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i • <br /> 12 March 2001 <br /> AGE-NC Project No 97-0333 <br /> Page 3 of 8 <br /> samples collected from MW-1, MW-2 and MW-3 at concentrations ranging as high as 110 <br /> mg/kg No other fuel components were detected by laboratory analysts Results of the June <br /> 2000 investigation were reported in Quarterly Report - Third Quarter 2000 dated 20 <br /> September 2000 prepared by AGE <br /> • 11 July 2040-Initial ground water monitoring and sampling were performed at wells MW-1, <br /> MW-2, MW-3, MW-4 and MW-5 Ground water levels were measured between 15 and 16 <br /> feet below the tops of the well casings, ground water flow direction at the site was inferred <br /> to be flowing towards the north at an approximate gradient of 0 001 Laboratory analysis of <br /> ground water samples at the site detected TPH-g at concentrations as high as 140,000 <br /> micrograms per liter (ug/1), BTEX compounds were detected at concentrations as high as <br /> 28,000µg/1, MTBE and TAME were detected at concentrations as high as 980,000 ugll No <br /> other petroleum hydrocarbon constituents or fuel oxygenated compounds were detected <br /> Results of the July 2000 investigation were reported in Quarterly Report - Third Quarter <br /> 2440 dated 20 September 2000 prepared by AGE <br /> C August and September 2000- AGE conducted a sensitive receptor survey to locate potential <br /> vertical conduits within a 2,000 foot radius of the site The results of the sensitive receptor <br /> . survey located a municipal water well (City of Manteca Well No 4) located approximately <br /> 1,900 feet northwest of the site near and a second municipal water well (City of Manteca <br /> Well No 5) located approximately 1,500 feet south of the site Results of the investigation <br /> were reported to Sensitive Receptor Survey dated 08 September 2000 prepared by AGE <br /> C 11 October 2000- Ground water monitonng and sampling were performed at wells MW-1, <br /> MW-2, MW-3, MW-4 and MW-5 Ground water levels were measured between 16 and 17 <br /> feet below the tops of the well casings, ground water flow direction at the site was inferred <br /> to be flowing towards the northeast at an approximate gradient of 0 001 Laboratory analysis <br /> of ground water samples detected TPII-g at the site at concentrations as high as 140,000 gg/l, <br /> BTEX compounds were detected at concentrations as high as 28,000 ug/l, MTBE and TAME <br /> were detected at concentrations as high as 980,000 ug/l No other petroleum hydrocarbon <br /> constituents or fuel oxygenated compounds were detected during the laboratory analysis <br /> Results of the July 2000 investigation were reported in Quarterly Report - Foulth Quarter <br /> 2000 dated 11 October 2000 prepared by AGE <br /> 24 REGIONAL GEOLOGIC SETTING <br /> The property is situated within the Great Valley Geomorphic Province of California, a large, <br /> clongatc, northwest trending, asymmetne structural trough The Great Valley Province has been <br /> filled with thick sequences of sediment ranging in age from Jurassic to Recent, creating anearly flat- <br /> lying alluvial plain, extending from the Tehachapi ;Mountains in the south to the Klarnath Mountains <br />