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GP-2, GP-4 and GP-8, respectively. Map M54A presents the water-level elevation <br />contours for the KLM aquifer. September 1986 water levels were used to develop the <br />map. <br />Figure 2.7-29d exhibits water levels for well GP-2 that have not shown much <br />change except for the gradual decrease in late 1985 and a gradual increase during <br />1986. Water-level elevations are presently CNovember 1986) close to 6890 feet above <br />MSL. <br />Well GP-4 is a flowing well and Figure 2.7-29e presents pressure readings in <br />the KLM aquifer converted to water-level elevations. The water-level elevations <br />show some erratic appearance. This is most likely explained by a difference in <br />• method of measurement of pressures on well GP-4. The water-level elevation is <br />presently at 6580 ft-mal. <br />Figure 2.7-29f shows a gradual rise in the water-level elevation after <br />installation of well GP-8 until early 1986. Water-level data from early 1486 [o <br />November 1986 has remained roughly at 7133 feet above MSL. <br />Map M54A shows the water-level elevation for the KLM aquifer for the Trapper <br />Mine. The hydraulic gradient of the KLM aquifer near wells GP-8 and CP-2 is <br />approximately 0.14 ft/ft, but is approximately one-half this value near well GP-4. <br />HI Aquifer <br /> Wells GP-3, GP-7 and GC-1 are completed in the HI aquifer in the eastern <br />• portion of the Trapper Mine. Water-level elevations for the three wells have <br />2-523 t RElIISED fEB 13 '87 <br />