. In Superior Court of the County of San Bernardino, State of California. Department One. Cucamonga Vineyard Co. et al., plaintiff vs. San Antonio Water Co., defendant; no. 9187. to Lhst saflie oonaition, but T?ouldnot apply to saiy otner conuition is not eznctly likeit in PVoxY particular. The Court, ^ As i af>raii6, you takf; c certiiin »ell ^nd tnjasureinent from the spriri.«;s and Y ; of coursethat is cfi trie aeBUDiption tcv^t the cone i Lions are T>pi-nianent;you to not into coiicicer^.tion in calcult-tion anyBuch influenceB as rainfall or teFij;
. In Superior Court of the County of San Bernardino, State of California. Department One. Cucamonga Vineyard Co. et al., plaintiff vs. San Antonio Water Co., defendant; no. 9187. to Lhst saflie oonaition, but T?ouldnot apply to saiy otner conuition is not eznctly likeit in PVoxY particular. The Court, ^ As i af>raii6, you takf; c certiiin »ell ^nd tnjasureinent from the spriri.«;s and Y ; of coursethat is cfi trie aeBUDiption tcv^t the cone i Lions are T>pi-nianent;you to not into coiicicer^.tion in calcult-tion anyBuch influenceB as rainfall or teFij; or (; of otn-er \,oll8. iv liO, sir. i am tioing tai» to ans^ei the theory that the16th eire^t wells cuuso the rise and fkll of the Cucaninn^>Springs, and iffioriiit: every othnr vhi::h I believecoes cause r/noee tning^s. I was LraiouB to fim out /our theory v;a8, becauseI aesLunea you would use it labor on in other rheorieowhich you advance. ihe tneory is taat if of those j/ells res-ponsible for UiO decline, then the oof line woulc have beenHS Bhopn by my calculated line iristeuJ of np. it rejilly itr i-oKinloy, Ci ..ill you finish your doaoription of th0geologic ana uheir effect on tho arxdQreTOundwaters? A Kefffrrin^, i,o the diji^ua, oefondtuts exhibit Z3, theoluer formction, deaigruited by CQ on this ciagraa, whichis foldec in tue lonn of an arch, concucts tliia wtter fromthe point vliera it is received at the upper end to the lowerpoint inhere it vtj be tapped by wells or onier^e fJj ciene^asat the r at onco to sinkdown, ano liore the recent gravel lies over iiie ori/^inalmetciaorphic ro^k a, it sink? to tliat, and percolates downthat, anc enters tiie upturned strata of tiie old formation C,where it io received, biC t-s t»oon as it descenus to the pointwhere the are filled it becoites h presoure supply (rtwater; before that poin
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