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Demonstration of Compliance Climax Molybdenum Company <br /> With Regulation 41 Permit M-1977-493 <br /> Robinson TSF drainage north down the Tenmile Creek basin. Prior to 2005, drainage <br /> that collected on the surface of Robinson TSF was conveyed to Robinson Lake in the <br /> Eagle River basin through the West Gravity Line. The West Gravity Line was <br /> subsequently abandoned and plugged with concrete. This project eliminated a <br /> significant source of impacted water inflow to the Eagle River basin. <br /> ■ In 2008, in accordance with information provided in TR-15, Climax conducted a sludge <br /> removal project in the east end of Robinson Lake to optimize the capacity of the facility <br /> for future production. Sludge and sediment removal was again conducted in 2010 and <br /> early 2011, and approximately one million cubic yards of material were removed. This <br /> work significantly reduced the amount of material that could potentially leach <br /> contaminants. <br /> Thus, no new or increased sources of contamination were initiated in the Eagle River Watershed <br /> subsequent to January 31, 1994. Rather, several projects have eliminated and mitigated <br /> historical sources in the area. <br /> An increasing trend of certain water quality parameters in monitoring well EVMW-1 S was <br /> observed beginning in late 2012 to early 2013. Following the procedures of the WQMP to protect <br /> downgradient water resources, the DRMS and Eagle Park Reservoir Company were notified and <br /> a program that included increased monitoring frequency, field investigation and data evaluation <br /> was conducted. The results of these efforts have been reported to DRMS and Eagle Park <br /> Reservoir Company (Tetra Tech, 2013 and Tetra Tech, 2014). As presented in the 2014 Status <br /> Report; Robinson Seep Investigation (Tetra Tech, 2014), a review of the data collected over 2013 <br /> and 2014 indicate that the previously observed, and short-lived, increasing trends observed for <br /> primary indicators have reversed, and an overall decreasing trend has been observed since the <br /> summer of 2013. These data suggest that the cause of the increasing trends observed in 2013 <br /> was likely related to the filling of Robinson Lake in 2011 to prepare for the resumption of Climax <br /> milling operations in 2012. The Robinson Lake water level had been maintained at a lower <br /> elevation typically not exceeding 10,850 feet for a ten year period from 2000— 2010. Following <br /> the completion of the sludge removal project(described above) in 2010, the reservoir was refilled <br /> between April and July 2011, from a water surface elevation of 10,830 feet to 10,875 feet, an <br /> elevation typical of water storage at Climax in the mid-to late- 1990s. When viewed in the context <br /> of conditions relative to January 31, 1994,this event is not indicative of a new or increased source <br /> of groundwater contamination. Rather, it is reflective of historical conditions in the upper Eagle <br /> River Basin at this particular facility. Most importantly, as observed in the data described in the <br /> following section, groundwater quality in this basin has remained within the historical range of <br /> constituent concentrations. <br /> 4.2 Data Evaluation <br /> Groundwater monitoring well EVMW, constructed in September 1993, below the Robinson Lake <br /> Seepage Collection System Cut-Off Wall, was replaced by a similar shallow monitoring well, <br /> EVMW-1 S, in October 2011. These monitoring locations provide a combined period of record <br /> from 1993 through the third quarter of 2016. Similar to well ARwell in the Arkansas River <br /> Watershed, monitoring at EVMW began with four consecutive quarters of sampling from <br /> September 1993 through September 1994. Monitoring was suspended following the initial year <br /> December 2016 13 <br />