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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it, and measured the watcr-lovel in it at varioustimss, to ascertain whether there was a rise of water at anytime above the surface water; the other wells on the exhi-bit 1 aw not familiar with. k iill you examine Interveners ilxhibit number 1, Andstate wViat opinions youxaeduce from it/ A Interveners blxhibit nunkbor 1 is drawn much the taut aiilxhibit K of the aefendcmts, except that it covers a lar^-jenumber of other wells lyin^ further south, and is i.ot an in-dex to the direction in <vhich water will travel, as will beseen by reference to iLihibit y, that the lines are not laidout parallel v/ith the mountain ran^s, or parallel withthe strike of the anciont alluvium, but at an angle to thesedeposits, and by runniiv:, the line on an angle to the south-easterly, a fallxof the waterplane can bo mad* as thedelineftor niay desire, and the only and final test of thewater plane and of the direction in widch water Tould travelwould be by layin, uown hycirographic contours, con^ectin^;
Text Appearing After Image:
1/ -r^, , , the levels of Uie v9,iiou8 .79)la, ^ Will you examine Interveiiora 5zhioit number 2, aridstate wiiat coirunent you fUi.ve to .nake upon it, v,ith reieronceto the ano-^irjj; triat it inykeoV A Intervener a Exhibit Kiumber ,?, snoT/?8 portions of the hydro-^aphic contxour alon^, tue uietrict of the xied Hills, anaif theoo fjytirographic contours are reliea on, which are sLOTmin the aec.vy lines, aiici iiiarkeu vath the elovalionr, the wat-TfroiTi tno 16th street v.eliB woulc percolate tc tne southwest,as is shown oy the hyurogiaphic contours v:hich i introduoeutnis !:orning, and taker; in ccniiection with erhibit nuruber 1of the intervonors, it v/oula Bno* Uad, in the old fon.iationon tr;c east side, the water percolate to the fioutheast, inthe 0 posite direction from tiiat r-hich it travels in therecent iorriuition to tne vvest side. li vhat is indicated by the ch*ii^e in water (/ratie ^>iiereV ii ihe changes in water ^~;r?iue tnere are due to ti.e contactbetween tue rec

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