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I - <br /> a <br /> '1c <br /> Aeration with <br /> OF WATER RESOURCES <br /> EXPLANATION <br /> PQ <br /> alOb <br /> 1p <br /> e <br /> a Alluvium Flood-basin deposits <br /> ZQal, unconsolidated clay, silt, sand and Unconsolidated surficial and near <br /> a gravel deposited on undissected alluvial surface deposits of clay, silt, <br /> fans of present streams, little or no sand, and gravel reworked from <br /> r <br /> o soil development: permeable to moderately alluvial fans and deposited on < <br /> e permeable the flood plain of the San Joaquin z <br /> o Qalp, unconsolidated clay, silt, sand, and River: moderately to poorly permeable F <br /> y gravel deposited on partly dissected < <br /> .0 alluvial fans, soil profile developed d <br /> y with variable hardpan: moderately to <br /> poorly permeable <br /> cNILdl <br /> a <br /> o Terrace deposits <br /> m Unconsolidated clay, silt, sand, and gravel of old stream terraces above <br /> 11 the level of present stream valleys: generally above water table <br /> Y <br /> 4 x <br /> z <br /> r <br /> Rive r <br /> ......:::..... <br /> Tulare Formation <br /> a <br /> Q f w u Unconsolidated end semieonsolidated continental deposits, poor to well- d <br /> R v e rp sorted, olive-gray to yellow-brown, intercalated fluvial, micaceous, 2 <br /> v <br /> c .. arkosic sediments and calcareous greywacka of clay. silt, send, and < <br /> v <br /> u <br /> 0 gravel interbedded with transitional deposits and lecustrine sediments, <br /> E � evidence of several paleosols:, highly to variably permeable <br /> y 4 <br /> UNCONFORMITY <br /> a <br /> ' a TPTU m <br /> S eme¢ka p�t'`tn 4eeg stalline cocks, undifferentiated C <br /> o Unconsolida ked �Ae�mxeotescl� a d and well indurated continental and marine w <br /> 1 F <br /> o e`a`vel.,esnda tone; <br /> ' 'l'a shale; bentonite; cley- <br /> c clay, silt. aand" rend` :vu a <br /> in trusive or metamorphic base- <br /> atone; carbonaceous- sfirlt,& !nd,.underiytag P <br /> meat complexi.Gocks-I e t •r,ka� thL�s.�z one exceeds depth of most water wells z <br /> 3700... in the''sca {'i. Ft4 fi <br /> 70 a. tea°.. "•r 2"' _ � <br /> 31 a a <br />