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Three wells, 25-5, 26.5, and 27-5 are situated in lower spoils adjacent to the Wedge Impoundment which receives spoils water discharge. AlL three of these wells were • outfitted with continuous recorders operated by the U S Geological Survey (USGS) until the end of 1983. WeLI 25-5, the highest upgradient of these three wells on the spoils slope, indicated an absence of recharge in 1987, 1988, 1990, and 1991, but exhibited recharge in all other years since 1983. Yell 27-5, lowest of the three, shows that its water levels ere most likely dependent upon the water level in the Wedge Impoundment located 50 feet away. These findings are also supported by the USGS personnel operating the recorders prior to 1984. Yell 26-5, located between Wells 25-5 and 27-5, normally exhibits very Little seasonal variability and water levels higher than either 25-5 or 27-5. This is not a normal ground water level gradient; therefore, its water Levels should be reviewed with caution. Perhaps, as with Yell 22-5, water is being trapped in the borehole. Seven spoil wells were completed in the fall of 1987. Three (Yell 59-5, 60-5, and 61-5) were completed upgradient of the Spoils Spring #3 area, while four (Yells 62-5 to 65-5) ware completed in the Spoits Spring #1 area. The purpose of placing several wells at each site was to accurately define the potent iometric surface of the spoils aquifer at each location. Water Levels et Yells 59S through 61-5 have experienced an increase between July and September of 1994. This is due to regrading of topsoil in this area that • occurred during this time frame. This regrading affected Spoil Spring #3 immediately downgradient of these three spoil wells and thereby affected the water levels in those wells. Water levels at all other spoil wells exhibit normal seasonal variations. Yell 65.5 has been dry for the entire period of record. It is located in an area where the spoils are unsaturated. Ground Water Level Summary. ALl alluvial wells ere showing distinct seasonal water level fluctuations in response to periods of precipitation recharge or the lack of precipitation. Overburden end coal well water levels are fluctuating in response to the precipitation recharge, induced ground water flow to the mine pits, and in some cases, changes in reservoir water levels. Spoil well water levels still indicate that only the furthest downslope highwall portions of the spoil exhibit significant amounts of saturation. Levels in a spoil well near the Wedge Impoundment is largely controlled by water level fluctuations in the impoundment. Water levels in several wells this year were lower than they have been before as a result of low snowpack recharge and dewatering by the Wolf Creek coal mine pit. .~ 4