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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v^hsro theword east is written, w; , . l.^ost ury, aiia all of ttie cio*ie-t,as shown on tj-iat i.iar), on tne east aide, were reduced to asn;ali bxea; on t.t . :- .iae, the west cienega written onthe tiap hL,d been uitched with several ditches, anu ttie iiie&s-urenents of water which 1 gjave hero the ot-Uer day, very smalqurjititiea, were coming, froia tliose developweats; and th westcioriOi-jti \;as piactically dry at taf^t ti;ite anu not as suown onthis iiap; this rriap was really uiaue to show the orii^inal con-dition of theciene^as before any devolopraent except the Ytunnel had been ;.iaae, ,. .icve you exfv ined plaintiffs .^il^iibit 39? A Yes. State waat opinions you i:iave ueauced frora it with re-ference t,o the matters in issue here? A The opinion deduceu fror. tfiat is that the two forPifitionsthe one 8ho?m as sumriat of had hill on the ri^^hl huriu side,and the other foimation ne(sinriint; at the point where the twobroken lines showing- east and vest sice convert, that
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_^4L 1 2 3 4 5 6 7 8 9 10 11 12 1617 1819 2021 222324 25 262V2829 beii\i the ancient forniition, and the other thft oaoin fori.ifc-tion above, are Bhown try tLis exhibit to be two ^ istiiiotformations, beiri^ noncoiiforruable, as the ned hill Iie.e ap-peared in tliS fonii of rui uplift, which has gradually erodeuand abraded, until it <iae reached the preoent flat-top coii-dition; .hereae, Uie other formation lies against it non-conforii^ably, bei v-, the result of recent wash cepositea a^^aiBstthat ancient alluviunu ^gain, 1 for;;) the opinion tliat thedeposit ooth on the ei^at tMQ .eat side ctiannels, over thecut throutjh the ancient alluviuj.i, is very sli^M, as thegrade of the upper basin projected throu^;h coincidet prac-tically with tVie dotted iiae showing channels throu(;h theEjicient alluviuxii, and -sero tnt^ outs deep tiiroue,h the hedHill the upper basin .vouj.w atwvu ts-sauiued a different grade,inateac of buildint, up to that point; which snov^s the pointof control of

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