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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />2.0 GEOTECHNICAL EVALUATION <br /> <br />2.1 Field Investigation <br /> <br />2.1.1 General <br /> <br />The geotechni ca1 i nvesti gati ons at Peterson Lake Dam were carri ed out to <br />supplement work performed previously in 1982 and 1985. The objective was to <br />characterize the embankment dam and its foundation, investigate sources of <br />potential construction material, and to gather soil samples for laboratory <br />testing. The field investigations consisted of surficial geologic mapping and <br />subsurface exploration by means of bore holes, test pits, and seismic <br />refraction surveys. Multi-level standpipe piezometers were installed in each <br />bore hole following completion. The work was performed during the months of <br />August and September, 1986, di rectly by, or under the supervi si on of, MKE <br />personne 1 . <br /> <br />2.1.2 Geologic Mapping <br /> <br />A surficial geology map of Peterson lake Reservoir is included in Figure V.2. <br />The dam foundati on and much of the reservoi r are in Precambri an metamorphi c <br />and igneous bedrock. Dark gray gneiss, schist, granite, and white pegmatite <br />of the Idaho Spri ngs Formation outcrop on both abutments and throughout the <br />northern one-half of the reservoir. Foliation and sChistocity are subvertical <br />and wavy; and strike approximately N70oE. Princ;"pal joint sets are parallel <br />to foliation and schistocity, N250W, 700NE and N20oE, 4SoNW. The western side <br />and southern end of the reservoir, including the area of the auxiliary <br />spillway, are covered with glacial till of Pleistocene age. The till is a <br />1 i ght brown, c1 ayey sand and gravel wi th 1 arge subrounded bou1 ders to four <br />feet in diameter. <br /> <br />2.1.3 Subsurface Investigation <br /> <br />Peterson lake Dam and Reservoi r were i nvesti gated usi ng four rotary bore <br />holes, 13 test pits, and 11S0 linear feet of seismic refraction survey lines. <br /> <br />-43- <br />