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The unconsolidated contental deposits consists chiefly of alluvium but in some <br /> areas include widespread lacustrine and marsh or estuarine sediments. These <br /> deposits constitute late Cenozoic fill in the structural trough, whose axis in the <br /> San Joaquin Valley lies west of the present topographic axis of the valley. <br /> Appreciable folding and minor faulting also has occurred; however, these <br /> structural features have had no significant barrier effect on ground-water <br /> movement. <br /> Consolidated rocks form the boundaries beneath and on the flanks of the <br /> productive ground-water reservoir in the unconsolidated deposits. Only minor <br /> quantities of water occur in joints or fractures in the consolidated rocks in the <br /> Sierra Nevada, and the principal water supply to the valley-the stream runoff- <br /> passes over them. <br /> Ground water occurs under both confined (artesian) and unconfined (water <br /> table) conditions in the Central Valley. The degree of confinement varies <br /> widely because of the heterogeneity of the continental deposits. In the big <br /> alluvial fans on the east side of the San Joaquin Valley, the ground water is <br /> unconfined. The most extensive confined aquifer is the major aquifer system <br /> overlain by the Corcoran Clay Member of the Tulare Formation, which covers <br /> more than 5,000 square miles in the San Joaquin Valley. <br /> Recharge to the ground-water reservoir is by infiltration of rainfall, infiltration <br /> from streams,canals,and ditches,by infiltration of excess irrigation water,and <br /> by underflow entering the valley from tributary stream canyons. <br /> 3.3 Historical Use Aerial photographs were reviewed for evidence of prior on-site and off-site <br /> Information features that could pose a potential environmental concern to the subject <br /> property. These features included, but were not limited to, sumps, pits,ponds, <br /> `— ASTs, landfills, outside storage of hazardous materials, and general land use. <br /> Aerial photographs from the years 1968, 1981, and 1992 were reviewed at <br /> Pacific Aerial Survey, Oakland, California. The earliest available photograph <br /> covering the property, dates to 1968. The following observations were made <br /> during the aerial photograph review: <br /> �- 5/1/1968: (1:30000) The Tiki Lagun is visible on the photo however it is a <br /> smaller operation with some open boat docks and one covered boat <br /> dock. The campground area to the east of West McDonald Road <br /> r was not visible. The surrounding areas appear to be in agricultural <br /> use. An agricultural processing operation appears about one mile <br /> to the west of the subject property across Turner Cut. <br /> 10118/81: (1:54000) The subject property has been expanded since the <br /> previous photograph. All of the covered boat docks are visible,and <br /> there are some campground spaces on the north of the property, <br /> east of West McDonald Road. The surrounding area is still <br /> predominantly agriculture. <br /> BLASLAND,BOUCK&LEE.INC. <br /> NEWT1q.WPL) 5/706 engineers & scientists 3-4 <br />