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Fish Creek sandstone wells Water levels in the two Fish Creek sandstone wells, 9l M001 and 91 Nt004, in the SWMD continue to indicate slight drawdown due to undermining and subsidence. However, 91 bt001 has recovered to levels very close to pre-subsidence levels. The Ashley domestic well in the EMD is also completed in this formation and shows no impact due to mining at this time. Conductivity and pH measurements of these wells indicate no change in water quality that is consistent with predictions. Alluvial Wells Water levels continue to show seasonal variation with no apparent changes due to mining. Salinity increases aze evident in alluvial wells on Foidel and Fish Creek but this increase is likely not due to bedrock discharge from natural discharge points. Underground mine water discharge to these two creeks are likely the cause of the observed increases in salinity over baseline levels. The PHC does not address alluvial well salinity changes caused by surface water changes and alluvium recharge. Well 006-AY-1 upstream of mining on Fish Creek shows increasing conductivity as does welt 006-AZ-3 neaz the Fish Creek Borehole and well 008-AU-3 near the Fish Creek Tipple. Lazger changes in conductivity are evident the closer the wells are located to the Fish Creek Borehole, the mine portal and facility area, and spoil springs at the Fish Creek Tipple. Well 008-AT-I, downstream of all mining impacts on Trout Creek indicates variation in TDS from 700-900 mg/l since the inception of monitoring. The Jones domestic alluvial well on Trout Creek indicates TDS of approximately 500 mg/I. Middle Creek alluvium remains unaffected by underground mining activities. The PHC predicts quantity impacts to the Wadge overburden and to a lesser degree the Twentymile sandstone aquifer. No signiticant water quality changes are predicted. Generally, data confirms these predictions at the present time. Diminution of Bedrock Discharge to Alluvium and Surface Streams (also Effects on Alluvial and Surface Water Oualitv As a Result of Bedrock Discharge) Both of these impacts aze predicted to be small and analysis of the data does not indicate that either can be detected at this time. Streamflow shows normal seasonal vaziation. Subsidence Impacts on Ground Water Ouantitv Review of the ground water data reveals that subsidence does appear to impact ground water levels by increasing permeability due to bed separation and fracturing induced by subsidence, especially in the Twentymile sandstone and the Wadge Overburden. Impacts aze discussed for each ground water unit above under Dewaterine and Potentiometric Drawdown in Bedrock Units. Subsidence Impacts on Alluvial Ground Water in the Foidel and Middle Creek Alluvial Valleys The PHC predicts no impacts to alluvial water quality in the Foidel and Middle Creek alluvial valleys due to subsidence. Analysis of the data indicates water quality changes in alluvial