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2006-04-19_REPORT - M1977004
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2006-04-19_REPORT - M1977004
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Last modified
8/23/2019 8:39:31 AM
Creation date
11/27/2007 3:20:36 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1977004
IBM Index Class Name
Report
Doc Date
4/19/2006
Doc Name
Annual Fee/Report/Map
From
Homestake Mining Company
To
DMG
Permit Index Doc Type
Annual Fee / Report
Media Type
D
Archive
No
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Pitch Reclamation Project April 1a, 20U6 <br />2005 Annual RectamaUon Report Pago 8 <br />• 4.3 Pinnacle Mine Workings Monitoring <br />A concrete plug was constructed in the Pinnacle Add in September 1995. Authorization for the <br />placement of the Pinnacle Adil plug was requested by Homestake in April 1995, through Technical <br />Revision #4 (TR4) -Pinnacle Adif Closure, Pitch Project, Technical Revision for Pemtif #77~4NR <br />(Golder Associates, Inc, ). Conditional approval of the Technical Revision request was granted by <br />the Colorado -Division of Minerals and Geology in a teller dated May 26, 1995. <br />The intention of the plug was to partially seal the Pinnacle Adit and allow the area around the mine <br />workings to resalurate. The resaturation of the workings was predicted to re-establish a <br />geochemically reducing environment and lower the solubility of uranium and radium within the <br />underground workings of the Pinnacle Mine. DMG's approval of TR4 required Homestake to <br />monitor the effects of resaturation in the Pinnacle workings For five years or until hydrologic <br />conditions stabilized. Components in the Monitoring Plan outlined In TR4 (Section 4.0). included <br />continuation of discharge water quality monitoring al the POC (SW•33), monitoring of groundwater <br />resaturation levels, annual spring and seep surveys in areas down-gradient from Pinnacle workings, <br />and monitoring For changes in water quality that could be attributable to resaturation. The stated <br />purpose of the monitoring program was to verify the intended effectiveness of the adit plug. <br />Homestake has continued to monitor the following facets of resaturation through 2005: <br />• Survey of springs and seeps, <br />• Groundwater levels in piezometers installed in the area of the Pinnacle workings. <br />• Water quality and flow from the Pinnacle Adit at sampling point PP•01, and <br />• Monitor discharges from the property at the Point-of-Compliance SW-33. <br />In 2006, HMC wdl continue to monitor the resaturation of the south wall of the North Pit as done in <br />2005. <br />4.3.1 Spring and Seep Monitoring <br />Spring and seep surveys were conducted to monitor changes in shallow groundwater conditions due <br />to construction of the Pinnacle Adit plug. These surveys have been conducted annually since July <br />1995 and were repeated in 2005. In general, flow from some springs and seeps increased for a <br />beef period after the adit plug installation and have declined to a steady state since the spring of <br />1997. Small variances. noted since 1997, are believed to be attributable to conditions including <br />precipitation, depth of snow pack, timing of snowmelt, and the potential for infiltration with respect to <br />frozen ground. All "active" spring and seep locations are presented in Figure 3. Locations of <br />springs and seeps currently designated as "inactive" (not observed over the past five years) have <br />been removed from Figure 3. Locations of inactive springs and seeps can be found on maps issued <br />with past reports. An eleven-year cumulative summary of the all spring and seep surveys including <br />flow measurement results is provided as Table 2. <br />4.3.2 Groundwater Levels <br />Seven piezometers were installed in the area of the Pinnacle Mine to monitor the piezometic <br />surface within the workings area behind the adit plug. The piezometers are identi5ed as P4 through <br />f' 10 Piezometer P7 was installed as a replacement for P6, which was lost during plug <br />yroulinglconstruction. The locations of these piezometers are provided in Figure 3. All seven <br />i;~r..~ometers fluctuate seasonally with the highest levels in late May or early June. The water levels <br />are sympathetic with snowmelt and large precipitation events and decrease to stable levels after <br />
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