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Homestake Mining Company May 10,2019 <br /> Regular(112d)Operation Reclamation Permit Application Package <br /> Two areas of slope failure were reported at the IRD. The 10,300 ft slip" measured approximately <br /> 200 ft wide and 150 ft long, and vertical displacement was"a few feet". Slope movement occurred <br /> in a saturated zone caused by groundwater seepage. The "10,200 ft slip" is thought to have been <br /> caused by elevated pore water pressure. No dimensions are reported, but the mapped extent <br /> (Figure 3-15) is smaller than that of the 10,300 ft slip. <br /> These TCRD and IRD slopes were remediated and no additional slope movements were noted. <br /> Three inclinometers were installed in 2017 to monitor the impacts of the phosphate injection <br /> program on the overall slope movement, as discussed in Section 3.4.2.2. <br /> 3.4.2. Slope Movement Monitoring Program <br /> Slope stability has been monitored since the open pit mine development began in 1979. In early <br /> 1983 the slope monitoring system included survey stations, slope monitors, tension crack <br /> monitors, established lines of sight through the forest, piezometers, and inclinometers <br /> (HMC, 1983). In 1994, the monitoring program was updated and included mapping of tension <br /> cracks and scarps, new installation of inclinometers, a semi-annual photo station documentation <br /> program, and installation of a new network of survey points. <br /> 3.4.2.1. Surficial Mapping of Landslide Features <br /> Detailed mapping of tension cracks and scarps on the east walls of the North Pit and South Pit <br /> was first completed in 1994 by Golder, as reported by AAI (1999). The original map was updated <br /> by AAI (1999) (Drawing 02) and later by SRK (2007) based on field reconnaissance. Mapping <br /> methods, areal extent of mapped area, and accuracy of mapped features are not reported in <br /> either AAI (1999) or SRK (2007). The map shows the North Pit's East Wall main scarp, relative <br /> sense of motion, and measured vertical displacements over a topographic base map. Since being <br /> created in 1994, the map has been used as a basis for monitoring and assessing the extent of <br /> surface deformation caused by slope failure at the Mine. <br /> 3.4.2.2. Inclinometers <br /> A total of six inclinometers are installed and monitored annually at the Mine (Drawing 03). In the <br /> fall of 1998 three inclinometers(198-1, 198-2, and 198-3)were installed to monitor slope movement <br /> in the North Pit (AAI, 2000b). Two inclinometers are located on the South Wall of the North Pit <br /> and one is installed above the main scarp on the East Wall of the North Pit. The installation report <br /> (AAI, 2000b) discusses and shows the location of two additional inclinometers/piezometers <br /> (I/P96-8 and I/P97-10); however, no information such as readings of these inclinometers were <br /> encountered during the review of Mine documents. <br /> Inclinometers IN-1, IN-2, and IN-3 were installed on the downstream face of the IRD in <br /> August 2017 (BGC Engineering USA Inc. (BGC), 2019a); these inclinometers were installed <br /> midway between groundwater extraction and reinjection wells to monitor rock dump stability <br /> during phosphate reagent injections. There are currently no inclinometers located west of the East <br /> Wall main scarp within the area of previous slope failure. <br /> EXHIBIT E-RULE 6.4.5(AMENDED RECLAMATION PLAN) Page 43 <br /> HOMESTAKE MINING COMPANY <br />