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KLE/NFELOER <br /> MgM1t Rnpk.fligM1tSOWfiam. <br /> ' The following information was obtained from a report dated September 18, 2001 titled <br /> "Additional Information For The Report Of Waste Discharge" by Bonneau Dickson of <br /> Berkley, California. <br /> Potable water for the CNP plant is obtained from the City of Lathrop water system. The <br /> CNP plant uses the water in the manufacturing of the following: <br /> ♦ rice milk ♦ soy milk <br /> ♦ flavored teas ♦ cream soups <br /> Wastewater is generated throughout the plant primarily from wet mill maceration of <br /> vegetables, surface spillage, clean in place solution, and evaporates. The wastewater is <br /> collected and pretreated by screening, pH adjustment, dissolved air flotation, biological <br /> treatment (trickling filter), coagulation and flocculation in the lamella separator. <br /> Wastewater is pumped to the Manteca Wastewater Treatment Plant, hauled offsite, or <br /> discharged to the land. <br /> 2.3 GENERAL GEOLOGIC AND HYDROLOGIC SETTING <br /> The site lies within the Great Valley Geomorphic Province of California. The valley is <br /> approximately 400 miles long and averages about 50 miles wide, and comprises about <br /> 20,000 square miles. The valley has been filled with a thick sequence of marine and <br /> non-marine sediments from the late Jurassic to Holocene. The uppermost strata of the <br /> Great Valley represent, for the most part, the alluvial, flood, and delta plains of two <br /> major rivers (Sacramento and San Joaquin Rivers) and their tributaries. <br /> The valley deposits are derived from the Coast Ranges to the west and the Sierra <br /> Nevada to the east. Granitic and metamorphic rocks outcrop along the eastern and <br /> southeastern flanks of the valley. Marine sedimentary rocks outcrop along most of the <br /> western, southwestern, southern, and southeastern flanks and volcanic rocks and <br /> deposits outcrop along the northeastern flanks of the valley. The valley geomorphology <br /> includes dissected uplands, low alluvial plains and fans, river flood plains and channels, <br /> and overflow lands and lake bottoms. <br /> 101486.41ST012R025 Page 5 of 20 February 1, 2012 <br /> Copyright 2012 Kleinfelder <br />