. 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. i- Are you ref-^rrir;^ now to the water in the ancient or inthn recent aeposit? W I art not reforrin^; to the water in any particular deposit;you have piven us 160 inches as : fro;, the San /intonioCanyon, and you have ^^ot it c oesinv- this sluice way, thisoutlet of the gravel basin, .«here crater is proceeding, south-?/ard to Chino and the San Ani Kiver a ^Te-it depth, and 1inquired of you why water
. 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. i- Are you ref-^rrir;^ now to the water in the ancient or inthn recent aeposit? W I art not reforrin^; to the water in any particular deposit;you have piven us 160 inches as : fro;, the San /intonioCanyon, and you have ^^ot it c oesinv- this sluice way, thisoutlet of the gravel basin, .«here crater is proceeding, south-?/ard to Chino and the San Ani Kiver a ^Te-it depth, and 1inquired of you why water from the San Antonio Ctjiyon,instead of ^ across this depression, in order to buttup a^iiist the Red liill, aoes ot folio?/ your outlet andproceed southward there. A ftell, in s^iswerint; such a question as that, you have torecoi^-ni?,e the ];nown facts, regarding; the geology, and dis-tinguish tho two formations, and that really ip tvo questioBs;1 can take the lii UT> one at a if you wish to , I askod you only one question, ou have a corabi)ied condition in your question; now, ifwe start first with the early deposit, or quaternary pleios-. ticene , tf. it ir, kriown in gpolo^^y, the water afterit haspntr;rcd that is preecure, f ollov b the olu the natuie of an invertea eiphon, emertain,, in wells orsprings where it is folded or at a t;reater uiatrrnce clown inthe niain a-rAn of the valley, th like the Saait& ^iiu iiivor,the Chine b&sin, or elaertiere; anu after navin^ once onterecthose okiannels, at soiae noint below the foothills, it wouldthen traveroft the CwUiso in wnicu lnuij foimtioa was it^idCom orijjiiiully. )k-iv/, turnint_, ne: t to ^ho o-hcraiae of it oi the recentalluviorns, or rccEnt quuLG*\iaiy, tliat nr^s also been laiu apwnsoiiiowiiat in tiiut :vay, but no I consoliautoa or laia uov/nwithsuch a pre-jondoronce of fine Litterial, ao Uiu tenuency ofthe *abor is to flow or porcolato alon/j the liue on whichtho
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