Laserfiche WebLink
Phase 1I Environmental Site Assessment <br /> Multi-Modal Station <br /> Stockton,San Joaquin County,California <br /> Page 2 <br /> • Condor Identified two HRECS on the site <br /> + A cabinet, paint, and sign shops were located at 930 E Miner Avenue (248 N Aurora Street) in the <br /> 1940s through the early- to mid-1960s If historical disposal methods for paints and solvents were <br /> used on site, there is a potential risk for soil and groundwater contamination <br /> + Auto repair and auto body shops have been located at several site properties for many years <br /> Addresses of former and current auto repair and body shop businesses include 122, 204, and 210 N <br /> Grant Street, and 729, 811, 815, 829, 843, and 915 E Weber Avenue Typical wastes for these <br /> facilities include motor oil, antifreeze, brake fluid, paint, and solvents While current businesses <br /> appear to be disposing of waste materials in the proper manner, no records of how waste disposal at <br /> these businesses was conducted in the past were identified If common historical disposal methods <br /> were used on site, there is a potential risk for soil and groundwater contamination <br /> These RECs and HRECs were investigated in greater detail during the Phase II ESA Additionally, the <br /> businesses on parcels without previously identified RECs or HRECs were further reviewed to investigate <br /> past handling practices of hazardous materials and wastes <br /> The potential liability for the cleanup of hazardous substances and the available defenses to such liability <br /> are outlined in the Comprehensive Environmental Response, Compensation, and Liability Act(CERCLA) <br /> and its amendments, commonly known as the Superfund law The American Society of Testing and <br /> Materials (ASTM) states that a Phase II ESA, performed after the completion of a Phase I ESA, will help <br /> to satisfy the requirement of"all appropriate inquiry into the previous ownership and uses of the property <br /> consistent with good commercial or customary practice" [42 USC § 9601(35)(B)] and will help to provide <br /> "innocent landowner defense" (ASTM Standard E 1527-00, See 1 1) to the purchaser involved in a <br /> . commercial real estate transaction In addition, ASTM asserts that a Phase II ESA evaluates RECs "for <br /> the purpose of providing sufficient information regarding the nature and extent of contamination to assist <br /> in making informed business decisions" (ASTM Standard E 1903-97, See 1 2) including "the potential <br /> financial exposure associated with environmental risks" (ASTM Standard E 1903-97, Sec 3 1 3) It <br /> should be understood that a Phase II ESA only further investigates the site for existing or potential <br /> contamination <br /> 3.0 GENERALIZED GEOLOGIC SETTING <br /> The site is located in the middle of the San Joaquin Valley in the Great Valley Geomorphic Province The <br /> Great Valley Geomorphic Province is a northwest-trending, westward-dipping geosyncline that has been <br /> filled with up to six vertical miles of lithified marine and non-marine sediments, and unlithified non- <br /> marine sediments Geologic conditions at depth are relatively well known as a result of exploratory and <br /> production drilling for the nearby French Camp, Lathrop, and Stockton natural gas fields <br /> According to published geologic maps, surface deposits underlying the site consist of eolian sand <br /> belonging to the upper member of the Modesto Formation These sand deposits are estimated to be more <br /> than 9,000 years old and are underlain by more than 3,000 feet of Cenozoic alluvial sediment primarily <br /> consisting of Pliocene and Miocene sands and clays Regionally, the upper 3,000 feet of Great Valley <br /> alluvial sediments are resultant of erosion of the ,Sierra Nevada granitic basement rocks to the east and, to <br /> a lesser degree, the Coast Range marine and non-marine sediments and Franciscan Assemblage and <br /> granitic basement rocks to the west <br /> The unconsolidated Cenozoic alluvial sedimentary deposits are unconformably underlain by an estimated <br /> 9,000 to 10,000 feet of Upper Cretaceous marine sands and shales belonging to the Great Valley <br /> • Sequence The Upper Cretaceous sand units of the Great Valley Sequence are the primary natural gas <br /> �aC� CONDOR <br />