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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 /> <br />Specific details for each alternative are shown in Table 3. <br /> <br />Item <br />Top of Dam Elevation <br />-Spill~aJ{Ifle~atI;n------------- <br /> <br />------------------------------- <br />Dam Height <br /> <br />------------------------------- <br />Dam Length <br />------------------------------- <br />Reservoir Surface Area <br /> <br />TABLE 3 - Dam Alternatives <br />Alternative 1 <br /> <br />17.1 acres <br /> <br />Alternative 2 <br />5367 feet <br /> <br />------------------------------- <br />5360 feet <br />------------------------------- <br />47 feet <br /> <br />------------------------------- <br />1156 feet <br />------------------------------- <br />16.9 acres <br />------------------------------- <br />300 ac-ft <br />e sIte may gIVe <br /> <br />5375 feet <br /> <br />------------------------------- <br />5368 feet <br />------------------------------- <br />45 feet <br /> <br />------------------------------- <br />1040 feet <br /> <br />------------------------------- ------------------------------- <br />Normal Storage Capacity 300 ac-ft <br /> <br />These v ues are approxunatlOns ase <br />slightly different values. <br /> <br /> <br />PLAN OF DEVELOPMENT <br /> <br />General. To be able to evaluate the physical needs and subsequent costs for each dam site, a geotechnical <br />evaluation of each site was conducted. This included subsurface investigations, laboratory testing of the <br />soils form the site, a geotechnical evaluation of stability and seepage, and a hydrologic and hydraulic <br />evaluation of the required spillway and outlet works. A summary of these evaluations follows. <br /> <br />Geotechnical Investigations. The geotechnical investigations conducted on the proposed reservoir site <br />are described in Appendix B of this report. These investigations were conducted in June of200l by Smith <br />Geotechnical. The investigation included drilling four borings at the north dam site, two borings at the <br />south dam site, four borings in the borrow are within the reservoir, and laboratory testing on selected <br />samples. The plan of development is based on this data and additional drilling, sampling, and testing will <br />have to be conducted prior to final design after the final location for the dam is determined. <br /> <br />Soil and Rock Description. <br /> <br />1. Overburden Soils. The overburden soils at the dam sites consist of overburden sandy <br />clays, clayey sands, silty sands, and sandy silts. These soils range from nonplastic to low plastic <br />with t'1e plastic soils having a plasticity index (PI) or approximately 15. These soils should be <br />acceptable for use to construct the dam core whereas the nonplastic soils should not be utilized to <br />construct the core but can be used in the dam shell. <br /> <br />The soils were found to be relatively uniform across the site with the more plastic soils being found <br />on the east side of the drainage and the low to nonplastic soils being encountered on the west side <br />of the drainage. We would recommend only the soils on the east side of the drainage be used for <br />core material. <br /> <br />2. Bedrock. Underlying the overburden soil is the Lyons sandstone. The bedrock was found <br />at depths ranging from ten (10) feet to thirty (30) feet below grade. The bedrock is relatively <br />hard, fractured, and is thinly bedded. A quarry operation north of the site provides a good <br />location to view this formation. <br /> <br /> <br />The Lyons sandstone is a sedimentary rock of the Triassic and Permian ages and is fine grained <br />with weak to strong cementation. This rock may be susceptible to solutioning in a partially <br />saturated environment and may be susceptible to erosion where the cementation is weak. The <br />shear strength and hardness of the rock is acceptable for a dam foundation of the height proposed. <br />The only weakness is the seepage potential due to the fractured nature of the rock. <br /> <br />3. Borrow/Materials. The primary source of borrow materials is expected to come from <br /> <br />Stone Canyon Dam Feasibility <br /> <br />Page 8 <br />