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' k4KLEINFELDER <br /> I - <br /> 2 SITE SETTING <br /> 2.1 SITE LOCATION <br /> The site is located in Section 5, of Township 2 North, Range 6 East of the Mount Diablo Baseline <br /> and Meridian According to the 1976 photorevised U S Geological Survey "Stockton West, <br /> California, 7 5-Minute Topographic Quadrangle Map, the property has an elevation of <br /> approximately 10 feet above mean sea level <br /> The site is in the southern portion of San Joaquin County Assessor's Parcel Number (APN) 139- <br /> 090-08 <br /> 2.2 CURRENT SITE USE AND VICINITY CHARACTERISTICS <br /> The project site is currently vacant industrial and commercial land The site is bordered to the <br /> north by vacant land along the site north, central and northwestern boundary The eastern boundary <br /> is adjacent to an ARCO retail service station The ARCO east site boundary is adjacent to North <br /> Center Street The west and south boundaries are adjacent to the Stockton Deep Water Channel <br /> The site general vicinity is characterized by mixed use, retail, light commercial, industrial, <br /> professional offices, and residential property <br /> 2.3 GEOLOGY AND HYDROGEOLOGY <br /> The site lies within the Great Valley Geomorphic Province of California The valley is <br /> approximately 400 miles long and averages about 50 miles wide, and comprises about 20,000 <br /> 1 square miles The valley has been filled with a thick sequence of marine and non-marine <br /> sediments from the late lurassic to Holocene The uppermost strata of the Great Valley <br /> represents, for the most part, the alluvial, flood, and delta plains of two major rivers (Sacramento <br /> 1 and San Joaquin Rivers) and their tributaries <br /> The valley deposits are derived from the Coast Ranges to the west and the Sierra Nevada to the <br /> ' east Granitic and metamorphic rocks outcrop along the eastern and southeastern flanks of the <br /> valley Marine sedimentary rocks outcrop along most of the western, southwestern, southern, <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 continentai rocks and deposits of a <br /> 20-1129-30/2017R3 14 Page 3 of 13 <br /> 0 1997, KleinfeldLr Ino July 14, 1997 <br />