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32A - TTM 2005-11, 2000 E FIRST
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32A - TTM 2005-11, 2000 E FIRST
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Last modified
1/3/2012 4:46:57 PM
Creation date
4/26/2006 11:54:20 AM
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City Clerk
Doc Type
Agenda Packet
Item #
32A
Date
5/1/2006
Destruction Year
2011
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<br />A-2. Strong Seismic Ground shaking? <br /> <br />Less Than Significant Impact <br /> <br />The project site is situated within a highly active seismic <br />region of southern California. A total of 38 active faults have <br />been identified within an approximate 60-mile radius of the <br />project site. The NewportjInglewood Fault located approximately <br />8 miles south from the City and the Whittier Fault located 13 <br />miles northeast of the City are considered to be the most <br />dominant faults in regard to potential seismic shaking impacts. <br />A seismic event along anyone of these faults could result in a <br />7.0 magnitude earthquake. A seismic event of this scale could <br />potentially result significant damage to the proposed project. <br />However, the seismic risks at the project site would not be <br />considered to be significantly different from other areas in the <br />southern California region. Through the City's development <br />review process, the proposed project would be required to <br />prepare a site-specific geotechnical study to evaluate seismic <br />constraints and the building loads of the project and identify <br />design recommendations to minimize potential seismic shaking <br />impacts. <br /> <br />Mitigation Measure <br /> <br />. Prior to issuance of grading permits the proj ect developer <br />shall prepare and submit for approval a geotechnical report <br />that addresses seismic constraints, soil stability and <br />provides design recommendation to insure the geotechnical <br />stability of the project site. <br /> <br />A-3. Seismic-related ground failure, including liquefaction? <br /> <br />Less Than Significant Impact <br /> <br />Soil liquefaction occurs when loose soil deposits below the <br />water table are subjected to large ground accelerations <br />generated from seismic events. Liquefaction is generally known <br />to occur in saturated cohesionless soils at depths shallower <br />than about 50-feet. According to the General Plan Land Use <br />Element EIR, there is very low-to-Iow potential for liquefaction <br />impacts. <br /> <br />12 <br /> <br />32Ai~6 <br />
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