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observed in fow of the borings,and thc base course was absent in the remaining borings. Slight to strong <br /> pctroleum odors werc obscrved in samples obtained from borings D-6 and B-9 at about 7'/s ro 19 fxt <br /> bclow existing site grades. The soil uni4c obscrved in the borings are desc�ibed below. <br /> Fill. Fill was encountered in each of the borings and typically varies from 6 co 12 feet in thickness. We <br /> understand the fill placcd along the alley curtently bisecting the property may extend up to 20 feet below• <br /> the ground surface. The fill primarily consists of very loose to medium dense sand with vaziable silt and <br /> occaaional gravel. As noted previous!�, boring B-3 aas located in the northeast corna of the site and <br /> cncountemd a concrete obstruction al about 10 feet below thc ground surface. <br /> Outwaeh Deposits. Outwash deposits undcrlic the fill and gencrally consist of inedium dense to very <br /> densc, finc to medium sand with variablr amounts of silt. The outwash varies from 5 to 10 feet in <br /> ihickncss. <br /> Glaciil Till. Glacial till was encountercd at a depth of 15 to 17 fcct bclow existing grade in a�.i of the <br /> borings. The glacial till typically consists of vcry dense silry sand with variable amounts of g2ve1 and <br /> cobbles. Thc upper few feet of thc till in boring E3-6 consisted of mcdium dense soils. <br /> Groundwafer Condltlons <br /> Perchcd groundwater was obscrved in fivc of thc tcn horings during drilling at depths ranging from 12 to <br /> 22 fcet below thc existing ground surfacc. Although perchcd walcr was only observcd in fivc borings, <br /> moist to wct soils were observed in several other boriugs. <br /> Perchcd groundwater is common in glacial till soils wherc water Gom precipitalion percolates through the <br /> more pertncable fill and outwash soils and mmes laterally on the very dense, Iess pertneable glacial tiL'. <br /> We expect that perched groundwatcr levcls will fluctuale scasonally with prccipitation. <br /> CONCLUSIONS AND RECOMMENDATIONS <br /> SUMMARY OF KEY GEOTECHNICAL ISSUES <br /> I3ascd on thc results of our subsurfacc cxplotation program and gco�cchnical analyses,subsurfacc soil and <br /> groundwatcr conditions arc favorablc for construction of thc Potala Villagc Mixed-Usc building. A <br /> summary of Ihe primary gcotechnical considerations is pro��ided below. Thc summary is presented for <br /> introductory purposcs only and should be used in c�.ijunction with the complctc rccommendations <br /> prcscntcd in this rcport. <br /> • Subsurfacc soils encounlercd at the site consist of Ihrec geologic units: fill,ounvash deposits,and <br /> glaci�l till. The fill ranges from 6 l0 12 fcet in thickncss in our borings; however, wc anticipatc <br /> GII up to 20 fcet thick abo��c thc scwcr located in thc alley. <br /> • 1'crched groundwatcr was obscrvcd in fivc of shc�cn borings during drilling. <br /> • 7'he site is designatcd as scismic Site Class C per the 20061I3C. <br /> • Cantilcver soldicr pilc H�allc will pro��ide an economical rctention sqslcm for the pmposed <br /> cxcavations at thc sitc. <br /> + Dcsign of thc foundation and requirc� exca��ation aill necd to address conditions of thc existing <br /> (ni idation of'Ihc Snohomisl:Hcalth Uistrict building. <br /> flkA'�� 1;n1-un�-nn Pnge3 G[oEMG�MHIIE� <br /> hn,r 6.1IulA' <br /> � <br />