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1135 CRAFTSMAN WAY Geotech Report 2018-01-02 MF Import
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1135 CRAFTSMAN WAY Geotech Report 2018-01-02 MF Import
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Last modified
10/25/2022 1:43:16 PM
Creation date
2/18/2021 9:52:53 AM
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Address Document
Street Name
CRAFTSMAN WAY
Street Number
1135
Address Document Type
Geotech Report
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r . <br /> ' Hart Crowser <br /> J-3446-01 <br /> ► Fapect ]ess than 1 to 1'h inches of setflement at footings. <br /> ► Design slabs with a modulus of subgrade reaction of 200 pounds per <br /> cubic inch. <br /> ► Provide 4 inches of capillary break material beneath slabs. <br /> ► Desi� pavement sections using a CSR value of 15 percent <br /> SUBSURFACE CONDTI'IONS <br /> Our understanding of the subsurface conditions is based on five deep <br /> borings, two shallow borina,s and laboratory testing of the samples (see <br /> Figure 2). Subsurface soil conditions interpreted from explorations <br /> accomplished at the site and soIl properties inferred from the 5eid and <br /> laboratory tesu formed the b:uis for developing the conclusions and <br /> recommendations contained wzthin this report. The nature and extent <br /> of variatians between the explorations may not become evident until <br /> construction. If variations then appear evident, it w11 be necessary to <br /> re-evaluate che recommendations of this report Deta7s of the <br /> conditions observed at the boring locations aze shown on the logs <br /> included in Appendix A ar�d should be referred to far specific <br /> information. <br /> SoiLs - �fedium Derue Granular Materia! aver Glacia! SoiLs <br /> Figure 3 is a generalized subs•.uface profle running north/south through <br /> the proposed new warehouse and covered storage bLuldings. <br /> 'I'he upper 20 to 30 feet of soils consist of ]oose to medium dense s�7ty <br /> sand and medium stiff to stiff sandy s�7t both with shell and wood <br /> fragmenu. We interpret this upper 20 to 30 feet of material as dredged <br /> hydraulic 5ll. Older maps and aerial photogaphs of the area indicate <br /> that most, if not all, of the sice was once a part of Port Gardner Bay. <br /> We interpret the wood fragments to be the result of the lumber mi7ling <br /> operations prior to filling Port Gardner Bay. The shell fra�ents, <br /> _ cspecially those located in soils above the sea ]evei, are further evidence <br /> of past filling activities using dredged so�s. <br /> � Pag �4 <br />
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