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Closure Summary Report <br /> UNIVERSAL SWEEPING SERVICES <br /> 1113 Shaw Road, Stockton, California <br /> 1.0. INTRODUCTION <br /> At the request of Mr.Joe Vella,Advanced Geo Environmental,Inc. (AGE)has prepared this Closure <br /> Summary Report (CSR) for 1115 Shaw Road, Stockton, California. Based upon the results of <br /> investigations of the former underground storage tank area at the site, it is AGE's opinion that a site <br /> closure is warranted for this facility. The site setting is illustrated on Figure 1; the former <br /> underground storage tank locations and existing site structure locations are depicted on Figure 2. <br /> This CSR has been prepared in accordance with the California Regional Water Quality Control <br /> Board (RWQCB) - Central Valley Region guidelines (Tri-Regional Board Staff Recommendations <br /> For Prelirninary�Investigations and Evaluation of Underground Tank Sites) for No Further Action <br /> Requests (See Appendix A). <br /> 2.0. BACKGROUND <br /> The site is bounded on the west by Highway 99 and on the east by Shaw Road. Light industrial <br /> facilities are located north and south of the property. A single large warehouse-type structure is <br /> located on the property. <br /> Universal Sweeping Services presently occupies this property,which was formerlythe site of Bobcat <br /> Central, an equipment sales and maintenance facility. <br /> 2.1. REGIONAL GEOLOGIC/HYDROGEOLOGIC SETTING <br /> The site is situated within the southern portion of the Great Valley Geomorphic Province of <br /> California, a large, elongate, northwest trending, asymmetric structural trough; the northern and <br /> southern portions of the Province have been designated the Sacramento and San Joaquin Valleys, <br /> The Province is bordered by the Coast Ranges to the west, the Klamath Mountains and Cascade <br /> Range to the north, and the Sierra Nevada to the east. <br /> The Great Valley has been filled with sediments derived from both marine and continental sources. <br /> Thickness of the sedimentary fill ranges from thin veneers along the valley edges to more than <br /> 20,000 feet in the south central portion of the valley. The sedimentary formations range in age from <br /> Jurassic to Recent,with the older deposits being primarily marine in origin and the younger deposits <br /> being primarily continental. Continental-derived sediments were primarily deposited in lacustrine, <br /> fluvial,and alluvial environments with sediment sources being the mountain ranges surrounding the <br /> valley(Olmsted and Davis, 1961);the site itself is located on unconsolidated and semi-consolidated <br /> alluvium, lake, playa and terrace deposits of Quaternary age (California Division of Mines and <br /> Advanced Gen Environmental,Inc. <br />