Laserfiche WebLink
i1 r <br /> i <br /> ' Site Conceptual Model <br /> LATHROP GAS AND FOOD MART <br /> ' 14800 South Highway 99,Manteca,California <br /> 1.0. INTRODUCTION <br /> Advanced GeoEnvironmental, Inc (AGE) has prepared this Site Conceptual Model (SCM) for <br /> ' Lathrop Gas and Food Mart,located at 14800 South Highway 99,Manteca,California(the site) The <br /> purposes of the SCM are to 1) identify the source(s)of contamination, 2)determine the nature and <br /> the extent of the contamination,3)identify the dominant fate and transport characteristics of the site, <br /> ' 4)specify potential exposure pathways, and 5) identify potential receptors that may be impacted by <br /> the contamination The site setting is illustrated on Figure 1 Site structures, soil borings, and <br /> monitoring well locations are depicted on Figure 2 <br /> This SCM has been prepared utilizing existing data collected during previous site subsurface <br /> , <br /> investigations, and includes a discussion of site background and a summary of previous subsurface <br /> ' investigations This model has been prepared in accordance with guidelines issued by the California <br /> Regional Water Quality Control Board- Central Valley Region(CVRWQCB)for the investigation <br /> of underground storage tank (UST) sites <br /> • 2.0, BACKGROUND <br /> The site is located at 14800 South Highway 99, Manteca, California, and is situated in an area of <br /> mixed commercial and agricultural use The site is bordered on the east by Highway 99,on the west <br /> by Highway 99 Frontage Road, on the north by the Lathrop Road off-ramp, and on the south by <br /> Lathrop Road Prominent features on the subject property are depicted on Figure 2 <br /> 1 <br /> 21 REGIONAL GEOLOGIC/HYDROGEOLOGIC SETTING <br /> According to Geologic Map of California, published in 1966 by the California Department of <br /> Conservation Division of Mines and Geology, the site area is shown to be within the Great Valley <br /> Geomorphic Province(GVGP)of California,a large,elongate,northwest-trending structural trough <br /> The GVGP is subdivided into two major divisions, designated the Sacramento and San Joaquin <br /> Valleys, which have been filled to the present elevation with thick sequences of sediment derived <br /> ' from 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 /> sedimentary formations vary in age from Jurassic to Recent,with the older deposits being primarily <br /> ' marine in origin and the younger deposits continental Continental-derived sediments were typically ` <br /> deposited in lacustrine,fluvial,and alluvial environments with sediment sources being the mountain <br /> ' ranges surrounding the valley(Olmsted and Davis, 196 1) 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) Rocks composing the basement complex of the province have not <br /> 01' Advanced GeoEnvironmental,Inc <br /> 1 <br />