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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oo on the rjcp anu detorciinc justhow iar it ia ort Iveiondants :iyhibit JjV ii At the ^K)int marked Section 30, on i»efeiidants i^ixiiibitJj, £.t t/uo intorsection of Zkm etrcftt ijjid Juciicl Avenue,Ontr^rio, the cnmler of soot ion 30, i» the r-oint vvherp tJuitre in!ail record wa? kept. Q Just ;-iark ti-fit Jiarwood ^ii.l you? .- i imvft written tJie vord Harwooo there; in a directii:io it ig two and a ojuarter wilos inetecid of t^o and a huifas 1 estiiiated,Lt )3ritt, U Due west? i. No, it it not due west; that is northwest frora the itedhill; due west tne (.ietcOice would be nucn lesn. Lr i-ci.inley, ; what watershed is it in? L Thct ia in the Ouc£:,juon«^a cster Shed; it is in the eauiewater!^hed vhich ie drained by the (Juoauaon^R Jpjiyon, cjadtriuitary to the hed hille. i Proceed and explain your views as to the n.infall, asto tixoso waters iri question. a The rainfall in that vicinity, likr every oMier localityia doyendenti on olsvation, and liavir^ a br.oic station from
Text Appearing After Image:
.^^ — 1 •filiich to figure, it is poeeible to obtain by calculation the 2 r&infall at other alevations known, in the ssuue neighborhood. 3 For the yiumope of dein/^ thie we apply a rale deduced by experi 4 raent from observations and firet promulgated by the United Stat 5 •eologiqJurvey for thie section of the Facific Coast; this 6 rule is founded on experiments, showing that the inean in- 7 creape of rainfall from B€i.-).evt!l on the south txiQ. west slope 8 of the Mountain ran/res in Crlifor i., incrot the rate 9 of .6 of an ir»h tpt h.mcred fiet rise in elevation, up to 10 -.. point 6000 feet naove eea-V-^v^l, fioir. that point up a 11 similar decrease occurs, ur to 9000 feet, \?hich ia the limit 12 of the r»inf?ll elevation?? mvorftfl ^J o^-porimonts up to this« 13 tiriie; fbove 9000 feet A-e know no thin/: about it, ro that it2§14 if inrospible to fi^-iure from rjiy ^norn e^tpsrimrnts the prob-is IS able n-inffill cbov-t^rt rlpvrition. - It! il6 This i-ule is fvpT

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