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Phase II Limited Subsurface Investigation Work Plan 99 AUTO RECYCLING (De Rose Property) 430 Moffat Boulevard,Manteca California 1.0. INTRODUCTION At the request of Mr. Richard Montes,Advanced GeoEnvironmental, Inc. (AGE)has prepared the enclosed Phase II Limited Subsurface Investigation Work Plan for the property at 430 Moffat Boulevard,Manteca, California(site). The work is being performed as part of a due diligence for a property transfer. The location of the site is illustrated on Figure 1. A plan of the site is illustrated on Figure 2. This work plan was prepared as required by the San Joaquin County Environmental Health Department(EHD)for the procurement of a soil boring permit,and is in accordance with Appendix A to Tri-Regional Recommendations-Reporting,dated 30 August 1991,prepared by the California Regional Water Quality Control Board(RWQCB)for the investigation of underground storage tank (UST) sites. 2.0. BACKGROUND The site, located at 430 Moffat Boulevard in the city of Manteca, California, is situated in an area of mixed commercial and light industrial use. The site is presently utilized as a automobile "recycling" (towing) yard and/or auto dismantling facility. Several buildings are located on the facility;auto/truck parts are stored throughout the south and western portions of the site.Historically, the site was utilized as an agricultural packing facility and a city of Manteca vehicle maintenance and/or storage facility. The prominent features on the subject property are depicted in Figure 2. 2.1. REGIONAL GEOLOGIC/HYDROGEOLOGIC SETTING The site is situated within the southern portion of the Great Valley Geomorphic Province of California, a large, elongate, northwest trending, asymmetric structural trough; the northern and southern portions of the Province have been designated the Sacramento and San Joaquin Valleys, respectively.The Province is bordered by the Coast Ranges to the west,the Klamath Mountains and Cascade Range to the north, and the Sierra Nevada to the east. The Great Valley has been filled with sediments derived from both marine and continental sources. Thickness of the sedimentary fill ranges from thin veneers along the valley edges to more than 20,000 feet in the south central portion of the valley.The sedimentary formations range in age from Jurassic to Recent,with the older deposits being primarily marine in origin and the younger deposits being primarily continental. Continental-derived sediments were primarily deposited in lacustrine, fluvial,and alluvial environments with sediment sources being the mountain ranges surrounding the valley(Olmsted and Davis, 1961);the site itself is located on unconsolidated and semi-consolidated Advanced GeoEnvironmental,Inc.