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City of Santa Ana Emergency Operations Plan <br />Part I Basic Plan <br />In addition to the major faults described above, rupture of a number of smaller faults could potentially impact <br />Orange County, including the Norwalk Fault (located in the north of the county in the Fullerton area), the El <br />Modena Fault (located in the City of Orange area), and the Peralta Hills Fault (in the Anaheim Hills area). <br />Undiscovered blind faults may also emerge at any time. <br />Addressing the Earthquake Hazard <br />In California, many agencies are focused on seismic safety issues: the State's Seismic Safety Commission, the <br />Applied Technology Council, California Office of Emergency Services, United States Geological Survey, Cal <br />Tech, the California Geological Survey, as well as a number of universities and private foundations. These <br />organizations, in partnership with other state and federal agencies, have undertaken a rigorous program in <br />California to identify seismic hazards and risks including active fault identification, bedrock shaking, tsunami <br />inundation zones, ground motion amplification, liquefaction, and earthquake -induced landslides. Seismic hazard <br />maps have been published and are available for many communities in California through the State Division of <br />Mines and Geology. <br />In California, each earthquake is followed by revisions and improvements to Building Codes. The 1933 Long <br />Beach Earthquake resulted in the first seismic safety standards in building codes, including the Field Act requiring <br />earthquake -resistant school construction. The 1971 Sylmar (or San Fernando) earthquake brought another set of <br />increased structural standards. Similar re-evaluations occurred after the 1989 Loma Prieta and 1994 Northridge <br />earthquakes. These code changes have resulted in stronger and more earthquake resistant structures. <br />The Alquist-Priolo Earthquake Fault Zoning Act was passed in 1972 to mitigate the hazard of surface faulting to <br />structures for human occupancy. This state law was a direct result of the 1971 Sylmar Earthquake, which was <br />associated with extensive surface fault ruptures that damaged numerous homes, hospitals, commercial buildings, <br />and other structures. Surface rupture is the most easily avoided seismic hazard and this Act prohibits construction <br />atop earthquake faults. <br />The Seismic Hazards Mapping Act, passed in 1990, addresses non -surface fault rupture earthquake hazards, <br />including liquefaction and seismically induced landslides. The State Department of Conservation operates the <br />Seismic Mapping Program for California. Extensive information is available at their website: <br />http://gmw.consrv.ca. ovg /shmp/index.htm. <br />51 <br />