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=J <br />are shown on Map M54. <br />Well GP-1 is a flowing well and the pressure measurements which are shown as <br />water-level elevation in Figure 2.7-29a exhibit some erratic behavior. The method <br />of pressure measurements is not as accurate as conventional water-level <br />measurements. Water levels in the QR aquifer at well GP-1 have generally increased <br />over the last year. <br />Figure 2.7-29b presents water-level elevation versus time for well GP-5. <br />Water levels have shown some change in well GP-5 with an overall pattern of a <br />gradual decline. <br />Water levels in well GP-6 initially declined to early <br />• increasing water levels (see Figure 2.7-29c). Water levels <br />shown approximately four feet of change in the last year. <br />point is significantly higher than the following data. <br />attributed to a large amount of fluids from the drilling of <br />the immediate vicinity. <br />986 and since has shown <br />in the QR aquifer have <br />The October 1985 data <br />This can probably be <br />the well still left in <br />Map M54 shows a fairly uniform gradient in the QR aquifer in the eastern half <br />of the Trapper permit. The gradient in this area averages 0.12 ft/ft and is <br />governed by the dip of the heads. <br />KLM Aquifer <br /> The KLM aquifer in the pre-mining area is penetrated by three wells, GP-2, <br /> <br />•. GP-4 and GP-8. Figures 2.7-29d, 2.7-29e and 2.7-29f present hydrographs for wells <br />2-5235 REVISED FEB 13'87