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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 (November 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-msl. <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 1986 to <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 GP -2 is <br />approximately 0.14 ft/ft, but is approximately one-half this value near well GP -4. <br />HI Aquifer <br />2-523 t REVISED FEB 13 '87 <br />Wells <br />GP -3, GP -7 <br />and GC -1 <br />are completed in the <br />HI aquifer in <br />the eastern <br />• <br />portion of <br />the Trapper <br />Mine. <br />Water -level elevations <br />for the three <br />wells have <br />2-523 t REVISED FEB 13 '87 <br />