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• upgradient of the Lux domestic well. Two new wells, GD3 and II <br />GF11, were installed during duly, 1988 in the backfill material <br />upgradient of native OR aquifer wells GD2 and GF6, respectively. <br />Table 1-1 presents basic well data for all wells monitored in <br />1988. <br />Several springs have also been monitored to further define <br />the ground-water quality. Cottonwood Spring, West Buzzard and No <br />Name Seeps have been sampled to define ground-water quality <br />discharging from the backfill aquifers in these areas. Observed <br />discharges during May, September and November, 1988 at Cottonwood <br />Spring were 2.6 gpm, 2.B gpm and 2.7 gpm, respectively. The West <br />Buzzard Seep was found to be flowing at approximately 1B gpm in <br />• May. The West Buzzard Seep is located upstream near the NPDES <br />006 site. The No Name Seep is located near well GFS at the <br />contact of the undisturbed overburden and the backfilled spoil. <br />No Name Seep was observed flowing at 3.5 gpm in May. No flows <br />were observed during the West Buzzard site visits in September <br />and November. Pond water at the West Buzzard Seep was used for <br />water quality during September and November. <br />The Colt Seep had no data for 1988 as flow had stopped due <br />to the C pit dewatering in 1988 and was subsequently mined <br />through. <br />Table 1-2 presents the mine discharge for the Trapper Mine <br />for 1988. This data shows that, on an average, approximately B0 <br />gpm was pumped from the Trapper Mine in 1988. This data is <br />. useful in interpreting water-level changes. <br />Surface-water flow and quality have been monitored at the <br />1-2 <br />