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' 20 March 2002 <br /> • AGE-NC Project No 01-0877 <br /> Page 2 of 7 <br />' at a concentration of 3,900 mg/kg Soil samples collected beneath the fuel USTs and dispensers were <br /> not analyzed for TPH-d, TPH-mo and Oil and Grease <br />' Toluene was detected in all UST and dispenser samples at concentrations as high as 99 mg/kg <br /> (T3-E) Ethylbenzene and total xylenes were detected in the soil samples collected beneath the USTs <br /> at concentrations as high 200 mg/kg and 1,100 mg/kg, respectively <br /> Total Iead was detected in all of the soil samples at concentrations as high as 39 mg/kg Chromium, <br /> nickel and zinc were detected in the soil samples collected beneath the waste oil UST, fill location <br />' and the stockpile at concentrations as high as 40 mg/kg, 34 mg/kg and 330 mg/kg, respectively <br /> Metal concentrations are not outside the background, natural range of metals concentrations in <br /> California soils Hexavalent chromium and PCB's were not detected at or above laboratory reporting <br /> limits in the soil samples analyzed <br /> 2 2 REGIONAL GEOLOGIC/HYDROGEOLOGIC SETTING <br />' The site is located within the southern San Joaquin Valley which comprises part of the Great Valley <br /> geomorphic province of California The San Joaquin Valley is formed by the Great Valley <br /> geosyncline, which is a large, elongate, northwest-trending asymmetrical structural trough (basin) <br /> I It is bordered by the Coast Ranges to the west, the Klamath Mountains and Cascade Range to the <br /> north, and the Sierra Nevada to the east This trough has been filled with sediments derived from <br /> both marine and continental sources Thickness of the sedimentary fill ranges from thin veneers <br /> along the valley edges to more than 20,000 feet in the south central portion of the valley The <br /> sedimentary formations range in age with the older deposits being primarily marine in origin and the <br /> younger deposits being primarily continental Continental-derived sediments were primarily <br /> deposited in lacustrine,fluvial,and alluvial environments with sediment sources being the mountain <br /> ranges surrounding the valley(Olmsted and Davis, 196 1) The site is located on unconsolidated and <br /> semi-consolidated alluvium,lake,playa and terrace deposits of Quaternary age(California Division <br />' of Mines and Geology, 1977) <br /> The Modesto, Riverbank and Turlock Lake Formations and overlying Recent alluvium are the <br /> principal sources of domestic ground water in the 13,500-square mile San Joaquin Valley Ground <br /> Water Basin (Basin 5-22) <br /> 2 3 GROUND WATER DEPTH AND FLOW DIRECTION <br /> Based on information obtained during drilling,ground water depth beneath the site is approximately, <br /> 25 to 30 feet below surface grade(bsg) Based on information obtained from a nearby site(706 North <br /> Advanced GeoEnvi ron mental,Inc <br /> r <br />