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Geotechnical Repoi-t - Revised <br />Proposed Apartments: 1002, 1006, and 1008 Broadway Street, Everett, Washington <br />May 12, 2015 <br />3.4 GROUNDWATER <br />Groundwater seepage was not encountered in ow� borings or hand augcrs. The till <br />underlying the site generally has low permeability and perched ground�vater may develop <br />in lenses of more pei7neable soi) within the till foi7nation. If encountei•ed, we anticipate <br />groundwater seepage rates will be light. <br />There will be fluctuations in seepage depeiidin� o�� the seasoii, amowlt of rainiall, surface <br />water iunoff, and other factors. Generally, the water level is higher and seepage rates are <br />greater in tlie wetter, winter months (typically October through May). <br />4.0 GEOTECHNICAL RECOMMENDATlONS <br />4.1 SEI51111C DESIGN PARAME'1'ERS <br />The 2012 Intetnational Building Code (IBC) seismic design section provides a basis for <br />seismic design of strvctures. Table 1 below provides seismic design parameters for the <br />site that are in confonnance with the 2012 IBC, which specifes a design earthquake <br />having a 2% probability of occurrence in 50 years (rehu�n interval of 2,475 years), and the <br />2008 USGS seismic hazard maps. <br />Table 1— Seismic Design Parlineters <br />Spectral Spectral Site Design Spectral Control Periods <br />Acceleration Acceleration Response <br />Site Coefficients [sec.] <br />Class at 0.2 sec. [g] at I.0 sea �g] Parameters <br />SS S� Fa F�• Sos S�>i To Ts <br />C 1.2fi4 0.481 I.U00 1.319 0.843 0.423 0.100 0.502 <br />The spectral response accelerations were obtained from the USGS Earthquake Hazards <br />Program Interpolated Probabilistic Gi•ound Motion website (2008 data) f'oi• the project <br />latitude and longitude. <br />Liquefactin» Pote�rtial: Lic�uefaction is a pi•ocess that cali occur when soils lose shear• <br />stc•ength for• sliort periods of time during a seismic event. Ground shaking of suf'ficient <br />strength and duration results in the loss of grain-to-grain contact and an increase in pore <br />��ater pressure, causing tlie soil to behave as a fluid. Soils �vith a potential for <br />� 5-0-1� IOUA 13madway, Reviscd P�1�C S 1�21]i�i�;0, �i7C. <br />