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Geotechnical Engineering Evaluation NGA File No. 1021318 <br />Cliff Drive Short Plat Residence Development February 2, 2018 <br />Everett, Washington Page 3 <br />At the surface of Test Pits 1 through 4 we encountered approximately 1.0 to 3.0 feet of dark brown to <br />orange -brown, silty fine to medium sand with varying amounts of gravel, roots, and organics, which we <br />generally interpreted as topsoil and/or undocumented fill soils. Underlying the fill and topsoil we <br />encountered light brown to gray, fine to medium sand with varying amounts of silt and gravel along along <br />with iron -oxide weathering, which we interpreted as native glacial outwash soils. Test Pit 1 through 4 <br />were terminated within native advanced outwash soils at respective depths of 7.0, 8.0, 10.0, and 8.0 feet <br />below the existing ground surface. <br />Hydrogeologic Conditions <br />Moderate to heavy groundwater seepage was encountered within Test Pit 4 at approximately 8.0 feet <br />below the existing ground surface. We interpret the water observed to be perched groundwater. Perched <br />water occurs when surface water infiltrates. Perched water does not represent a regional groundwater <br />"table" within the upper soil horizons. Perched water tends to vary spatially and is dependent upon the <br />amount of rainfall. We would expect the amount of perched groundwater to decrease during drier times <br />of the year and increase during wetter periods. <br />SENSITIVE AREA EVALUATION <br />Seismic Hazard <br />The 2015 International Building Code (IBC) seismic design section provides a basis for seismic design <br />of structures. Since medium dense or better glacial outwash soils were generally encountered underlying <br />the site at depth, the site conditions best fit the IBC description for Site Class D. Table 1 below provides <br />seismic design parameters for the site that are in conformance with the 2015 IBC, which specifies <br />a design earthquake having a 2% probability of occurrence in 50 years (return interval of 2,475 years), <br />and the 2008 USGS seismic hazard maps. <br />Table 1— 2015 IBC Seismic Design Parameters <br />Site Class <br />Spectral Acceleration <br />Spectral Acceleration <br />Site Coefficients <br />Design Spectral <br />at 0.2 sec. (g) <br />at 1.0 sec. (g) <br />Response <br />Ss <br />Si <br />Parameters <br />Fa <br />F, <br />SDs <br />SDI <br />r _7 <br />D <br />1.399 <br />0.531 <br />1.000 <br />1.500 <br />0.933 <br />0.531 <br />The spectral response accelerations were obtained from the USGS Earthquake Hazards Program <br />Interpolated Probabilistic Ground Motion website (2008 data) for the project latitude and longitude. <br />Hazards associated with seismic activity include liquefaction potential and amplification of ground <br />motion. Liquefaction is caused by a rise in pore pressures in a loose, fine sand deposit beneath the <br />NELSON GEOTECHN/CAL ASSOCIATES, INC. <br />