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r <br />L_ <br />Surface Water Site SW-52W-FG6 (WSSF3). Thie site is situated oa Sage Creek downstream of <br />cbe impacts from the Seneca II-N Miae land also SCC's Yoast Miael. Monitoring of this <br />site commenced is September, 1990. Review of the hydrograph indicates Cbe highest Desk <br />flor on record. This Bite di aplaye n decreasing TDS trend. <br />Springs. Spriaq data may ba found after surface rater data is Apyeadix E. Dnta provided <br />are a water quality report for the year, historic flow measurements, a LOWESS plot of <br />field coaductivi ties (corrected to 25° C since 10/1/89), and a historic listing of percent <br />milliaquival en to of major ions and TDS. Ia Appendax 8, all springs have a WSPG pzef ix ', <br />(a.q., Spriaq 5-46 = WSPG66). <br />Spriaq 9-45 [a.k.a., the Olson Spring) is not a flowing apriag, but a [brae-foot diameter <br />wall placed is the alluvium of Dry Creek. Since a well xas drilled oa the Oleos ranch is <br />September, 1980, this •eyxiag• bas not been put to use, although it is water-righted for <br />stock use. Tba electrical conductivity (EC) plot indicates s decreasing trend. <br />Spring 5-1 ie located is as epaemaral stream chaanei that is an unnamed tributary to Sage <br />Creak. Further dornstream is this drainage is the 009 Poad that was constructed is <br />October, 1991. The HC plot iadlcatea an increasing tread. <br />Spria9 5-23 is located at the head waters of the 006 Gulch, in an ephemeral stream <br />channel. Thie spring is upstream of proposed mining and should not be affected by mining. <br />The 8C plot indicated an increasing trend until 1993, at which time it leveled off. <br />spring 5-41 is located downstream of Spring 5-23 in tae 006 Cu1ch stream chancel. It ie <br />ai tuated just downstream of the silted-ia Templ¢ Pond p2. It receives water from numerous <br />seeps issuing from this marshy, silted-in pond. The EC plot reveals a level trend. <br />Spring S-6, located downstream of Spring 5-61 in a side draw to tae 006 Gulca, is in an <br />ephemeral stream channel. The last flow monitored here vas in June, 1983, and is tae only <br />sample on record. <br />Spring 5-46 is a developed spring first moai toting during the 1979 spring survey. This <br />spring i9 not part of tae required monitoring program, however, due to its strategic • <br />]0 <br />