. 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. e UieChamplain clay, as wb call it from thf? top, euid )£ke a tiiin-ner over ttm,t portion th^n tte porioc preceuing. ^ Ifou itt:.ia less thin: Jacn it was moro tidn inatcau oflesn til in. .I. ihat was what i said wasnt it? U No, you said less thin. ix I hei; yoiir ; ao iGtimee one saya one tuint; whenttiinkin,; of ; 1 rreant rcore thin, 1 used oppositey;ord, V. And the appeartince of t
. 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. e UieChamplain clay, as wb call it from thf? top, euid )£ke a tiiin-ner over ttm,t portion th^n tte porioc preceuing. ^ Ifou itt:.ia less thin: Jacn it was moro tidn inatcau oflesn til in. .I. ihat was what i said wasnt it? U No, you said less thin. ix I hei; yoiir ; ao iGtimee one saya one tuint; whenttiinkin,; of ; 1 rreant rcore thin, 1 used oppositey;ord, V. And the appeartince of the rrater would not ha^e occurred,but for tlie ^iros-^ure of other wator behind itby forcin^^it ..Ion,- /ouli it? L It sould not;.bocause in order to hare the water appearthere, thore ffonld H^vb to be a head on the strata whichcauaea it to yppear, at eone hi{i,her el?ation that thepoint of ^^.r^^ireince. W Some hiher olf^vjtion? A Some hif;her elevation in the ?;.ir;« strata, ^ And if tViP strata where ths «at«r appears are much brokenup, iuibled up and dipjcinted, thor: Uiat pressure niay beexerted :.hy it not, by any watpr wisk which is in oontactwith such stratum?. 45 A Ifx it io in circulg-tory contact; not i;; str-tic conl/act;where you spesk of , you have to (iifttiru -r-Rh ue-tveeri static preenure ano hydraulic rrpiBrure; anci f*^ i ^prii^/s is always coi-ifv: thiouf;h ano furnisJiedimder hydraulic presmu-e, and therefore wetpr in circulation;water niif-ht be in contact through a r,euiu/ii 00 Anre that itdoes not circulate, it no Oiilo not &io the c»:ergcnoe»f vattr throiv^!h a coBrpor Btratum adjoii^in*;; The water appearing-; in these strata or connecting thecestr^-ta in ttie surface r,-£jiifestation8 which were anoken of,ffiuet h&vs bscn m circulatory condition. A it .iiufit have open; otaert^ise it could not have mrAv^.iias sprirv-s; that pres?ure :;ould not ce derived from a donseclose laaterial, in ffhi-h the contact W&g
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