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Tele Analysis <br /> Soil and ground water samples were analyzed for the following <br /> constituents. <br /> • Total Petroleum Hydrocarbons (TPH) as Gasoline and Diesel <br />' (EPA Method 8015-Modified), and <br /> • Benzene, Toluene, Ethylbenzenes, and Xylenes (BTEX) (EPA <br />' Method 8020) <br /> For QA/QC purposes during the ground water sampling, trip blanks <br /> were collected and analyzed for TPH-Gasoline and BTEX. <br />' Investigation Findings <br /> The findings of the Phase I and Phase II Investigations at Site <br /> have provided information regarding the site geology and <br /> hydrogeology and have = ease a characterized the the isite. l and vertical A discussion xtent of <br /> of the <br /> the petroleum product <br />' investigation findings is provided below. <br /> The information obtained during the installation of monitoring wells <br /> and soil borings indicates that the site is underlain by clays, silts and <br /> sands. Figures 5-4 and 5-5 represent cross-sections of Former Tank <br /> Site #2, the locations of the cross-sections are provided in Figure 5-3 <br /> Fill was encountered in varying thicknesses in all of the borings. It <br /> ' occurred in the first 2-to-3 feet of MW-1A, MW-3A, MW-5A, B1-A, <br /> B2-A, and B4-A, and in the first 7 feet of MW-2A and MW-4A In <br /> general, semiconsolidated silty and clayey soils extend from beneath <br /> ' the fill to a depth of approximately 10-to-20 feet. Below the silts and <br /> clays, unconsolidated <br /> localized layers of silt and gravel are present. <br /> These sands contai <br /> During drilling, ground water was initially encountered at <br /> approximate depths ranging between 9.5 and 19 feet below the group <br /> surface. After the wells f 5 feet b s�Thereforeound erwas ground waterathe <br /> at <br /> an approximate dept g <br /> site appears to be confined. <br /> ' The potentiometric surface defined during the investigations and <br /> subsequent quarterly monitoring events suggests that the ground <br /> 5-12 <br />