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M <br />" - {,y-� ;_:. -•f ..r.�r,ry - �,�" -„1 *r .'.#-'� ?' "arch .:'.;t,�� . ;.;,t �.�,".tea+_ .-� _.t?;c:•t b',+�.a, _ ?. «_. t+!...� AZ <br /> R-� <br /> SSB 91-1038 <br /> Thrifty Oil Company Siouan No.172 page 2 <br /> 7647 Pacific Avcnuc <br /> Stockton.California <br /> After surveying each well head, the ground-water gradient and flow direction were evaluated, <br /> using depth-to-ground-water measurements collected in June,1991- The field and analytical data <br /> collected during this investigation were compiled and are presented in this report. <br /> 2.0 BACKGROUND INPURNWMON <br /> Background information required to obtain an understanding of the project is presented in the <br /> following sections. <br /> 2.1 site Location <br /> The site is located at the southwest corner of the intersection of Pacific Avenue and Rivara Road <br /> in Stockton, California. Elevation at the site is approximately 13 feet above sea level. The site <br /> location is shown on the Site Vicinity Map (Plate P-1). <br /> 2.2 Site Description <br /> The site consists of a gasoline retail facility,three pump islands under a canopy,and paved traffic <br /> and parking areas. Gasoline is stored on-site in four underground storage tanks. Four ground- <br /> water monitoring wells were installed during the course of this investigation. The locations of <br /> the site facilities,including the monitoring well locations,are shown on the Site Plan (Plate P-2). <br /> 2.3 Reyionnl Genlo issettlor. <br /> Stockton is located at the border of the Sacramento and San Joaquin Valleys in the central <br /> portion of California or the center of the central valley geomorphic province of California <br /> (valley), The valley in the area of Stockton is underlain by unconsolidated Holocene <br /> continentally derived young alluvium. The younger alluviuni is underlain by unconsolidated older <br /> alluvium of Pleistocene and Holocene age. Pliocene to Pleistocene deposits of continentally <br /> derived sand, silt, clays, and poorly sorted gravels underlie older alluvial deposits. Regionally <br /> extensive clay bodies referred to as A through E clays are not believed to exist below the site. <br /> Other confining layers of less than regional extent may underlie the site. Marine sedimentary <br /> SSB ENVIRONMENTAL.CONSULTANTS,INC. <br />