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Reconnaissance <br />R Squared's geotechnical reconnaissance consisting of reviewing documents, performing a walk <br />over of the road, and logging three test pits in the road. Documents reviewed include the May <br />26 report, as built drawings, and a CDRMS memorandum from Wally Erickson to Allen <br />Sorenson, dated May 17, 2010, entitled "Idaho Mine Access Road, Wildcat Mining Corporation, <br />File No. M- 2010 - 003 ". <br />The test pits were excavated by a backhoe operated by Mr. Mossa at R direction at the <br />approximate locations shown in Figure 1. Test Pit #1 was located where the unsupported <br />outboard slope was highest and steepest; Test Pit #2 is in the middle of the outboard retaining <br />wall, approximately midway between two leaning vertical supporting logs; and Test Pit #3 is in <br />the cut -fill transition area uphill of the drainage crossing. Our engineer logged the materials <br />exposed in the test pits and collected bulk samples of these materials on which physical <br />properties tests were performed. Conditions encountered in our test pits are summarized in <br />Table 1. Bulk samples obtained from the test pits were placed in plastic 5- gallon buckets, <br />covered with plastic lids, and transported to Terracon Laboratory in Farmington, New Mexico. <br />Attempts were made to obtain undisturbed samples; however, the loose condition of the fill <br />and/or the presence of cobble -sized materials hampered these efforts. Laboratory tests <br />performed on the samples include, grain size distribution, Atterberg limits, and moisture content. <br />Materials exposed in the test pits are described in Table 1. Laboratory test results are <br />summarized in Table 2; test results received from the laboratory are provided in Appendix A. <br />Observations <br />Road <br />The road is approximately 500 feet long and, for purposes of discussion, has been divided it into <br />three sections: (1) the upper portion extending through a through -cut, (2) a cut -fill condition in <br />the middle, and (3) a fill embankment crossing a drainage and the bottom, with the fill thickness <br />grading to essentially nil as the roadway transitions to level ground. The river generally parallels <br />the cut -fill portion of the road; the toe of the hillside slope, outboard of the cut -fill road section, <br />is at or near the creek shoreline. The through cut section extends through colluvium/glacial till. <br />As the road transitions to the cut -fill portion, hard rock is exposed in steep cutslopes. In many <br />areas roadway slopes are greater than 15 percent. A shallow landslide was observed above the <br />cutslope near the transition from through -cut to cut -fill road sections, the colluvium/glacial till <br />contact with bedrock exposed in the cutslope. Cracks up to 1 inch wide were observed on the <br />road surface exiting from the uphill side of the upstream drainage retaining wall diagonally <br />toward the outboard slope then paralleling it for at least 30 feet. No seepage conditions were <br />observed in either cut or fill slopes despite the fact that spring snowmelt and runoff was near its <br />peak during the reconnaissance. The hillside slope outboard of the cut -fill road section is <br />covered with loose soil, rock, and debris. A damaged silt fence parallels the river bank at the <br />bottom of the hillside slope. Retaining walls parallel the road along a portion of the hillside <br />May 30, 2010 <br />