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

View Book Page: Book Viewer
About This Book: Catalog Entry
View All Images: All Images From Book
Click here to view book online to see this illustration in context in a browseable online version of this book.

Text Appearing Before Image:
n, uhy is it under those circuiustances ana con-ditiono tJiat taeUucation^^ G priM(;;;e dont flow more tirian tiieyever did after ^ou pile ao aaicii vater into it^ . For tiib sane reasmi that if you have a flume threemiles lon(^, if you pour water into the upper ptrt of tlie^uiae ^ou dont get it at Uie lover end till it haa tineto floTr doYm uhere, 1^ Ye»i but you have said hore a nu^a^^erof times and i^.Trask has said a niabar of tioea tlat tiiese springs quick-ly revSpond to Uif rain. Tt^iat &l soon as those wcllr. areclosed th«86 springs lie^^in to flov/ L.ore» and tliat ttiatdont show aiiythini^^ but tuat it i;; a coincidence of thisram that comes in there and traxisiaits this quick pressuredown UiroUt;h ttie aicicrlyin^j strata. A I beg your pardon for BLyinf^, trt you are net quoting aecorrectly, or r. Trask either. \*e said this: iiieu tiie rainsoonie Uiey do fc(jd t^.c sorin^s soinawliat from the water tka.fallin^^ in Uie irsmediate viciidty. But iiisi is all we didsay.
Text Appearing After Image:
Q Nov, tiic il iodiato vicinity is u.c 16th Street wells, is it TiOVi h \o indeed, it is not. jx They arc only 3;00 foet up the etream. ( i^ut the innediatc vicinity is Uiat riir^iit around tiie RedHill and that docs ahed latcr and helps the springe andal) the wells. How lar^.o a v.-atcrshed area is ttiere between the Fiubiowell and whore U.c nprings name outi Figure thnt outV n well, there is e vyatershert there eoraethiiig like asquare mile, possibly /.lore, from the contours on Un t map. Q Ahtt kind of soil is it there in the major part? :\ The hills are clay soil which shed their waters rapidlybo the gravel a in Uie channel, anc thereby they help thebarings* H How much rainffcll «an you get oif of Uie.t area ofgrounar How tnuch run-offY Tiiat is a mstber of computation which i have not made;but you net quite a lit LI-, ruii-off from that 8P(uare mileof area. Q Can you fi^^iirc out a square irdle there? i: 1 think 1 coulc do it if I had sufficient time. Q I wish you would do t»mi

Note About Images