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Pitch Reclamation Project -Sediment Control Embankment November, 2002 <br />Based on the field observations made during the initial site visit, and subsequent discussions with <br />Homestake, additional piezometers were installed in the embankment to further characterize the <br />seepage through the embankment. A summary of the site observations and field work is presented in <br />the following sections. Figure 4 shows the approximate location of the wet area of concern on the <br />downstream face of the embankment and the location of the additional piezometers. <br />3.2 Field Observations -September 1, 2000 <br />The site visit of September 1, 2000, included both observation of the embankment and slope <br />conditions, and review of design and construction data contained in the project files at the site office. A <br />summary of the significant observations and findings from the site visit is presented below. The complete <br />report of the site observations and data, and resulting conclusions is included in Appendix A for <br />reference. <br />The embankment slope and crest areas were walked several times in noting the following <br />observations. (Note: Left and right directions in this report are based on facing downstream.) <br />I. The area of concern noted by the CDWR was evident by an azea of dense, tall grass (<10-ft <br />diameter area) exists on the face of the slope. It was just below and to the left of the Standpipe <br />for Piezometer No. 4 and about mid-slope near the maximum cross-section of the <br />embankment. <br />2. The soils in and immediately adjacent to the left side of the dense grass were wet and showed <br />signs of sustained seepage. In addition, an area about 15-ft wide that indicated increase <br />moisture content over the adjacent aeeas extended across the face of the embankment from just <br />right of the wet area to the left abutment. <br />Signs of at least surficial movement were apparent in the 15-ft wide strip as well as in areas <br />above and below the strip. <br />4. A small void was observed in the scarp just left of the grassy area. A small amount of <br />embankment borrow material was present on the surface azound the void. It was not obvious <br />whether this material had been piped to the surface from uncontrolled seepage or eroded from <br />the scarp trace. <br />The Homesrnke Mining Company -5- The Glasgow Engineering Croup, lnc. <br />