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Homestake 2010 Geotechnical Observations <br />Pit=, Reclamation P-je t Indian Creek and Tie Camp Creek Waste Rock Dumps <br />In 2010, water levels in this piezometer were once again sporadic and required additional <br />high pressure flushing to push through the silt built up in the casing. The water level <br />readings in June, August and November are shown on Table 1, but not included in the <br />yearly summaries at the bottom of the table. Excluding these false reading, the average <br />depth to water was 188.8 feet bgs, down from 184.78 feet bgs in 2009. The maximum <br />differential in 2010 was 0.3 feet, down from 8.2 feet in 2009 and 15.5 feet in 2008. However, <br />this piezometer may have reached a point where it no longer can provide accurate <br />information of the phreatic surface in this portion of the rock dump. <br />In 2011, we will once again attempt to clear the silt by flushing the casing with high pressure <br />water as soon as field conditions warrant. In the event that flushing does not restore the <br />functionality of the piezometer, we will evaluate the purpose and need of this piezometer <br />and decide if replacement is critical to long-term monitoring of the Indian Creek Waste Rock <br />Dump. <br />2. Tie Camp Waste Rock Dump <br />__J a) "10400 -10100" Level <br />Site Description: The Tie Camp Waste Rock Dump was regraded in 1994 following <br />procedures approved in the February 1994 Technical Revision. During 1995, minor, <br />localized areas of slope instability were noted, corrected, and reported in the 1995 Annual <br />Geotechnical Report. <br />2010 Observations: Piezometer TC10375 monitors the Tie Camp Creek Waste Rock Dump. <br />In 2010, water levels averaged 168.35 feet logs, with a maximum observed seasonal <br />fluctuation of 1.83 feet between May and June. The maximum fluctuation was down from <br />the 2008 maximum fluctuation of 12.3 feet and 6.1 feet in 2009. This is deemed as an <br />acceptable seasonal variation. Field observations indicate that the repairs performed in <br />1995 were successful and no new areas of surficial instability were observed from 1996 <br />through 2010. In 2011, we will continue to monitor the surface conditions of the Tie Camp <br />dump after the spring snow melt. <br />3. Piezometers - 2010 General Comments <br />The 2010 water level measurements showed a maximum differential following snow melt in <br />line with historical readings. Following the dry conditions of 2001 through 2003, the <br />seasonal variations have increased in recent years as heavier snow packs have occurred. <br />However, there continues to be problems related to silt and corrosion in some of the <br />piezometers. Homestake will continue to evaluate the conditions of the piezometers and <br />remedy the buildup of silt in the casings, as possible. We will continue to monitor and <br />evaluate the cause and effect of seasonal spikes in the piezometric water levels, and also <br />observe any changes in surface features of the rock dumps. There continues to be no <br />indication of concern related to instability in either the Indian Creek or Tie Camp Creek <br />waste rock dumps. <br />Homestake Pitch Reclamation Project Page 3 <br />2010 Annual Geotechnical Report December 20, 2010 <br />M-1977-004HR 2010AnnualGeotechnicalReportText_Final.doc