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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 1986 and since has shown <br />• increasing water levels (see Figure 2.7-29c). Water levels in the QR aquifer have <br />shown approximately four feet of change in the last year. The October 1985 data <br />point is significantly higher than the following data. This can probably be <br />attributed to a large amount of fluids from the drilling of the well still left in <br />the immediate vicinity. <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 />2-5235 REVISED FEB 13'87 <br />The <br />KLM <br />aquifer in <br />the pre -mining <br />area <br />is penetrated <br />by three wells, <br />GP -2, <br />•. <br />GP -4 and <br />GP -8. <br />Figures <br />2.7-29d, 2.7-29e <br />and <br />2.7-29f present <br />hydrographs for <br />wells <br />2-5235 REVISED FEB 13'87 <br />