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<br />1 <br />' not completely recovered from the previous sampling during the <br />November measurement. Water levels have been fairly steady in well <br />1 GB83 during 1986. <br />t Water level data for the P wells is presented in Table A-7 of <br />' Appendix A. Water level in alluvial well P1 was :>teady in 1986 (see <br />Figure A-24). Water levels in well P1 have stayed high since 1984 <br />' because the base flow of Pyeatt Creek has increaseol and has maintained <br />the high levels in the alluvium. Water levels in the Lewis Shale <br />(well P3, see Figure A-25), which is in contact with the Pyeatt <br />alluvium, have varied very similar to the alluvial aquifer in this <br />area. Water levels in the Second White Sandstone e~quifer near well P5 <br />' continued to show a yearly cycle of a rapid rise during the Spring and <br />then a gradual declining the remainder of the year. water levels in <br />' the Third White Sandstone well, P8 (see Figure A-27), also have shown <br />' the yearly fluctuation. <br />Water levels of Johnson Gulch alluvial well, J1, are presented in <br />Figure A-28. This plot shows steady water levels for 1986 in this <br />' alluvial aquifer, except for one measurement. The Flume alluvial <br />aquifer is monitored with alluvial wells GC3 and Coy. The water level <br />in alluvial well, Coy, (see Figure A-29) rose until May of 1986 and <br />' has gradually declined for the remainder of 1986. Figure A-8 shows a <br />steady water level for alluvial well GC3 for the last two years. <br />1 <br /> <br />' 2-6 <br />