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• Wells BOl through B06 and Well BOS are monitored semiannually for water levels <br />to assess slope stability in and around the East Mine facilities. <br />Patterns typically associated with these wells in the past were again evident <br />during the 1995 monitoring. Wells BO1, B03, BOS, B06, and B08 rQnw;ncrt dry <br />throughout the year. Wells B02 and B04 shaved imderate water level fluctuations <br />within the established normal ranges previously documented. Conductivity values <br />at BOT L'P,IilainPri within the range of values previously established. Other <br />monitored parameters fluctuated slightly within established ranges. The 1993 <br />report indicated that sulfate and total dissolved solids appeared to be slightly <br />elevated at B07. In 1995 sulfate was 344 mq/1 oonq~ared to the 1993 average of <br />380 mg/1. The 1995 TDS value was 1050 mg/1 cot~ared to the 1993 average of <br />1,188 mg/1. The 1992 AHR presented min;anvn and maxinnim Values for the period <br />of record from 4/83 to 10/92. The range for sulfate was 64 to 731. The range <br />for TDS was 244 to 1900. The 1993 and 1995 values for sulfate and TDS fall <br />within the minim,m and maxim,m Values documented in the 1992 AHI2. <br />• OVW~t G7i0[R~IDF+B-~2 MCNlTaRiNG WELLS <br />Well (7VFEa (see Map No. 4-1) was monitored monthly for water level only to assess <br />stability of the West Mine fill cronstructed over East Roatcap Creek. Well OVWM <br />showed typical water level fluctuations during 1995 within the normal range <br />established for this site (see Tab 5 Figure 5). <br />D1Q3i14i FaRK W,IZ]VILM GRgIIIid4~TIIt MCSIITORING WELLS <br />Three wells, I~E4-1, 1~E4-2, and I~E~T-3 (see Map No. 8-3) are oa~~leted in the North <br />Fork (~uuLison alluvium. During 1995 the wells were monitored nunthly for water <br />levels and shaved typical seasonal fluctuations within previously established <br />ranges (see Tab 5 Figures 6, 7 S 8). MW-1 and MW-3 were monitored quarterly for <br />quality during 1995 to monitor potential groundwater effects stemming fran the <br />coal stockpile and loadout facilities located in the North Fork Valley. Well <br />MW-1 is east of the loadout in an area that should be outside or above the area <br />of influence of the coal stockpile and loadout facilities. Well MW-3 i.s <br />southwest of the coal stockpile azea in a location that should see the full <br />impact of any potential groundwater degradation. The TDS level in the wells <br />gives a good indication whether the ground water in the area has been degraded. <br />• Zn 1993 the TDS in wells MW-1 and M~v-3 was 388 and 380 mg/1 respectively. These <br />values are considered baseline values. Well AiS+1-1 had a TDS level of 650 and 760 <br />3 <br />