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31A - 3770 W. MCFADDEN AVE.
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09/06/2005
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31A - 3770 W. MCFADDEN AVE.
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Last modified
1/3/2012 4:52:49 PM
Creation date
8/31/2005 10:48:17 AM
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City Clerk
Doc Type
Agenda Packet
Item #
31A
Date
9/6/2005
Destruction Year
2010
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<br />D. Disturb any human remains, including those interred <br />outside of formal cemeteries. <br /> <br />Less Than Significant Impact <br /> <br />According to the City's General Plan Land Use Element EIR <br />there are no known cultural resources on the project site. <br />The project site is currently improved. The probability for <br />the discovery of unknown cultural resources during <br />construction operations would be low. <br /> <br />VI. GEOLOGY/SOILS <br /> <br />A-l. Rupture of a known earthquake fault, as delineated on <br />the most recent Alquist-Priolo Earthquake Fault Zoning <br />Map issued by the State geologist for the area or <br />based on other substantial evidence of a known fault? <br /> <br />No Impact <br /> <br />According to the Seismic Hazard Zone Map, the proj ect site <br />is not located within a current Alquist-Priolo Earthquake <br />Faul t Zone for fault surface rupture hazard. The surface <br />traces of any active or potentially active faults are not <br />known to pass directly through or extend towards the project <br />si te. Therefore, the potential for surface rupture due to <br />faul ting occurring beneath the site during the design life <br />of the proposed project is considered low. <br /> <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 <br />have been identified wi thin an approximate 60-mile radius <br />of the proj ect site. The Newport/Inglewood Fault located <br />approximately 13 miles south from the City of Santa Ana is <br />considered to be one of the most dominant faults in regard <br />to potential seismic shaking impacts. The project site <br />could potentially be subj ect to a maximum credible <br />horizontal ground acceleration of O. 30g from a magnitude <br />6.9 earthquake along the Newport/Inglewood fault zone. A <br />seismic event of this scale could potentially result <br />significant damage to the proposed proj ect. However, the <br />seismic risks at the proj ect site would not be considered <br />significantly different from other areas in the southern <br /> <br />8 <br /> <br />31A-32 <br />
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