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4.Emironmemal Analysis _ <br /> ground acceleration produced during an earthquake can cause displacements in the soil. These <br /> displacements can decrease the soil strength and trigger down slope movement. <br /> Ground Motion and Slope Instability — <br /> Evaluation of slope stability in a region requires knowledge of conditions under which <br /> earthquake-induced landslides have occurred in the past. A magnitude 4.0 earthquake is relatively _ <br /> common in California,with light to moderate perceived shaking that causes either no or very light <br /> damage. As discussed in the setting above,the proposed project site could experience ground <br /> shaking up to a Modified Mercalli intensity of MM-VIII, which is an earthquake that everyone — <br /> would feel and one that could cause moderate to severe structural damage depending on location, <br /> age of structure,and construction. The estimated PGA could reach 0.4 g according to the regional <br /> probabilistic seismic hazard assessment completed by the California Geological Survey(CGS, <br /> 2003a). The Tracy-Vernalis area could be affected by earthquakes occurring in the Bay Area and <br /> the San Joaquin Valley and be subjected to earthquake magnitudes capable of causing failure in <br /> non-engineered, unsupported slopes or permanent reclamation slopes. <br /> Slope Stability Analysis for Proposed Project Site _ <br /> Geomatrix conducted a preliminary analysis to assess the stability of the temporary 3/4:1 (H:V) <br /> and permanent 2:1 (H:V)quarry slopes expected at the proposed project site. The preliminary <br /> stability analysis addressed slope stability under static and earthquake-induced conditions <br /> (Geomatrix, 2002), which was based on applicable,available subsurface information, laboratory <br /> analysis of a clay sample from the DSS Quarry site, and postulated seismic loadings.The 2005 _ <br /> Kleinfelder,Inc. study conducted a subsequent slope stability evaluation, which included a site- <br /> specific field investigation of the subsurface materials and static and pseudo-static(earthquake <br /> motion) slope stability computer modeling. _ <br /> Slope Configuration Requirements <br /> As presented in the Regulatory Framework section of this chapter, Chapter 9-1415.3 of the San <br /> Joaquin County Development Title,Ordinance for Quarry Excavations(Title) require that <br /> temporary cut slopes not exceed 1:1 (H:V) although temporary slopes at setback lines can be _ <br /> maintained at 1/2:1 (H:V) if geologic and engineering analysis determine that the slopes will have <br /> a minimum factor of safety of 1.5 against static deep-seated and near surface slope failure and a <br /> minimum factor of safety of 1.1 against seismic failure. Permanent slopes are required by the _ <br /> Title not to exceed 2:1 (H:V)but can be maintained at 1.5:1 (H:V) if slope stability analysis <br /> demonstrates that the slope would have the minimum required factor of safety(as above, 1.5 <br /> under static conditions and 1.1 under seismic conditions). Permanent 2:1 (H:V) slopes exceeding — <br /> 50 feet in height are required by the Title to be terraced with a maximum vertical distance <br /> between terraces of 50 feet. Terraces must be 12 feet wide and have appropriate drainage. <br /> Results of Slope Stability Analysis <br /> Based upon the findings of the 2005 slope stability evaluations and experience at other nearby — <br /> quarries with similar geology, Kleinfelder, Inc. concluded that the proposed 3/4:1 (H:V)temporary <br /> RMC Pacific Vernalis Quarry Mining and Reclamation Project 4.7-18 ESA 1203015 <br /> Draft Environmental Impact Report May 2006 <br />