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r r <br /> August 18, 2014 <br /> Gibson Bluff <br /> L&A Job No. 14-056 <br /> Page 5 <br /> allow stormwater to seep through relatively easily. The Esperance sand deposits can <br /> stand in steep cuts or natural slopes for extended period when undisturbed. Where <br /> exposed on slopes devoid of vegetation cover and subject to storm runoff or groundwater <br /> seepage, the Esperance sand deposits can be gradually eroded and may slough and <br /> redeposit to a flatter inclination. <br /> Soil Condition <br /> Subsurface condition at the site was explored on June 16, 2014, with three test borings <br /> drilled with a portable drill rig owned and operated by Davies Drilling of Seattle. The <br /> approximate locations of the test borings are shown on Plate 2 - Site and Exploration <br /> Location Plan. The test borings were each drilled to 31.5 feet deep. Soil samples <br /> obtained from the test borings were visually classified in general accordance with United <br /> Soil Classification System, a copy of which is presented on Plate 3. A geotechnical <br /> engineer from our office was present during the exploration, examined soil samples <br /> retrieved from the test borings, recorded soil and geologic conditions encountered, and <br /> completed logs of the test borings. Detailed descriptions of the soil layers encountered <br /> during site exploration are presented in test boring logs on Plates 4 through 6. <br /> Standard Penetration Tests were conducted, in accordance with ASTM D-1586, in the <br /> bore holes using a standard split-spoon sampler of 2-inch outside diameter, driven with a <br /> 140-pound hammer that was raised and released for a 30-inch free fall. The number of <br /> blows required to advance the sampler a given distance is an indication of the density for <br /> granular soils or the consistency of cohesive soils. The sampler was advanced 18 inches <br /> LIU & ASSOCIATES, INC. <br />