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Draft Environmental Impact Report Page IV.G-8 <br /> Forward Landfill Expansion <br /> project site and these active faults would generally attenuate to minor ground shaking events at <br /> the site. Along the eastern Great Valley Margin, the less active Foothills Fault system <br /> (approximately 26 miles to the east) has a low likelihood of a major event during the project <br /> lifetime and a lower ground shaking impact to the project site. <br /> The closest known fault is the Tracy-Stockton Fault Zone passing through Stockton 6.5 miles <br /> northwest of the landfill. However, the Tracy-Stockton Fault Zone is not considered an active <br /> fault. A potential fault, referred to as the Stockton fault, is an east-west trending feature derived <br /> from oil well data projected to underlie the project site. The Stockton fault defines the northern <br /> edge of the Stockton Arch, a basement rock that divides the San Joaquin Basin on the south <br /> from the Sacramento Basin to the north. The Stockton fault is an inferred fault and considered <br /> not active. <br /> The San Andreas and associated faultsywand Ha like all known active faults in <br /> ( Calaveras etc), <br /> California (with documented historical events),fall under the State of California Alquist-Priolo <br /> Special Studies Zone Act (1972), which requires specific seismic studies to be performed prior to <br /> development, and places restrictions on certain types of development. <br /> Potential seismic impacts for the proposed expanded Forward Landfill were evaluated by <br /> GeoSyntec (JTD, 2001). The seismic analyses by GeoSyntec consisted of developing design <br /> ground motions based on the seismic hazard data in Table IV.G-1. The assessment entailed <br /> review of the impacts of potential seismic hazards on the design ground motions for the built <br /> out-landfill. <br /> The project site has no identified active faults. Available literature on the proximity of active <br /> and potentially active faults and seismic source zones within 100 miles of the project site were <br /> reviewed, and the strong ground shaking duration(D-s), and the peak horizontal ground <br /> accelerations (PHGAs) for MPE and MCE were evaluated as part of the design criteria. Table <br /> G-1 summarizes these data for the pertinent faults of the region(Abrahmson and Silva 1996, <br /> 1997;USGS/CDMG, 1996;Topposada and others, 1994)within 70 miles of the site, and presents <br /> their designated CDMG"activity" rating, distance from the project site, maximum credible <br /> earthquake magnitudes, and PHGA's (potential movement). <br /> The key determination is the identification of seismic loads that might occur at the site <br /> following regional earthquakes. The idea of such seismic analyses is to calculate the highest <br /> potential for ground shaking and ground acceleration at the landfill site from the active and <br />.. potentially faults within the 100 miles, and then to design the landfill to mitigate such events. <br /> The fault with the highest probability to generate large earthquake loads at the site, as can be <br /> seen in Table IV.G-1,is the Great Valley fault system,which is the closest potentially active fault <br /> to the landfill(approximately 21 miles southwest of the site). A MPE moment magnitude (MW) <br /> 6.4 earthquake on the Great Valley fault with its associated 11.8 seconds of duration of strong <br /> ground shaking would produce a PHGA of approximately 0.098. A MCE Mw of 6.7 on this fault <br /> with its longer duration of 15.3 seconds of strong ground shaking would generate a PHGA of <br /> approximately 0.13. Although the Great Valley fault yields the highest PHGA, the San Andreas <br /> Fault system could produce the longest duration of ground shaking. The MPE and MCE on the <br /> San Andreas show that the same M,7.9 event at a distance of 70 miles could produce a ground j <br /> shaking duration of 45.4 seconds. Given these data, Geosyntec concluded that the M,,,of 7.9 <br /> along the San Andreas Fault would produce the most damaging seismic impact to Forward <br /> Landfill. The probability of a strong (magnitude 7.0)earthquake occurring between 1990 and <br /> 2020 in the San Francisco Bay Area region is estimated at 67 percent. The probability of a major <br /> earthquake along the segment of the San Andreas Fault closest to the site is approximately 23 <br />