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Site Background Information <br /> VANCO TRUCK&AU­0 PLAZA <br /> 1033 West Charter Way, Stockton, Callfornia <br /> BACKGROUND <br /> The site is situated in an area of mixed commercial and fight industrial use, bordered by <br /> Navy Drive on the north and West Charter Way on the south. The prominent features of <br /> the subject property are depicted on Figure 2. <br /> REGIONAL GEOLOGIC 1 HYDROGEOLOGIC SETTING <br /> The site is situated within the southern portion of the Great Valley Geomorphic Province <br /> of Califomia;.a large, elongate, northwest trending, asymmetric structural trough; the <br /> northern and southern portions of the Province have been designated the Sacramento and <br /> San Joaquin Valleys, respectively. The Province is lbordered by the Coast Ranges to the. <br /> west,.the Klamath Mountains and Cascade Range to the north, and the Sierra Nevada to <br /> the east:: <br /> The Great%Valley has been filled with sediments de bed from both marine and continental <br /> sources.Thickness of the sedimentary fill ranges from thin veneers along the valley edges <br /> to more than 20,000 feet in the south central portion of,the valley. The sedimentary <br /> formations range in age from Jurassic to Recent;with the older,deposits being primarily <br /> marine in origin and the younger deposits,continen I.Continental-derived sediments were <br /> typically deposited in lacustrine, fluvial, and alluvia environments with sediment,sources <br /> being the mountain ranges surrounding the valley( Imsted and Davis, 1961);the site itself <br /> is located on unconsolidated-and semi-consolida ed alluvium, lake, playa, and terrace <br /> deposits of-,Quaternary age (California Division .f Mines and Geology, 1977). Rocks <br /> composing the basement complex of the Province iave not-been completely defined, but <br /> are believed to be metamorphic and igneous in origin. <br /> The Modesto, Riverbank,and Turlock Lake Format ons and overlying Recent alluvium are <br /> the principal sources of domestic ground water in the 13,500-square mile San Joaquin <br /> Valley Ground Water Basin (Basin 5-22). The c epth to ground water at,the site is <br /> approximately.20 feet to 25 feet,below surface gr ade (bsg) based on information from <br /> quarterly monitoring events performed by AGE at, he site; the ground water elevation is <br /> approximately 10 feet-below mean sea level (MSL). Ground water generally flows toward <br /> the northeast; however, this may vary due to local recharge and discharge patterns. <br /> FUEL-DISPENSING SYSTEM UPGRADE <br /> In February 2003, as part of a fuel-dispensing system upgrade, the underground storage <br /> tank (UST) sumps, fuel dispensers, and associated piping were excavated by the Fillner <br /> Advanced GeoEnvironmental,inc. <br />