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( '; <br /> � Proposed Modernilation and Addirions to Subsurjace Explorarion, Geolvgic Hazards. <br /> 6'iserthower Middle Schoo! and Geotechnica!Engineering Repon <br /> Ereretr, Washington Pro'ecr and Site Corditrons <br /> foot depth intervals. The exploration borings were continuously observed and logged by a <br /> geotechnical engineer from our firm. The exploration logs presented in the Appendix are <br /> based on the field logs, drilling actio:�, and inspection of the samples secured. <br /> Disturbed but representative samples were obtained by using the Standard Penetration Test <br /> procedure in accordance with ASTM:D 1586. This test and sampling method consists of <br /> driving a ssandard 2-inch outside-diameter, split-barrel sampler a distance of 18 inches into the <br /> soil with o 140-pound haznmer free-falling a distance of 30 inches. The number of blows for <br /> each 6-inch interval is recorded and the number of blows required to drive the sampler the <br /> final 12 inches is known as the Standard Penetration Resistance ("N") or blow count. If a total <br /> of 50 is recorded within one 6-inch interval, the blow count is recorded as the number of blows <br /> for the corresponding number of inr.hes of penetration. The resistance, or N-value, provides a <br /> measure of the relative densiry of granular soils or the relative consistency of cohesive soils; <br /> these values are plotted on the attached exploration boring logs. i <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 transparted ro <br /> our laboratory for further visual classification and laboratory testing, as necessary. <br /> 4.0 SUBSURFACE CONDITIONS <br /> Subsurface conditions at the projec[ site were inferred &om the field explorations accomplished <br /> for this study and visual reconnaissance of the site. As shown on the field soil logs, the <br /> exploration borings generally encountered fill overlying glacially consolidated "till" soils. The <br /> depth to the underlying dense till varied from approximately 1 to 12 feet. <br /> Sub�urface conditions at the project site were inferred from the field explorations accomplished <br /> for this study and visual reconnaissance of the site. As shown on the field soil logs beneath the <br /> fill/topsoil, exploration borings generally encountered a mixture of silt, fine to coarse sand and <br /> rounded gravel interpreted as till deposits. This interpretation is consistent with the geology <br /> mapped in the site area as shown on the U.S. Geological Survey (USGS) publication: <br /> Preliminary Geologic Mnp of S«rficinl Deposits in the Seattle 30' X 60" Quadrangle, by <br /> Yount, Minard, and Dembroff (1993). The following section presents more detailed <br /> subsurface information beginning from the youngest (shallowest) to oldest (deepest) sediment <br /> types. <br /> lanunrv 33, s'ODd ASSOCIdTED E.1RTN SC/E,VCES, LVC. �` <br /> .517(d-KEOJ739d3-Pro�rcuCWl7JyiXfi��'Y- R':K Page 4 1 71 <br /> �y <br />