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• <br />l J <br />• <br />3.1.2 Cuts <br />Cuts have been made during development of the benches <br />at the site in both colluvial soils and in bedrock. The <br />stability of all cuts was evaluated during our geotechnical <br />review phase of this investigation. <br />The stability of slopes cut into bedrock was evaluated <br />based on the character of the exposed rock, the orientation <br />of the cut slopes, and the orientations of geologic dis- <br />continuities within the rock mass. They are generally consi- <br />dered to be stable overall, although some local problems of <br />rockfall may occur. <br />The diversion channel cut, which lies at the back of <br />the Fan level fill, has been cut into both colluvial soils <br />and bedrock at ankles between about 45 and 50 degrees. While <br />the cut generally appears stable where it has been made into <br />bedrock, several slides have developed where the cut is in <br />soil. These indicate that the safety factor of the cut in <br />soils is close to unity. <br />While other soil cuts have been excavated at similar <br />slopes to the diversion channel cut, they are generally of <br />lesser heights than the diversion channel cut. No signs of <br />instability were observed in any of these cuts, and it was <br />noted that all these slopes had been successfully revegetated. <br />Their stability is attributed to tfTe favorable physical pro- <br />perties of the colluvial soils and the revegetation of the <br />slopes. These slopes .are considered to be steep for unce- <br />mented sediments. However, it is considered tha[ no addi- <br />tional stabilizing procedures should be undertaken in view of <br />their pas[ and current performance, even though there is some <br />risk that local failures may occur in tlTese cuts. <br />- 14 - <br />GF6HYD110 CONSULTING.INC. <br />