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Phase I Environmental Site Assessment Project d 99-1261 Proposed AutoZone Site.Manteca,Calitornia February 19. 1999 Page 4 i Limiting Conditions and Methodology Used The methodology employed during this investigation is in general accordance with the methodology outlined in the ASTM Designation: E 1527, and includes: a review of readily available records; site reconnaissance, interviews with local government officials; and evaluation of data and report preparation. I11. SITE DESCRIPTION Location The subject site is located on the western side of South Main Street on the northern half of the parcel currently occupied by Dons Mobil Glass. Dons Mobil Glass is located at 151 South Main Street in the City of Manteca. County of San Joaquin, i California. The subject site,which is owned by Value Reclamation Corporation,has i been assigned assessors parcel number of 219-410-11 (see Figure Ia, Vicinity Map). I Site Vicinity The subject site is bounded by South Main Street to the east, Firestone Tires - Los Amigas Tire Service(123 South Main Street) to the north, Maple Street to the east, and Don's Mobile Glass (151 South Main Street) to the south (see Figure No. Ic, Site Map). To the east, directly across Main Street from the subject site is the Save $ Market (grocery store) and the parking lot for Bank of America and to the west, directly across Maple Street from the site, is a Public Parking Lot. Generally, the subject property is a rectangular shaped parcel of approximately 1.24 acres located within a light commercial / industrial area of the City of Manteca. Residential properties are located in the areas to both the west and east of the subject site. Geologic Setting Regional geologic maps of the area(CDMG, 1990), indicate that the subject site is located in an area underlain by Quaternary(Holocene)-aged dune sand deposits. The site is located approximately 15.6 miles from the Coastal Ranges-Sierran Block Fault Zone(San Joaquin Fault); and 25 miles from the Greenville Fault Zone. These fault zones are reported to have shown indications of Late Quaternary seismic activity. Our review of the proper literature (Hart, E. W. 1994, CDMG, 199 1) indicates that the subject site lies outside the present Earthquake Fault Zones, which are described in the Alquist-Priolo Earthquake Fault Zoning Act as being placed along active faults. i