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I <br /> Interwest Construction Co.-Railway Avenue Improvements, Everett,WA Feb. 14,2019/Revised Feb. 7,2020 <br /> IGeotechnical Engineering Report P1486-T18 <br /> Throughout the drilling operation, soil samples were obtained at 21/2 to 5-foot depth intervals by <br /> I means of the Standard Penetration Test (SPT) per American Society for Testing and Materials <br /> (ASTM:D-1586),or using a large split-spoon sampler. This testing and sampling procedure consists <br /> of driving a standard 2-inch-outside-diameter steel split-spoon sampler 18 inches into the soil with a <br /> I 140-pound hammer free-falling 30 inches. The number of blows struck during the final 12 inches is <br /> recorded on the boring logs. If a total of 50 blows are struck within any 6-inch interval,the driving <br /> is stopped, and the blow count is recorded as 50 blows for the actual penetration distance. The <br /> I resulting blow count values indicate the relative density of granular soils and the relative <br /> consistency of cohesive soils. <br /> IThe enclosed boring logs describe the vertical sequence of soils and materials encountered in the <br /> boring, based primarily on our field classifications and supported by our subsequent laboratory <br /> examination and testing. Where a soil contact was observed to be gradational,our logs indicate the <br /> Iaverage contact depth. Where a soil type changed between sample intervals, we inferred the <br /> contact depth. Our logs also graphically indicate the blow count,sample type,sample number,and <br /> I approximate depth of each soil sample obtained from the borings, as well as any laboratory tests <br /> performed on these soil samples. If any groundwater was encountered in a borehole, the <br /> approximate groundwater depth is depicted on the boring log. Groundwater depth estimates are <br /> I typically based on the moisture content of soil samples,the wetted height on the drilling rods,and <br /> the water level measured in the borehole after the auger has been extracted. The soils were <br /> classified visually in general accordance with the system described in Figure A-1,which includes a <br /> key to our exploration logs. Summary logs of the explorations are included as Figures A-2 and A-7. <br /> 3.0 SITE CONDITIONS <br /> IThe following sections present our observations, measurements, findings, and interpretations <br /> regarding, surface, soil, groundwater, and infiltration conditions. <br /> I3.1 Surface Conditions <br /> As previously indicated, the project site consists of a historical log and timber storage site for the <br /> I Kimberly-Clark Corporation,parcels of which are now owned by the City of Everett or previously <br /> listed companies. Several abandoned concrete structures remain alongthe length of the proposed <br /> p g P P <br /> roadway, water line, and storm line extension. Most of these structures appear partially buried <br /> I and/or have fallen into disrepair. Multiple large piles of rubble and construction debris are also <br /> scattered, concentrated toward the northern end of the project site. The area appears to be used <br /> mainly for stockpiling and storage of shipping containers and truck trailers at present. <br /> I <br /> The length of the project site and the surrounding area is relatively flat,with very gradual elevation <br /> gain from the Snohomish River shoreline east of the site to the BNSF Railroad ROW west of the site. <br /> I <br /> Vegetation onsite consists mainly of various types of grass, which is tall and unkempt in many <br /> I portions of the project area. Ornamental trees line the gravel entrances to some of the parcels <br /> owned by the City of Everett, and small saplings have begun to grow in neighboring areas. <br /> I <br /> IMigizi Group, Inc. Page 3 of 13 <br />