Laserfiche WebLink
<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 />3.0 GEOTECHNICAL EVALUATION <br /> <br />3.1 Field Investigation <br /> <br />3.1.1 General <br /> <br />Geotechnical investigations at Comanche Dam were carried out to supplement <br />work performed previously in 1965 and 1982. The objective was to characterize <br />the embankment dam and foundati on, i nvesti gate sources of potenti a 1 <br />construction material and obtain soil samples for laboratory testing. The <br />field investigations consisted of surficial geologic mapping and subsurface <br />exploration by means of bore holes, test pits, and seismic refraction <br />surveys. Multi-level standpipe piezometers were installed in each bore hole <br />upon compl eti on. The work was performed duri ng the months of August and <br />September, 1986 and October, 1987, directly by or under the supervision of MKE <br />personnel. <br /> <br />3.1.2 Geologic Mapping <br /> <br />A surficial geologic map is included in Drawing 2024-GIl. Comanche Dam and <br />Reservoi r is si tuated on a gl aci al morai ne of Plei stocene age composed of <br />sandy gravel till. The glacial till contains large subrounded erratics to six <br />feet in di ameter. Lenti cul ar-shaped 1 acustri ne deposits composed of thi nly <br />bedded fine sand and silt occur within the moraine. These are associated with <br />shallOl'l lakes that formed from seasonal melting at the edge of the advancing <br />or receding glacier. The sides of the glaciated valley are composed of <br />metamorphic and igneous rock of the Idaho Spri ngs Formati on whi ch is of <br />Preca~brian age. Several quarternary talus deposits of angular boulders occur <br />at the base of the steeper slopes and terminate within the reservoir. <br /> <br />3.1.3 Subsurface Investigation <br /> <br />The Comanche Dam and Reservoi r were i nvesti gated in 1986 and 1987 by fi ve <br />rotary bore holes, 23 test pits, and 1750 linear feet of seismic refraction <br /> <br />2084H <br /> <br />-10- <br />