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Ground water in San Joaquin Valley, California . OiO^OlNOOOONOONOOONNONOOOOOaOHNOOOOOOONINO Q<S ? NNt-iNHO^oocqcqto d oj 03 O o o .a .a .a .a <B rj <UO O rt o .|.a 5 -dV-d ^222 6J52 o o o d o tT o =•« -d° -d -d-d d ,2 2£S - -iTD (jaQJ^- © O) ® ^ PO -do OOOO :<n :ppqppw :pw :pppfq cja^ ft )00««l<D«OOMOtOON103050500050300050300000500100000000000000000000000000 • oooo ooooooooooooooooooooooc eSuBa •ifltiosdi qs -UAV O J, •uoi^oas i050505OOOOOOOOOOt COCOONCOCOCONNNNNNNcDcOOOCOCOOCCtOO©^OtOCO?000!0<OcOcOcO?0 .a-s I sl|l! IPS sSS i||™-8 S 3M -r-i ° ° £E :K :£W o :£W oc x: x x x x o o • . : OrOCOT-H-^l x r. ; - ~. — r; x as x < X X X X X X X X X <M(N04<M<MC^tN<N<NC^<M<M<MCqcq< CwONCOOOCOCOOtOCDtOCON. 252 GROUND WATER IN SAN JOAQUIN VALLEY. TULARE CONDITIONS. Tulare County, lying north of Kern and east of Kings, includesthe eastern edge of the large central artesian basin at its widestpart, all of the delta of Kaweah and Tule rivers and a part of thatof Kings River, and the famous citrus region of the foothills and thehigher parts of the valley floor about Portersville, Exeter, and also includes, in the southwestern corner, a part of the old bed ofTulare Lake and a part of the district submerged during the lastextremely high water, in 1880. The high water of 1905-1907 didnot quite reach the Tulare County line. Kings, Kaweah, and Tule rivers are the chief sources of such addi-tions to the ground waters as are made in this county, as they arethe sources of the surface waters used by the various canal of these streams has a distinct though rather flat delta, andthe attitude of the ground-water plane indicates that the streamchannels and canals a
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Keywords: ., bookcentury1900, bookdecade1910, bookpubl, booksubjectwatersupply
