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PHASE I EXPLORATIONS <br /> HWA GeoSciences Inc. (HWA) conducted four(4) geotechnical borings during Phase I <br /> explorations. The borings were advanced by Holocene Drilling Inc., of Fife, Washington, <br /> on August 15th, 2014. A hollow stem auger and automatic hydraulic hammer was used to <br /> advance these borings. <br /> PHASE II EXPLORATIONS <br /> HWA GeoSciences Inc. (HWA) advanced two (2)machine-drilled boring and five (5) <br /> hand borings during Phase II explorations. The machine drilled boring was advanced by <br /> Environmental Drilling Inc. (EDI), of Snohomish, Washington, using a hollow stem <br /> auger. The hand borings were advanced by HWA personnel on February 2n1, 2016. <br /> Dynamic cone penetrometer(DCP)testing was performed in each hand boring to evaluate <br /> soil density at depths below the bottom of the hand boring. <br /> Standard Penetration Test(SPT) sampling was performed using a 2-inch outside diameter <br /> split-spoon sampler driven by a 140-pound auto hammer for all machine-drilled borings. <br /> During the SPT, samples were obtained by driving the sampler 18 inches into the soil <br /> with the hammer free-falling 30 inches. The numbers of blows required for each 6 inches <br /> of penetration were recorded. The Standard Penetration Resistance ("N-value") of the <br /> soil is calculated as the number of blows required for the final 12 inches of penetration. <br /> This resistance, or N-value,provides an indication of relative density of granular soils and <br /> the relative consistency of cohesive soils; both indicators of soil strength and foundation <br /> bearing capacity. <br /> A geotechnical engineer or geologist from HWA logged each exploration and recorded all <br /> pertinent information. Pertinent information including soil sample depths, stratigraphy, <br /> soil engineering characteristics, and ground water occurrence was recorded. The <br /> stratigraphic contacts shown on the individual exploration logs represent the approximate <br /> boundaries between soil types; actual transitions may be more gradual. The soil and <br /> ground water conditions depicted are only for the specific date and location reported and, <br /> therefore, are not necessarily representative of other locations and times. A legend of the <br /> terms and symbols used on the exploration log is presented in Figure A-1. Summary logs <br /> of the borehole exploration are presented in Figures A-2 through A-12. <br />