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k'g KLEINFELDER The site is bounded to the north by Yosemite Avenue, to the south by California State Highway 120 Bypass, to the west by Powers Avenue and residential development and to the east by California State Highway 99. The land use in the site vicinity is characterized as mixed use, retail, light commercial, agricultural and residential property. 2.3 GEOLOGY AND HYDROGEOLOGY The site lies within the Great Valley Geomorphic Province of California. The valley is approximately 400 miles lons! and avera-es about 50 miles wide,-and comprises about 20,000 square miles. The valley has been filled with a thiel: sequence of marine and non-marine sediments from the late Jurassic to Holocene. The uppermost strata of the Great Valley represents, for the most part. the alluvial. flood, and delta plains of two major rivers (Sacramento and San Joaquin Rivers)and their tributaries. The valley deposits are derived from the Coast Ranges to the west and the Sierra Nevada to the east. 'Granitic and metamorphic rocks outcrop along the eastern and southeastern Flanks of the valley. Marine sedinientary rocks outcrop along most of the western, southwestern, southern, and southeastern flanks: and volcanic rocks and deposits outcrop along the northeastern flanks of the valley. The valley �_eornorhhologN• includes dissected uplands. low alluvial plains and fans. river flood plains and channels. and ovcrflow lands and lake bottom~. Site specific geologic information was obtained from two documents prepared for Spreckels Sugar by Kenneth D. Schmidt. Groundwater Quality Consultant (Schmidt 1985 and Schmidt 1993). The documents are technical reports oil groundwater monitoring efforts associated with the wastewater, lime and mud Bonds On site. According to Mr. Schmidt; coarse-grained alluvial deposits, primarily tine to.medium graiined sand, are present to a depth of at least 60 feet below grade. Localized clay strata are also present in the upper 60 feet. Additionally, two major clay layers are present beneath the site at approximate depths of 95 to 141 feet, and 188 to 243 feet. Mr. Schmidt (dentilies the deeper clay layer (188 to 243 feet) as the Corcoran Clay, a major regional confining bed that occurs alrnng the west side of the Satz Joaquin Valley. Mr. Schmidt indicates that several major _ravel deposits occur at depths of 40 to 65 feet, 110 to 130 feet. and 300 to 340 feet below the site. The deepest gravel layer is reportedly the aquifer tapped by the factory water supply wells. 20-397H-03A13W201()766 Pa,w-1 W'20 ©1999.Klcinrcldcr. Inc. 5cptember9. 1999