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I <br /> composed of a wide variety of rock types, including granitic, metamorphic, and volcanic rocks <br /> West of the San Joaquin Valley are the Coast Ranges, which are composed of metamorphic rocks <br /> of the Franciscan Formation A structurally significant feature in the Site area is the Stockton <br /> IFault, which trends northeast-southwest and is approximately eight miles northwest of the Site <br /> The soils beneath the Site characterized during the February 1993 drilling (Wallace-Kuhl) <br /> I consisted of fine sands and silt/sand mixtures to approximately 50 feet below ground surface <br /> (bgs) Below this depth, a fine to coarse sand and silty clay are present Similar soils were <br /> reportedly observed to a depth of 15 feet bgs during removal of the USTs in 1990 <br /> 1.3 Hydrology <br /> The Site has been graded and modified to promote surface drainage Catch basins collect <br /> rainwater for flow north through underground pipes into the adjacent airport storm water system <br /> Surface drainage is to Little John Creek, a water course oriented east-west, approximately 1 5 <br /> miles north of the Site Little John Creek flows into Camp Slough and eventually into the San <br /> Joaquin River <br /> IGroundwater was encountered during drilling in February 1993 at depths ranging from 46 <br /> to 49 feet bgs Groundwater measurements made in the wells on February 24, 1993 indicated a <br /> static groundwater surface of approximately 45 feet bgs The groundwater flow direction <br /> beneath the Site on February 24, 1993 was calculated to be to the northeast with a hydraulic <br /> gradient of 0 001 feet/foot (ft/ft) <br /> The depth to groundwater in the three monitoring wells, MW1, MW2, MW3, on <br /> December 31, 1995 was 42 87, 42 87, and 42 55 feet bgs, respectively The hydraulic gradient <br /> I was calculated at 0 002 ft/ft flowing to the east-northeast The gradient is flatter than the <br /> calculated gradient for the previous quarter and the direction has changed slightly from <br /> southeasterly to east-northeasterly Versar believes this reflects seasonal fluctuations in the <br /> Igroundwater flow Groundwater elevations and gradient are included in Table 1 and shown on <br /> Figure 3 <br /> I <br /> 2 a SITE BACKGROUND <br /> The area surrounding the Site has been characterized by a mix of airport and agricultural <br /> usage for over 40 years The Site has been in existence since the early 1950s as an airplane <br /> fueling station and was expanded to its present size of approximately 25 acres in 1974 The fuel <br /> storage for the Site was originally located in three 5,000-gallon steel USTs installed in the early <br /> 1950s These USTs were removed in 1990 The USTs were oriented east-west and rested on a <br /> six-inch thick concrete slab The slab remains in place at an estimated depth of 11 feet bgs The <br /> H 1PROJECTSIDSAISTOCKTON13RD\REPORT FL 2 <br />