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-15- <br />• The gravel road was built in 1977, and the behavior of <br />individual cuts during this period can be evaluated and used <br />for the recommendations on cut slopes and configurations in <br />these geological conditions for the design of the upgraded haul <br />road. <br />Our documentation of these cuts and observations on their <br />behavior are presented in this section. The cuts were numbered <br />for convenience's sake (see Geotechnical Maps, Plates 2 A - 2 D). <br />The cut No. 1 is located in a ridge between the Munger <br />Creek valley and the valley of its tributary. The cut is excav- <br />ated in terrace deposits. The cut reaches its maximum height <br />of 50 to SS feet; the cut slope is between 55 and 75 degrees. <br />The inspection of the cut face does not reveal any indications <br />of stability problems. In spite of the overall steep cut slope, <br />there are no significant sloughs visible at the cut face. Even <br />the amount of soil eroded from the cut face is very minor. <br />The_cut_NO__2 is located partly in soils and partly in <br />slope-forming shales and sandstones. The lower cut portion <br />that has been excavated in colluvial soils is low and at a <br />slope of about 52 degrees. There are minor sloughs visible <br />on the cut surface showing distinctly the difference between <br />the terrace deposits of the cut number 1 and the colluvial soils <br /> in this cut portion. The remaining portion of the cut is in <br />• rocks, excavated at an angle of about 63 degrees. The height <br /> of the cut reaches s ome 50 feet. The cut has been excavated <br />