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• Two additional bore holes were placed at approximately stations 83+00 and 85+00 by <br />MCC personnel where Sylvester Gulch will be crossed which showed the clay soils <br />extended to at least 30 feet below the surface. <br />A seismic refraction study was performed by UMS in April 2003 under the direction of <br />ESC to obtain depth to bedrock information especially in the areas where soil borings <br />could not be performed due to weather conditions. Typically the seismic lines were <br />extended 100 feet either side of the bottom of the drainage. The locations of the seismic <br />lines are shown in Figures 1 through 6. The complete report of the seismic work can be <br />found in Appendix D of this report. <br />A field geologic mapping of the landslides along the proposed route was performed by R <br />Squared Incorporated in 2004 under the direction of SEI to accurately delineate all <br />landslides that could directly impact the stability of the proposed road. These landslides <br />are shown in Figures 1 through 6. <br />A borrow source investigation to locate suitable borrow material for the construction of <br />the roadway was performed in December 2004. This work was performed using a small <br />backhoe supplied by MCC excavating four holes to a depth of approximately seven feet <br />at the locations shown on Detail Sheet 14 of 15 found in Appendix A of this report. Soil <br />samples were placed in five gallon buckets and sealed and shipped to GEI for laboratory <br />testing. <br />• 5.2 Laboratory Testing <br />Laboratory testing was performed by GEI in 2003 and 2005 on selected samples obtained <br />during the drilling program. Tests performed included: <br />• Moisture Content <br />• Atteberg Limits <br />• Consolidation <br />• Consolidated Undrained Shear Tests with Measured Pore Pressures <br />• R Value <br />• Standard Proctor <br />• Gradation <br />The results of these tests can be found in Appendix E of this report. <br />5.3 Slope Stability Analysis <br />Slope stability analyses were performed on 11 proposed roadway cross sections and at <br />the proposed borrow site. The geometry of the cross sections were based both on the <br />geologic profiles obtained during the drilling program and seismic study and the <br />proposed roadway section. The native soil strength parameters were based upon the <br />laboratory testing program. The strength of the borrow material was based on tests <br />• performed on the borrow material recompacted to 95 percent of standard proctor before <br />they were placed in the shear machine. The strength of the sandstone bedrock was based <br />