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m KLEINFELDER <br />and southeastern flanks; and volcanic rocks and deposits outcrop along the northeastern flanks of <br />the valley. The valley geomorphology includes dissected uplands, low alluvial plains and fans, <br />river flood plains and channels, and overflow lands and lake bottoms. The majority of the native <br />sediments near the site consist of Miocene to Holocene continental rocks and deposits of a <br />heterogeneous mixture of generally poorly sorted clay, silt, sand and gravel. <br />Based upon the San Joaquin County Flood Control and Water Conservation District <br />(SJCFC/WCD), Spring 1999 Groundwater Report, groundwater in the vicinity of the site is <br />anticipated at approximately 65 feet bgs. The regional direction of groundwater flow has not <br />been calculated at this time, however based on the SJCFC/WCD report we anticipate the <br />groundwater to flow towards the north. <br />24134.E01 / ST03R304 Page 3 of 10 <br />Copyright 2003, Kleinfelder, Inc. February 26, 2003