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• No unusual observations are noted with respect to Foidel Creek alluvium groundwater levels. The historical <br />increasing conductivity trend in we11001-S-5 (Figure 32) stabilized in 2004, and appears to be increasing again <br />through the end of 2007. <br />No unusual observations are noted with respect to Fish Creek alluvium groundwater levels. The general water <br />level decline noted in well 006-AY-1 (Figure 34) since 1995, appears to continue in 2007. Overall, fluctuations <br />at this well are insignificant. No other notable water level observations are apparent based upon review of the <br />2007 data. Field conductivity readings at this well appear stable over the last few years. Two new alluvial wells <br />(AVF-13 and AVF-14) were installed in August 2001, and one (AVF-15) in June 2002. The only unusual <br />observation made to date were elevated iron concentrations in 2003 and 2004, some of which may be related to <br />subsidence ponding. These levels appear to have returned to those seen with normal seasonal fuctuations. The <br />data base for these sites will require expanding before a complete assessment can be made. <br />Surface Water: Recorded surface water flows for Foidel Creek, Fish Creek, and Trout Creek were generally <br />low in comparison to TCC's historic record. A stream gage study was initiated by TCC with the aid of a <br />consultant in the summer and fall of 2007. This study will continue in the spring, summer and fall of 2008. A <br />discussion of this study, including results for re-evaluating stream rating curves will be included in the 2008 <br />AHR. <br />Conductivity concentrations at site 301, 69, and 1005 on Trout Creek appeared elevated during the spring runoff <br />• season in April. This may be the result of upgradient spring runoff flushing through the old P & M mine area. <br />No other notable water quality impacts are evident at any surface water sites monitored during 2007. <br />Spoil SprinQS: Recorded 2007 spoil spring discharges remain negligible and, therefore, did not constitute a <br />significant portion of discharge from the TCC mine area with the potential to impact off-site areas. Discharges <br />from sedimentation ponds predominately occurred in conformance with applicable CDPS permit limitations and <br />therefore did not constitute significant impacts to receiving waters. Mine water discharge site 109 did not <br />discharge to Foidel in 2007. Site 115 did not discharge to Fish Creek in 2007. TCC redirected mine water from <br />the site 115 source in 2005 to underground locations for dust control. <br />Mine Discharge: No significant hydrology impacts, attributable to CDPS discharge activities at the Foidel <br />Creek Mine, were noted during 2007. <br />Mine Inflow: No unusual occurrences of inflow were noted as a result of the Annual Mine Inflow study. <br />Inflows are within the projected flows presented in the permit. Water quality has not changed significantly and <br />appears to Horror the quality of the adjacent spoil water. It appears that the elevated EC and iron readings are <br />associated with the water that has pooled in the mine sump, which is in contact with the overlying Marine Shale. <br />This contact has provided the opportunity for additional salts and iron to be leached from this unit. The pumping <br />of the sump should see a decrease in the elevation of the pool over time, with an anticipated decrease in the EC <br />and concentration of iron in the effluent. <br />16 <br />