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Subsurface Exploration, Geologic Hazard, and <br /> Boardwalk Condominium, Building C Geotechnical Engineering Report <br /> Everett, Washington Project and Site Conditions <br /> variations beyond the field exploration may not become fully evident until construction. If <br /> variations are observed at that time, it may be necessary to re-evaluate specific <br /> recommendations in this report and make appropriate changes. <br /> 3.1 Exploration Boring <br /> The exploration boring was completed by advancing a hollow-stem auger with a hand-portable, <br /> Acker-type drill rig. During the drilling process, samples were generally obtained at 2.5- to <br /> 5-foot-depth intervals. The exploration boring was continuously observed and logged by an <br /> engineering geologist from our firm. The exploration log presented in the Appendix is based <br /> on the field log, drilling action, and inspection of the samples collected. <br /> Disturbed but representative samples were obtained from the exploration boring by using the <br /> Standard Penetration Test (SPT) procedure in accordance with American Society for Testing <br /> and Materials (ASTM):D 1586. This test and sampling method consists of driving a standard <br /> 2-inch, outside-diameter, split-barrel sampler a distance of 18 inches into the soil with a <br /> 140-pound hammer free-falling a distance of 30 inches. The number of blows for each 6-inch <br /> interval is recorded and the number of blows required to drive the sampler the final 12 inches <br /> is known as the Standard Penetration Resistance ("N") or blow count. If a total of 50 is <br /> recorded within one 6-inch interval, the blow count is recorded as the number of blows for the <br /> corresponding number of inches of penetration. The resistance, or N-value, provides a <br /> measure of the relative density of granular soils or the relative consistency of cohesive soils; <br /> these values are plotted on the attached exploration boring log (Appendix). <br /> The samples obtained from the split-barrel sampler were classified in the field and <br /> representative portions placed in watertight containers. The samples were then transported to <br /> our laboratory for further visual classification. <br /> 4.0 SUBSURFACE CONDITIONS <br /> Subsurface conditions at the project site were inferred from the field exploration accomplished <br /> for this study, visual reconnaissance of the site, and review of applicable geologic literature. <br /> As shown on the exploration log, the exploration boring generally encountered approximately <br /> 12 feet of loose to medium dense fill material and weathered native soils. Below a depth of <br /> approximately 121/2 feet, we encountered medium dense to very dense native soils interpreted <br /> as Vashon ice contact deposits. The following section presents more detailed subsurface <br /> information organized from the shallowest (youngest) to the deepest (oldest) sediment types. <br /> September 12, 2012 ASSOCIATED EARTH SCIENCES, INC. <br /> FSM11d—EE120288A8—Projects1201202881EFNP Page 3 <br />