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• <br /> <br />The water-level elevation versus time plot for well GP5 is <br />presented in Figure A-21. The levels in the QR aquifer near well GP5 <br />have been fairly steady since June 1986. Well GP6 is completed in the <br />QR aquifer and is located approximately 4700 feet south of well GPS. <br />Water-level elevation versus time is presented in Figure A-22. Water <br />levels have risen approximately six feet in the QR aquifer in this <br />area since June 1986, probably due to a slight increase in recharge to <br />the QR aquifer. Water-level data for wells GP4, GP5 and GP6 are <br />presented in Table A-6. <br />Water level data for the three GBB wells is presented in Tables <br />A-6 and A-7. Figures A-23, A-24, and A-25 present the water-level <br />• elevation plots for the three wells. Static water levels for well <br />GBBi have been above land surface through June 1987. Water levels in <br />Well GBB2 are not thought to be representative of heads in the aquifer <br />due to the poor connection between the aquifer and well bore. Water <br />levels had been fairly steady in well GBB3 during 1986 through June <br />1987 with the March 1987 value being higher. The GBB wells were <br />dropped from the monitoring schedule with State approval and replaced <br />with well 81-03A. No GBB well data is present for the second half of <br />1987, <br />Water level data for the P wells is presented in Tables A-7 and <br />A-8 of Appendix A. Water level in alluvial well P1 was fairly steady <br />in 1987 (see Figure A-26). Water levels in well P1 have stayed high <br />• since 1984 because the base flow of Pyeatt Gulch has increased and has <br />2-7 <br />