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1997 0.095 c!s <br />1996 0.065 cfa • <br />Aevier of this site's TDS plot indicates no distinct trend. <br />Surface Water Site SW-S2W-FG4 (WSSP3). This eiG is situated on gage Creak dornetream of <br />the impacts from the Seneca II-w Mina (and also SCC' a Yonst Mlna) . Monitoring of this <br />Bite commenced in September 1990. Revier of the hydrograph indicates the highest peak <br />flow on record. This vita displays a decreasing TDS trend. The 9anaea II-W predicts and <br />irrigation aeaeon average TDS wlue o! 465 mq/1 for this site, chile a wlue of 495 mq/1 <br />ras observed. <br />Springs. Spring data may be found afGr surEau rater data in Appandiz E. Data provided <br />aza a rater quality report for the yaaz, tuetoric floc maasuramenis, a 7gwES9 plot of <br />field conductivities (corrected to 25° C ainca 10/1/89), and a historic listing of percent <br />milliaquiwlante of major ions and TDS. In Appendiz H, all springs haw a WSPG praEiz <br />(a.q., Spring 5-45 wSPG45). <br />Spring S-1 ie located in an ephemeral stream channel that is an u~uL ~d tributary to Saga • <br />Creak. Further Qometream in this drainsge is the 009 Pond that ras constructed in <br />October 1991. The SC plot indicates an increasing trend. <br />Spring 5-23 ie located at the headratare of the 006 Guleh, in an ephemeral stream channel. <br />This spring is upstream of proposed mining and should not be affected by mining. The EC <br />plot indicated an increasing trend until 1993, at rhich time it leveled off. <br />spring 9-41 is located dornstream o! Spring 5-23 in the 006 gilch stream channel. It ie <br />situated just dornetream of the silted-in Temple Pond •2. It receives rater from numarova <br />aaaps issuing from this mazehy, silted-in pow. Tha EC plot reveals a slightly decreasing <br />trend. <br />Spring S-5, located do~metraam of Spring 5-41 in a aide drar to the 006 Guleh, is in an <br />ephemeral stream channel. Flocs haw bean observed only [rice et this aita; Juno 1983 and <br />May 1997. <br />C <br />)~ <br />