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It is a broad structural trough surrounded by \r\nmountains. The northern part of the valley drains through the San Joaquin \r\nRiver northward to San Francisco Bay ; the southern part of the valley normally \r\nis a basin of interior drainage tributary to evaporation sumps in the trough of \r\nthe valley, chiefly Tulare and Buena Vista Lake beds. \r\nIn years of normal discharge most of the streamflow in the southern part of \r\nthe valley not diverted for irrigation finds its way to Tulare and Buena Vista \r\nLake beds. In the historic past, however, during years of heavy floods the low \r\ndivide between Buena Vista and Tulare Lakes and the low divide between \r\nTulare Lake and the San Joaquin River were overtopped and through-flowing \r\ndrainage occurred over the full length of the valley. Because the Tulare Lake \r\nbed is the lowest point and also the largest sump, this whole basin of interior \r\ndrainage is commonly referred to as the Tulare Lake drainage basin. \r\nAverage annual precipitation ranges from more than 15 inches in the north- \r\neastern part of the valley to less than 4 inches in the southwestern part. The \r\nprecipitation decreases from north to south and from east to west across the \r\nvalley. Streamflow, the critical quantity in the water supply, depends almost \r\nwholly on the amount and distribution of precipitation in the Sierra Nevada to \r\nthe east. Much of this precipitation falls as snow, and the snowpack acts as a \r\nnatural reservoir retaining much of the annual runoff until late spring and early \r\nsummer. \r\nThe mean seasonal runoff to the San Joaquin Valley is nearly 10 million acre- \r\nfeet, of which about two-thirds is tributary to the San Joaquin River; the remaining third is tributary to Tulare Lake drainage basin. In 1952 about 8.5 \r\nmillion acre-feet of surface water was diverted for irrigation. Withdrawals of \r\nground water for irrigation in 1952 approximated 7.5 million acre-feet. \r\nThe surface of the San Joaquin Valley is not a featureless plain but is characterized by various types of physiography such as dissected uplands, low \r\nalluvial plains and fans, river flood plains and channels, and overflow lands \r\nand lake bottoms. \r\nThe dissected uplands fringe the valley along its mountain borders. They are \r\nunderlain by unconsolidated to semiconsolidated continental deposits of late \r\nTertiary and early Quaternary age which have been moderately tilted and \r\nfolded. The topography of these uplands ranges from deeply dissected hill land \r\nhaving a relief of several hundred feet to gently rolling land whose relief Is only \r\na few feet. \r\nThe low plains and fans border the dissected uplands along their valley- \r\nward margins. They are generally fiat to gently undulating and featureless and are underlain by undeformed to slightly deformed alluvial deposits of \r\nQuaternary age. \r\nThe river flood plains and channels lie along the San Joaquia and Kings \r\nRivers in the axial part of the valley and along the major east-side streams. \r\nWhere the rivers are incised below the general land surface, the flood plains are \r\nwell defined; but in the axial trough of the valley, where the rivers are flanked \r\nby low-lying overflow lands, the flood-plain and channel deposits are confined to \r\nthe stream channel and to the natural levees that slope away from the river. \r\nOverflow lands and lake bottoms include the historic beds of Tulare, Buena \r\nVista, and Kern Lakes in the southern part of the valley, and the low-lying lands \r\nin the axial trough between the low alluvial plains and fans and the natural \r\nlevees of the San Joaquin River and its major tributaries. They are level and \r\nfeatureless and are underlain by lake and swamp deposits of Recent age. \r\nThe San Joaquin Valley is a great structural downwarp between the tilted \r\nblock of the Sierra Nevada on the east and the complexly folded and faulted \r\nCoast Ranges on the we","language":"ENGLISH","publisher":"U.S. Govt. Print. 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