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KI_ EINFEI_ DER <br /> lFile No 20-1008-52 A03 <br /> July 6, 1994 <br /> SITE SETTING <br />' 2.1 SITE LOCATION <br /> The San Joaquin County Motor Pool is located at 444 South Wilson Way in Stockton, <br />' California The motor pool is bound on three sides by Wilson Way, Sonoma Street and Della <br /> Street Eugenia Street enters onto the property and is the main avenue of access to the site <br /> A site plan is attached <br /> The San Joaquin County Motor Pool is hereafter referred to as the "project site " The project <br /> site is located in Township 1, North, Range 6 East, Northeast Quadrant of the Mount Diablo <br /> Baseline and Meridian According to a 1968 Stockton West Quadrangle Map (photo-revised <br /> in 1987), the area surrounding the site includes commercial buildings and residential area <br /> 2.2 SITE DESCRIPTION <br /> The site currently consists of welding, auto repair, and tire shops, office space and associated <br />' parking The property is enclosed by a fence There is no well on site, however, there are <br /> municipal wells within one-half mile of the site <br /> 2.3 GEOLOGY AND HYDROGEOLOGY <br /> The site lies in the Great Valley Geomorphic Province of California The valley is about 400 <br /> miles long (north-south), averages about 50 miles wide (east-west), and comprises <br /> approximately 20,000 square miles The valley has been filled with a thick sequence of <br /> marine and non-marine sediments from the late Jurrassnc to the Holocene tines The <br /> uppermost strata of the Great Valley represents, for the most part, the alluvial, flood, and <br /> delta plains of two major rivers (Sacramento and San Joaquin Rivers) and their tributaries <br /> The valley geomorphology includes dissected uplands, low alluvial plains and fans, river <br /> flood plains and channels, and overflow lands and lake bottoms <br />' The site is located on the dissected uplands and low alluvial plains of the northern portion <br /> of the San Joaquin Valley of the Great Central Valley The San Joaquin Valley is <br /> characterized by deep accumulations of Cretaceous and Quaternary Age sediments and include <br /> both marine and continental rocks and deposits <br /> Copyright 1994 Kleinfelder Inc Page 4 of 11 <br />