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2930 MAPLE ST KAISER PERMANENTE Geotech Report 2025-03-07
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2930 MAPLE ST KAISER PERMANENTE Geotech Report 2025-03-07
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3/7/2025 3:41:52 PM
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Address Document
Street Name
MAPLE ST
Street Number
2930
Tenant Name
KAISER PERMANENTE
Address Document Type
Geotech Report
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Geotechnical Engineering Report-Revised lrerracon <br /> Kaiser Everett Medical Center Everett,Washington -- s--- y� <br /> December 18, 2019 Terracon Project No. 81195071 GeoReport <br /> Description Value <br /> FPCA—Peak Ground Acceleration Site Coefficient 1.000 <br /> The IBC requires a site profile extending to a depth of 100 feet for seismic site classification. Borings were <br /> extended to a maximum depth of 40 feet. The site properties below the boring depth to 100 feet were estimated <br /> based on our experience and knowledge of geologic conditions of the general area. <br /> 2. These values were obtained using online seismic design maps and tools provided by OSHPD <br /> (https://seismicmaps.org ). ASCE 7 allows site coefficients Fa and Fy to be determined assuming that <br /> liquefaction does not occur for structures with fundamental periods of vibration less than 0.5 second. Based <br /> on the results of the exploration program,Site Class C may be used to determine the values of Fa and F,,.The <br /> fundamental period of vibration for the structure should be verified by the structural engineer. <br /> Surface-Fault Rupture <br /> The hazard of damage from onsite fault rupture appears to be low based on review of the USGS <br /> Earthquake Hazards Program Quaternary Faults and Folds Database available online <br /> (https://usgs.maps.arcgis.com/apps/webappviewer/index.html?id=5a6O38b3a1684561 a9bOaadf <br /> 88412fcf) accessed on June 10, 2019. The closest mapped fault is the Southern Whidbey Island <br /> fault zone, which lies approximately 6.8 miles to the southwest of the site. <br /> LIQUEFACTION <br /> Liquefaction is the phenomenon where saturated soils develop high porewater pressures during <br /> seismic shaking and lose their strength characteristics. This phenomenon generally occurs in <br /> areas of high seismicity, where groundwater is shallow and loose granular soils or relatively non- <br /> plastic fine-grained soils are present. Based on the site geology and subsurface groundwater <br /> conditions, we anticipate that the risk of liquefaction of the site soils is low. <br /> FLOOR SLABS <br /> Design parameters for floor slabs assume the requirements for Earthwork have been followed. <br /> Specific attention should be given to positive drainage away from the structure and positive drainage <br /> of the aggregate base beneath the floor slab. <br /> Floor Slab Design Parameters <br /> Item Description <br /> Minimum 6 inches of capillary break material consisting of free-draining, <br /> Floor Slab Support granular material with less than 3% retained on the#200 sieve) <br /> Responsive ■ Resourceful ■ Reliable <br />
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