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<br />I. Surface Water <br />A. Trout Creek <br />All the proposed mining will take place in Trout Creek drainage. Trout Creek <br />is a perennial stream. From the baseline study it was determined that peak <br />flows occur in early to mid June and flows are well in excess of 100 cfs from <br />May through July. Low flows of approximately 10 cfs occur in late fall, just <br />before winter freeze-up, and in early spring. Three sites were utilized for <br />the baseline flow study and two of these sites are part of the ongoing <br />monitoring program. TR-a is at the upstream edge of the mine and TR-b is <br />downstream of the permit boundary. <br />The quantity data submitted in the 1982 and 1983 hydrologic monitoring reports <br />is similar to that of the baseline with higher flows from above normal <br />precipitation. The gauge rating curves were recalibrated in 1983. The <br />recalibration showed that while low flow data was fairly accurate, high flow <br />data could be questionable. This is due in part to the changes the channel is <br />going through at the location of TR-b. These changes have caused interference <br />in the communication between the stilling basin and stream. It may be <br />necessary to change the location of TR-b if it does not appear that the <br />channel is stabilizing. <br />There were 4 water quality sampling points established along Trout Creek for <br />the baseline study. They were placed upstream of mining (TRA), adjacent to <br />old mine spoils (TRB), adjacent to the Moffat Area (TRC) and downstream of <br />mining (TRD). In the baseline study the 2 sites adjacent to the permit area <br />had the poorest water quality, with TRC the worst while the quality improved <br />downstream from mining at the site TRD due to dilution. The poor water <br />quality at sites TRB and TRC is due to drainage from unreclaimed mine spoils. <br />Numerous springs occur at the toe of the spoils slope and drain directly into <br />Trout Creek. <br />The water upstream in Trout Creek is of a calcium bicarbonate type while <br />immediately downstream from the mine the chemical character is of a calcium <br />sulfate type. The water quality criteria established by EPA in 1972 were used <br />for the baseline study. The most often exceeded criteria at all the stations <br />were iron, zinc, and manganese, however these values were exceeded less than <br />40% of the time. Nickel and silver also periodically exceeded the criteria. <br />Several values (nitrate, sulfate, sodium, calcium and magnesium) increased <br />substantially from the upstream site to the downstream site, but are still <br />within the recommended criteria. <br />The worst TDS levels during the baseline study occurred at the stations <br />adjacent to the mine area with some improvement at the downstream station. <br />Maximum value at TRA was 535 mg/1, TRB was 768 mg/1, TRC was 629 mg/1 and TRD <br />was 565 mg/1. The numerous springs that drain directly into the creek in the <br />vicinity of sites TRB and TRC have been sampled at TDS levels as high as <br />approximately 3,000 mg/l. From this data it is apparent that Trout Creek has <br />a tremendous dilution effect on spoils water quality. <br />