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MITIGATION: <br /> Proposed by Project <br /> Most of the soil disturbed by the project will eventually be <br /> stabilized by the placement of pavement, construction of buildings or <br /> revegetation for landscaping. <br /> Although erosion hazard at the site ranges from slight to none, <br /> standard best management practices to control erosion will be <br /> implemented as needed. This includes scheduling and limiting the extent <br /> of clearing, grading and trenching so as to assure that disturbed soils <br /> are stabilized prior to October 15 for each phase of construction. <br /> Topsoil will be scalped from construction pads and roads and <br /> stockpiled for later use on lawn and landscaping areas. <br /> A complete soils report will be required to be submitted to the <br /> City prior to issuance of any construction permits. <br /> GEOLOGY AND SEISMICITY <br /> EXISTING: <br /> The site is located in the center of the Great (Central) Valley of <br /> California. Geologic literature indicates as much as several thousand <br /> feet of flat-lying sedimentary rock strata underlie the site. The most <br /> recent sediments (soil ) were deposited during flood stages between <br /> natural levees associated with nearby streams and rivers. No unique <br /> geologic features have been identified at the site [5]. <br /> No- known active or inactive faults occur on or underlie the site. <br /> The inactive Stockton Fault, however, passes within approximately three <br /> miles of the site. This fault has been detected in the subsurface in <br /> deep wells associated with oil and gas exploration, but nowhere has it <br /> been observed at ground surface. The nearest known active fault is the <br /> Midway Fault, located 20 miles west of the site. The (active) Antioch <br /> Fault is located 25 miles west of the site [5]. <br /> No primary effects from a seismic event such as surface ruptures on <br /> an active fault are expected at the site. Ground shaking, a secondary <br /> effect of a seismic event, however may occur periodically. It is very <br /> unlikely that bedrock accelerations in excess of 0.25 g will be <br /> generated at the site by nearby active faults and resulting earthquakes. <br /> Therefore, damage resulting from primary and secondary effects of <br /> seismic events should be negligible, especially if structures are built <br /> in accordance with current Uniform Building Code regulations [5]. <br /> MITIGATION: <br /> No potential , significant, geologic or seismic impacts have been <br /> identified. This assumes that future structures are built in accordance <br /> with the current Uniform Building Code. No other mitigation is deemed <br /> necessary. <br /> 31 <br />