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SteNen Jacobson JN 98313 <br /> Page 2 <br /> August 17, 1998 <br /> the soils encountered. "Grab" samples of selected subsuriace soils were collected from the <br /> trackhoe bucket. The Test Pit Logs are attached to this report as Plates 3 through 7. <br /> In the westernmost portion of the site, adjacent to East Marine View Drive, the test pits <br /> encountered 6 to 10 feet of fill consisting of loose, brown, silty sand with some organics, gravel, <br /> and concrete and asphalt debris. Beneath 6 to 12 inches of topsoil, found below the fill or mostly at <br /> the ground surface, the native soils consist of 3 to 5 feet of loose to medium-dense, brown, <br /> weathered, silty sand wilh gravel which then became gray and very dense. The silty sands have <br /> been giacially consolid�ted and are referred to as glacial till. In our exploretions, the dense to very <br /> dense glacial till was encountered to a maximum =xplored depth of 16.5 feet below existing surface <br /> grade. <br /> The finai logs represent our interpretations of the fieid logs and laboratory tests. The stratificalion <br /> lines on the logs represent the approximale bounclaries between soil types at the exploration <br /> locations. T�ie actuai transition between soil types rray be gradual, and subsurface conditions can <br /> vary between exploration locations. The logs provicle specific subsurface information only at the <br /> localions tested. The relative densities and moisture descriptions indicated on the test pit logs are <br /> interpretive descriptions based on the conditions observed during excavation. The compaction of <br /> backfill was not in the scope of our services. Loosa soil wiil therefore be found in the area of the <br /> test pits. If lhis pre:.ents a problem, the i:a�kfiit ���ill need to be removed and replaced with <br /> structural fill during construction. <br /> Groundwater <br /> No groundwater seepage was observed in any of the test pits, however, they were left open for <br /> oniy a short time period. It should be noled that oro�ndwater levels vary seasonally with rainfall <br /> and other factors. We anticipate that groundwater cc�lc: be found between lhe near-surface, <br /> weathered soil and the underlying giacial tiil and in more perm�ahie soil layers or pockets within the <br /> till soils, especially durin� the normally wet winter and spring months. <br /> CONCLUSIONS AND RECOMMENDATIONS <br /> General <br /> Based on the test pits and our observations made during our site visit, it is our opinion that the <br /> proposed multi-residential development is feasibie on this site from a geotechnical engineering <br /> standpoint. The proposed buildings should be supported on conventional foundalions bearing on <br /> the dense to very dense glacial till soils. Que to the large size of the buiidings and the deep cuts <br /> proposed on the western ends of the buildings, we recommend that no structurai fill be placed <br /> under any portion of the buildings due to the potential for differential settlement. Lean-mix concrete <br /> could be used beneath footings on the eastern sides of the buildings where the proposed finish <br /> floor levels are above the existing ground level. <br /> One oF the main geotechnical challenges for this project is the construction of the below-grade <br /> parking levels and the proximity of East Marine View Drive to the excavation. Because of the large <br /> cuts proposed for the two buildings near the western property line, temporary shoring would be <br /> needed unless construction easements can be acquired from the City of Everett. All cuts siopes in <br /> ci:�,n cn cu�sui:r,��rs.mc <br />