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J. H. KLEINEELDER & ASSOCIATES File No. S-2282-1 <br /> February 9, 1978 <br /> PAGE THREE <br /> FIELD EXPLORATIONS <br /> The field explorations for this project were performed on <br /> January 20, 1978, and consisted of drilling and sampling five test <br /> borings . The approximate locations at which the borings were made <br /> are shown on the Site Plan, Plate I. All borings were drilled <br /> with truck mounted 6-inch diameter auger-type drilling equipment. <br /> Relatively undisturbed core samples were collected by driving a <br /> 2-inch inside diameter sampler into the soil using a 140-pound- <br /> hammer falling 30 inches ±. The number of blows required to <br /> advance the sampler one foot into the soil are noted on the Logs <br /> of Borings at the corresponding sample locations . All borings <br /> were drilled under the direction of an engineering geologist <br /> from our firm, who classified the soils and maintained a continuous <br /> log of the soils encountered in the borings . <br /> SOIL CONDITIONS <br /> The surface soils encountered at the locations explored <br /> consist of a grey-brown to brown silty fine sand. This soil <br /> is loose and extends to depths varying from 4 to 8-1/2 feet <br /> below the existing ground surface. The surface soil is <br /> underlain by silty and clayey sand with interbedded sandy silts <br /> to the total depth explored of 30 feet in the test borings . These <br /> soils are generally medium-dense or stiff. A medium-dense clean <br /> fine to medium sand was encountered between 6 to 11 feet at <br /> Boring Nos . 4 and 5, and between 8 to 15 feet in Boring No. 1. <br /> Ground water was encountered at approximately 14 feet below <br /> the ground surface in Boring No. 1. However, ground water was <br /> not encountered in the remaining borings . It appears that the <br /> water encountered in Boring No. 1 is perched water. San Joaquin <br /> County ground water maps for Spring 1977, indicate a ground water <br /> elevation of -10 feet, or approximately ± 30 feet below the existing <br /> ground surface at the site . It is possible that the ground water <br />