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F <br /> Site Background Information <br /> ENTERPRISE INVESTMENTS (Former J.B. Murphy Trucking) <br /> 355 Enterprise PIace, Tracy, California <br /> SITE LOCATION AND DESCRIPTION ' <br /> The site is located in a commercial/industrial area of north Tracy, California, at an estimated <br /> elevation of 5 feet above mean sea level. The site is presently occupied by Jimco Construction and <br /> Rerailing. The site is located on the north side of Enterprise Place. The major portion of the site <br /> consists of an unpaved dirt area used as a parking lot for trucks(Figure 2).A two-story office facility <br /> and truck garage are presently located on the site. <br /> ' REGIONAL GEOLOGIC SETTING <br /> '. . The site is located within the northern San Joaquin Valley which comprises part of the Great Valley <br /> geomorphic province of California. The San Joaquin Valley is formed by the Great Valley <br /> geosyncline,which is a large, elongate,northwest-trending asymmetrical structural trough(basin). <br /> It is bordered by the Coast Ranges to the west, the Klamath Mountains and Cascade Range to the <br /> north, and the Sierra Nevada to the east. This trough has been filled with sediments derived from <br /> both marine and continental sources. Thickness of the sedimentary fill ranges from thin veneers <br /> along the valley edges to more than 20,000 feet in the south central portion of the valley. The <br /> I` sedimentary formations range in age with the older deposits being primarily marine in origin and the <br /> younger deposits being primarily continental. Continental-derived sediments were primarily <br /> deposited in lacustrine,fluvial,and alluvial environments with sediment sources being the mountain, <br /> ranges surrounding the valley(Olmsted and Davis, 1961).The site is located on unconsolidated and <br /> -.., semi-consolidated alluvium,lake,playa and terrace deposits of Quaternary age(California Division <br /> of Mines and Geology, 1977).The Modesto,Riverbank and Turlock Lake Formations and overlying <br /> Recent alluvium are the principal sources of domestic ground water in the 13,500-square mile San <br /> Joaquin Valley Ground Water Basin(Basin 5-22). <br /> STRATIGRAPHY <br /> Generally, gray to brown, damp to saturated, silty clay was encountered from surface grade to <br /> approximately 15 to 20 feet bsg and 25 to 30 feet bsg. Discontinuous intervals of brown, saturated <br /> sandy silt of varying thickness was encountered at 15 to 20 feet bsg and 30 to 35 feet bsg. Pea gravel <br /> was encountered in the former UST pit at 5 feet and 10 feet bsg, presumably imported back-fill <br /> material <br /> UNDERGROUND STORAGE TANK REMOVAL <br /> On 12 August 1997, one 10,000-gallon diesel UST was removed from the site by Stockton Service <br /> Advanced Geo)Environmental,Inc. <br />