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Geotechnical Engineering Evaluation NGA File No. 1322621 <br /> Clark Garage Slope February 4,2022 <br /> Everett,Washington Page 3 <br /> Explorations: We visited the site on January 4, 2022 to explore the subsurface conditions along the steep <br /> slope and the proposed residence addition. The explorations consisted of three hand augers extending to <br /> depths of up to 5.0 feet below existing ground surface. A geologist from Nelson Geotechnical Associates, <br /> Inc. (NGA) completed the explorations, and examined the soils and geologic conditions encountered. All <br /> of our explorations encountered approximately 1.0 to 1.5 feet of orange-brown organic-rich silty sand <br /> with gravel and roots that we interpreted as surficial topsoil and/or undocumented fill. Underlying the <br /> undocumented fill and/or surficial topsoil in all of our explorations, we encountered medium dense to <br /> dense gray, silty fine to coarse sand with varying amounts of gravel and cobbles that we interpreted to be <br /> native glacial till soils. All of our explorations were terminated within native glacial soils at depths in the <br /> range of 3.0 to 5.0 feet below the existing ground surface. <br /> Hydrogeologic Conditions <br /> Groundwater seepage was encountered within our explorations in hand auger 1 and 2 at depths of 1.5 <br /> and 1.0 feet below the existing ground surface, respectfully. We interpreted this water to be perched <br /> water. Perched water conditions may occur on the site during periods of wet weather. Perched water <br /> occurs when surface water infiltrates through less dense, more permeable soils and accumulates on top <br /> of underlying, less permeable soils. Perched water does not represent a regional groundwater "table" <br /> within the upper soil horizons. Perched water tends to vary spatially and is dependent upon the amount <br /> of rainfall. We would expect the amount of perched water to decrease during drier times of the year and <br /> increase during wetter periods. <br /> SENSITIVE AREA EVALUATION <br /> Seismic Hazard <br /> We reviewed the 2018 International Building Code (IBC) for seismic site classification for this project. <br /> Since very dense soils are interpreted to underlie the site at depth,the site best fits the IBC description for <br /> Site Class D. Table 1 below provides seismic design parameters for the site that are in conformance with <br /> the 2018 IBC, which specifies a design earthquake having a two percent probability of occurrence in 50 <br /> years(return interval of 2,475 years), and the 2008 USGS seismic hazard maps. <br /> Table 1—2018 IBC Seismic Design Parameters <br /> Site Class Spectral Spectral Site Coefficients Design Spectral <br /> Acceleration at 0.2 Acceleration at 1.0 Response Parameters <br /> sec. (g) sec. (g) <br /> S, S1 Fa F„ SDS Sol <br /> D 1.420 0.543 1.000 1.500 0.946 0.543 <br /> NELSON GEOTECHNICAL ASSOCIATES, INC. <br />