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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ated niasawhich lowered the head, to the saae extent lowers the disOcharge to tne duct; /. In tlio assu-.ed conditions that you niake. that would in-(Vitauly follow. It WDuld iuive to ije fomplete stturation ofall tiie voids so that one jaolecule would rest on the otbBr.>* If tne heads or oponint;;s of tnese ducts at tueir intakes areBX far up tOT7ardB the mountains, still if the plane of sat-uration of the overlyin£j new alluvium v;aa sufficiont to ex-tend up near to tiie Liour^tains, tiiat would add to v.e pres-sure of v/ater, and the inflow of water into tiiose duotsrii Yes; if the plane oi saturation of uiy new alluviumextended over tiio openin(; of the ducts, anu tiio saturationwere coinplete, tliat ^sould undoubtedly add to tne old alluviun at Uiat point. in anu.verin,, Uicse questions, I amanswering on your assumed hypotnotical conditions, and noton any of my own opinions as to Uie conditions.■■^ It does not involve any admission on your part tiiat suchuonuitionc exist.
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84 4584 A That is whitt I uncierctand. Q llov, in a stale of nature, boloro t .ore ./ /j any iijyasionof the Jucanion;?! district by ^-elle and tunnel c a.d r>uinpingplant0, the dischar/je fro.i the Gprinjs rae in a fprcat /leas-ure a c-onatant discl^iarg© ¥ai it notr That io, it variedaomowhat, but it didnt var/ very ,Teatly?A Ab far as re have any records, it has varied cTeatly atall times. You take liihibit 32 of the plaintiffs, -).ichrives all tlie old /neacure.ents that vo have knoTrled^e of, itshows very fpi^at variations. Backx of that we liavent anyknowledge except such as we can fjathor by reasoning from the(:eolo(;y and the ancient hydro^p^aphic conditions; and underthose conditions, I believe tUere 7<ero equally great varia-tions. The conditions of the Iod Ilills ^rould indicate thatat somo ancie t time the water has risen throu^; the ancientalluviur.i aUioat to tr.e suu.i dt of Uie hi^jiest ;^ed liill. 1tt«can see by ^jaliin;- over the surface the rcrains ol ancie

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