Identifier: insuperiorcourto07cuca (find matches)
Title: 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
Year: 1907 (1900s)
Authors: Cucamonga Vineyard Co
Subjects:
Publisher: (San Bernardino?
Contributing Library: University of California Libraries
Digitizing Sponsor: Internet Archive

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wiiat 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 whichthose deposit a were orit^iiiiily It. id down, and a portionof oiUB 160 inches, uoe^, throu^ti the rooent alluviuni ,finu ity way throut^h ihat outle^; i do not t/iink tliat allof it vcoee, iicauii© of tue wcy in whik that deposit laioii(,ifiully fon-itL; in older to co that it would nave toLrsvVal tranevc-ruoly to ti^ strike, which ie a la* not aur-ie-siblo, in dealiiifc^ .vith water trrTslin^; thiou^/i uctuerfc,roijnd BOHICQS. H iou at;.ted thhat the Courvine vfll, next to the vntarioColony lanus, 1C4 feet Qocp, or auch a uiatter, inuicatesa K^eut dev.th of dry j.ji.terit 1, ana thr.t It is very coarse:thoae tV.in^s you tiave cu.reed tor it uoea, 6Xid i a^ree to that; that is part of the facts, s, ..hy chculd youz i/at-r, your 160 inches, -asfeia tliatopportunity to pursue tne iiiis of least res iance, dov;n
Text Appearing After Image:
_6 throu,;;li the outlet here, why ehould the 160 inches from theSan Anto^^io Canyon, one-ei^jhth of the entire ordiuuryflow of the San Antoriio Canyon, avoiaiix the opportunityto tjet out throutjh this coarse gravel, and sand, depressedat a ^^re:.t de th below the surface, at the point wnich ie xzriiarked by our friends r irasland r x^inkle, as an outlotof the ^avel basin, in order to ^o clean across the samegravol basin, and butt up against the weot siae of the Hedhill, principally we £-re inforrjod in the nei^hbornooo ofthe Jadie tunnel and the 16th street wolls? . iijst, -.ectiuse a part of it truvols tnrou h the ancientalluviums wnich aie undcrlyin^j the recent coarse deposit of\&hich you speak; seconuly, Decauae in this coarse deposititself, there are certain stratifications, which are notanytiiin-j like as marked as in the ancient, but nover-theldss they do exist in a measure, which would have a ten-dency to ^aide some of that water away, but I do sp-y I hat apercefita^-e

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