ARCHIVED REPORTS_XR0003259 - Laserfiche WebLink

Home Browse Search

' Closure Summar.y Report 2003 VAN BUSKIRK GOLF COURSE FACILITY- ' 1740 Houston Avenue, Stockton, California ' 1.0. INTRODUCTION At the request of the City of Stockton,Advanced.GeoEnvironmental, Inc. (AGE) has'prepared this closure summary report for the Van Buskirk Golf Course maintenance facility(site)located at 1740 Houston Avenue, Stockton, California (Figure 1). The work included collection of ground water samples from two soil borings to assess the impact of petroleum hydrocarbons and fuel oxygenating ' compounds on ground water beneath the site. This report is prepared in accordance with guidelines established in Appendix A and Appendix B to ' Tri-Regional Recommendations-Reporting, dated 30 August 1991,prepared by the Central Valley Regional Water Quality Control Board (CVRWQCB) for the investigation of UST sites. Site background infonnation'was summarized in'the AGE-prepared-Additional Soil and Ground Water ' Assessment Work Plan, dated 31 July 2000, which was approved by the San Joaquin County Environmental Health Department(EHD)by letter dated 04 August 2000. 1 The.Van Buskirk Golf Course is located at 1.740 Houston Avenue,Stockton, California(Figure 1). The golf course is located in the incorporated City of Stockton.The golf course is situated along the ' south side of Houston Avenue and is bound on the east by Interstate 5, Walker Slough to the south, and open-space to the west. The maintenance facility site is located on the south central portion of the golf course. maintenance facility . The e ance ac rty s>te consists of a maintenance shop structure, storage shed, and.open storage area(Figure 2).In addition;the facility formerly operated two fuel USTs and fuel dispensers. ' The USTs formerly located at the'site consisted.of a 550-gallon gasoline tank and a 1,000-gallon diesel tank. 2.0. REGIONAL GEOLOGIC/HYDROGEOLOGIC SETTING ' The property is situated within the Great Valley Geomorphic Province of California, a large, elongate, northwest trending, asymmetric structural trough. The Great,Valley Province has been filled with thick sequences of sediment ranging in age from Jurassic to Recent,creating a nearly flat- lying alluvial plain,extending from the Tehachapi Mountains in the south to the Klamath Mountains in the north. The western and eastern bouridaries'of this province are the California Coast Range and ' the Sierra Nevada, respectively. Rocks composing the basement complex of the province have not been completely defined but.are'believed to-be of metamorphic and igneous origins. The northern and southern portions of the Great Valley Province have been designated the Sacramento and San ' Joaquin Valleys, respectively. Advanced GeoEnviranmental,Inc.