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The CSZ is considered as being capable of generating earthquakes of magnitudes 8 to 9. No earthquakes <br /> on the CSZ have been instrumentally recorded; however, through the geologic record and historical <br /> records of tsunamis in Japan, it is believed that the most recent CSZ event occurred in the year 1700. <br /> Recurrence intervals for CSZ interplate earthquakes are thought to be on the order of 400 to 600 years. <br /> 4.1.2.Seismic Hazards <br /> We evaluated the site for seismic hazards including liquefaction, lateral spreading and fault rupture. Our <br /> evaluation indicates the site does not have liquefiable soils present and, therefore, also has little to no <br /> risk of liquefaction-induced ground disturbance including lateral spreading. There are no mapped faults in <br /> the immediate vicinity of the site, with the exception of the Southern Whidbey Island fault zone mapped <br /> approximately 6 miles southwest of the site. Our opinion is that there is a low risk of fault displacement <br /> resulting in ground rupture at the surface. <br /> 4.1.3.2015 IBC Seismic Design Information <br /> We recommend the use of the 2015 IBC parameters listed in Table 1 for soil profile type, short period <br /> spectral response acceleration (Ss), 1-second period spectral response acceleration (Si) and seismic <br /> coefficients (FA and Fv)for the project site. <br /> TABLE 1. 2015 IBC PARAMTERS <br /> 2016 IBC Parameter Recommended Value <br /> Soil Profile Type C <br /> Short Period Spectral Response Acceleration,Ss(percent g) 125.9 <br /> 1-Second Period Spectral Response Acceleration,Sz(percent g) 47.9 <br /> Seismic Coefficient, FA 1.0 <br /> Seismic Coefficient,Fv 1.32 <br /> 4.2. Fo.ux-,dations <br /> We recommend that the proposed LRC building be supported on shallow spread footings founded on the <br /> dense to very dense advance outwash deposits encountered in our borings or on properly compacted <br /> structural fill extending down to medium dense to very dense native advance outwash. Existing fill and <br /> unsuitable weathered glacial soils should be removed from under the planned LRC building foundations. <br /> For shallow foundation support, we recommend widths of at least 24 and 36 inches, respectively, for <br /> continuous wall and isolated column footings supporting the proposed building. The design frost depth in <br /> the Puget Sound area is 12 inches; therefore, we recommend that exterior footings for the building be <br /> founded at least 18 inches below lowest adjacent finished grade. Interior footings should be founded at <br /> least 12 inches below bottom of slab or adjacent finished grade. <br /> The following recommendations for the building foundations are based on the subsurface conditions <br /> observed in the borings. <br /> GEOENGINEERS� July22,2019 Pagc5 <br /> -� Fk ND.5886-011.00 <br />