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05 January 2009 <br /> AGE-NC Project No. 09-1664 <br /> Page 2 of 6 <br /> 2.2. REGIONAL GEOLOGIC/HYDROGEOLOGIC SETTING <br /> The site is situated within the southern portion of the Great Valley Geomorphic Province of <br /> California, a large, elongate, northwest trending, asymmetric structural trough; the northern and <br /> southern portions of the Province have been designated the Sacramento and San Joaquin Valleys, <br /> respectively.The Province is bordered by the Coast Ranges to the west,the Klamath Mountains and <br /> Cascade Range to the north, and the Sierra Nevada to the east. <br /> The Great Valley has been filled with sediments derived from both marine and continental sources. <br /> Thickness of the sedimentary fill ranges from thin veneers along the valley edges to more than <br /> 20,000 feet in the south central portion of the valley.The sedimentary formations range in age from <br /> Jurassic to Recent,with the older deposits being primarily marine in origin and the younger deposits <br /> being primarily continental.Continental-derived sediments were primarily deposited in lacustrine, <br /> fluvial,and alluvial environments with sediment sources being the mountain ranges surrounding the <br /> valley(Olmsted and Davis, 1961);the site itself is located on unconsolidated and semi-consolidated <br /> alluvium, lake, playa, and terrace deposits of Quaternary age (California Division of Mines and <br /> Geology, 1977).Rocks composing the basement complex of the Province have not been completely <br /> defined but are believed to be metamorphic and igneous in origin. <br /> The Modesto, Riverbank, and Turlock Lake Formations and overlying Recent alluvium are the <br /> principal sources of domestic ground water in the 13,500-square mile San Joaquin Valley Ground <br /> Water Basin(Basin 5-22). <br /> 2.3. GROUND WATER DEPTH AND FLOW DIRECTION <br /> Based on data obtained from a nearby site (800 Main Street, Stockton, California) the depth to <br /> ground water at the site is approximately 30 to 35 feet bsg. The prevailing ground water flow <br /> direction in the vicinity of the site is estimated to be toward the east-northeast. However, flow <br /> direction may be both locally and seasonably variable. <br /> 3.0. SCOPE OF WORK <br /> The analytical results from the UST removal soil samples indicate that an unauthorized release of <br /> petroleum hydrocarbon compounds from the former UST has occurred at the site.AGE proposes to <br /> advance twos &borings to collect soil and an in-situ grab ground water sample to assess the extent <br /> of petroleum hydrocarbon impact to soil and ground water beneath the site. The preliminary site <br /> assessment will consist of the following tasks: <br /> .Wraad Ge EavirowealaL rac <br />