S <br />Gaging Station 09243700, located on Middle Creek just above the <br />mine site (see Map 4a of the permit application) were submitted <br />with the permit application. The following discussion <br />simrtnarizes that data and information. <br />Peak discharge in Middle Creek generally occurs from mid-April <br />through mid-June and is the result of snow melt, incident <br />precipitation and alluvial ground water discharge. Maximum <br />recorded discharge is 172 cfs. High monthly discharge occurs <br />in May and averages 21.3 cfs. During the summer months, June <br />through August, the average discharge is 2.03 cfs. There is no <br />flow for numerous days during the year on Middle Creek above <br />Mine No. 3. This no flow condition generally occurs in the <br />fall; therefore, Middle Creek is considered to have no base <br />flow. <br />Surface waters are calcium-bicarbonate in character with a pH <br />range between 7,2 and 8.5. TDS concentrations range from <br />230 mg/1 to 608 mg/1. TDS concentration sometimes shows an <br />inverse relation to streamflow. Total suspended solids (TSS1 <br />range from 5 mg/1 to 599 mg/1. TSS concentration is highest <br />during the high flow periods of snow melt runoff and after <br />intense precipitation events. Detailed water quality analyses <br />for Middle Creek are compiled in Tables 27, 28, and 29 of the <br />permit application. <br />-23- <br />