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14 June 2004 <br /> AGE-NC Project No. 04-1180 <br /> Page 2 of 5 <br /> 2.3. 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 /> 1� <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).The estimated depth to ground water at the site is approximately 30 to 40 <br /> feet below surface grade based on information from surrounding sites monitored by AGE.However, <br /> this may be greatly modified by local recharge and discharge patterns. <br /> 3.0. PROCEDURES <br /> The field work reported herein was performed in accordance with procedures outlined in the <br /> AGE-prepared Limited Subsurface Investigation Work Plan, dated 25 May 2004, and approved by <br /> the San Joaquin County Environmental Health Department(SJCEHD).A boring permit and permit <br /> fee were submitted to the SJCEHD prior to implementation of field work. A copy of the approved <br /> permit is included as Appendix C. <br /> 3.1. DRILLING <br /> On 01 June 2004, two soil probe borings (P 1 and P2)were advanced at the site to collect soil and <br /> ground water samples as part of the assessment activities. Each boring was advanced to 50 feet <br /> below surface grade(bsg)using"direct push"technology,utilizing a truck-mounted Geoprobe 5400 <br /> r Advanced GeoEnvironmental,Inc. <br /> ..r <br />