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<br />1990 and 1991 has to be natural due to the location of this well in <br />relation to minine. The 1992 water levels were similar to the 1991 <br />_ i <br />value. <br />The water-level elevations for well GP2 is shown on Eieure <br />A-23. Levels have shown a .small decline during the three years <br />from mid-1986 to 1989. A small rise was observed in 1990, and in <br />1991 and 1992 the water levels have been fairly steady near the <br />?959 '7311]P_. Tnese chances in water-levels for the KLM aouifer nicer <br />- - ~ <br />well GP2 are not from mining activities since the nearest mininglis <br />.approximately two miles away. Water-level elevation data for welLls <br />GP1 and GP2 is tabulated in Table A-E (pace A-51). Water-1e'Ie1 <br />elevation data for well GP3 is t.sbulated in Table A-6 also. Figure <br />A-24 presents the plot of water-level elevation rl•ata versus time , <br />for well GP:3. Water levels in this well significantly declined in <br />late 1987. Water levels continued to der_line to late 1939. A <br />water level rise was observed during 1990 through the first half of <br />1991 in the HI squifer ne.sr this area, which may have been r_auied <br />by ungradient mining or slightly larger recharge during 1990. The <br />i <br />water level in well GP3 has shown a small inr_rease in 1992. <br />rigure A-25 presents the water-level elevation data for will <br />GP4. Data prior to 1933 shows a great deal of variance. A w.aier <br />level rise has been observed in 1990. Values for 1991 show a small <br />decline while the 1992 levels were fairly steady. <br />The caster-level elevation vers~~s time plat for well GP5 his <br />presented in rigure A-26. The levels in the ~.K aquifer near weQ1 <br />~,P5 have been gradually declining since 1985. Water levels • <br />Z-10 <br />