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PR-12 Exhibit 71 30 <br />4.4.5.5 Spring J-7 <br />Spring J-7 is located in Poison Gulch which is tributary to Dry Fork (Map 1). It is within the SOD area that will <br />be developed between years 2009 and 2013. The source of this spring appears to issue from alluvium. Baseline <br />monitoring of Spring J-7 began in the spring of 2006 and included measuring flow, collecting field water quality <br />data, and collecting samples for laboratory water quality analyses from May through October 2006 (CDMG, <br />2005b). Routine monitoring at this location began in 2007. <br />4.4.5.6 Deep Creek Spring #2 <br />Deep Creek Spring #2 is located in Deep Creek which is tributary to North Fork of the Gunnison River (Map 1). <br />It is in the DFL areas that will be developed between years 2009 and 2013. The source of this spring appears to <br />issue from alluvium. Baseline monitoring at Deep Creek Spring #2 began in the spring of 2007 and included <br />measuring flow, collecting field water quality data, and collecting samples for laboratory water quality analyses <br />from April through September 2007 (CBMG, 2005b). Routine monitoring will begin in 2008. <br />4.4.5.7 Deep Creek Trail Spring <br />Deep Creek Trail Spring is located in Deep Creek which is tributary to North Fork of the Gunnison River (Map <br />1). It is in the SOD area that will be developed between years 2009 and 2013. The source of this spring appears <br />to issue from alluvium. Baseline monitoring at Deep Creek Trail Spring began in the spring of 2007 and included <br />measuring flow, collecting field water quality data, and collecting samples for laboratory water quality analyses <br />from April through September 2007 (CBMG, 2005b). Routine monitoring will begin in 2008. <br />4.4.5.8 96-2-2 Area Spring <br />The 96-2-2 Area Spring is located in Deep Creek which is tributary to North Fork of the Gunnison River (Map 1). <br />It is in the DFL area that will be developed between years 2009 and 2013. The source of this spring appears to <br />issue from colluvium. Baseline monitoring at 96-2-2 Spring began in the spring of 2007 and included measuring <br />flow, collecting field water quality data, and collecting samples for laboratory water quality analyses from April <br />through September 2007 (CBMG, 2005b). Routine monitoring will begin in 2008. <br />4.5 Ground Water Monitoring <br />0 <br />Currently, there are 27 monitored wells in the WETM ground water monitoring plan, including the SOM-23-1-1-1, <br />SOM-23-H 2, SOM-23-H 3, and SOM-23-1-1-4 wells that MCC re-introduced into the monitoring program in <br />2005. Well SOM-23-H-1 was monitored in 2005 and part of 2006, however, although there was audible water <br />flowing in well, the well casing was damaged at depth of 135 feet. 145 feet, and 190 feet and it was completely <br />obstructed at 243 feet (original depth was 604 feet). As a result, monitoring data collected from this Nell is <br />suspect and the well will not be monitored in the future. <br />September 2007 <br />HrdroGeo, Inc.