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("KLE/NFELOER <br /> Bright People.Right Solutions. <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 Berkley, <br /> California. <br /> Potable water for the CNP plant is obtained from the City of Lathrop water system. The plant <br /> 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 vegetables, <br /> surface spillage, clean in place solution, and evaporates. The wastewater is collected and <br /> pretreated by screening, pH adjustment, dissolved air flotation, biological treatment (trickling <br /> filter), coagulation and flocculation in the lamella separator. Wastewater is pumped to the <br /> Manteca Wastewater Treatment Plant, hauled offsite, or 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 20,000 <br /> square miles. The valley has been filled with a thick sequence of marine and non-marine <br /> sediments from the late Jurassic to Holocene. The uppermost strata of the Great Valley <br /> represent, for the most part, the alluvial, flood, and delta plains of two major rivers (Sacramento <br /> and San Joaquin Rivers) and their tributaries. <br /> The valley deposits are derived from the Coast Ranges to the west and the Sierra Nevada to <br /> the east. Granitic and metamorphic rocks outcrop along the eastern and southeastern flanks of <br /> the valley. Marine sedimentary rocks outcrop along most of the western, southwestern, <br /> southern, and southeastern flanks; and volcanic rocks and deposits outcrop along the <br /> northeastern flanks of the valley. The valley geomorphology includes dissected uplands, low <br /> alluvial plains and fans, river flood plains and channels, and overflow lands and lake bottoms. <br /> The majority of the native sediments near the site consist of Miocene to Holocene continental <br /> rocks and deposits of a heterogeneous mixture of generally poorly sorted clay, silt, sand and <br /> gravel. <br /> 00101486.8/SAC15R19291 Page 7 of 17 May 6, 2015 <br /> ©2015 Kleinfelder <br />