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� i <br /> File No 20-3941-01 E01 in KLEINFELL) ER <br /> August 20, 1996 <br /> The site itself is located In the western boundary of the San Joaquin Valley in an area <br /> characterized by dissected uplands Dissected uplands commonly appear along the flanks of <br /> the valley near the mountain borders They show forms characteristic of alluvial fans, but <br /> range in relief from several hundred feet to only a few feet <br /> The majority of the native sediments near the site consist of Miocene to Holocene continental <br /> rocks and deposits of a heterogeneous mixture of generally poorly sorted clay, silt, sand and <br /> gravel Some beds of claystone, siltstone, sandstone, and conglomerate are also present <br /> Currently, based on the San Joaquin County Flood Control and Water Conservation District <br /> Report for Fall 1994, the depth to groundwater at the project site area is 65 to 70 feet bsg The <br /> same report shows that the regional groundwater flow direction is towards the northwest <br /> 20-3941-01 E011MR960163 Page 6 of 21 01996, Kleinfelder,Inc <br />