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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s not crossiiexanination, -^ndthat it a-^plies to ai)othor locality. The Court: The ob;:ection is ovorraled. cfondanto except,A Yes. I testified to tliat. hrd is trae nJDSolutoly inLhe San I^emardino valley. The dike of the Uan i^emardinovalley belon/,;;s to the chaiiplain deposit. It is an extension01 L!;o Texas point deposit,in Lytic Creek, arid this depositof the Gan iJernardino valley ^-as maae at tlio Bajr-.e pcriods.ihwiia the last der^ositc ia the rxicajonga basin ^er* r.trx!e. Theydo not apply to tiiO ancient aluvluin. Ilie Ljsn x©r:.-.rdinovalley is in the recent alluviULi. /jid ^dlc the artesianbasin in thp- -ft Bernardino valley 7ra,s fo-^T-r exactly aa Iiave there sLatod, it does not apply to -. .v, L.rtesia^ forr.a-tion at the led Hills whicli bolon^^ to a previour. colcicalDoriod.Q Uut you stated the lake — you have stated in ^rour t«>sti«)ny on direct examination Uiat this .:uca..ion(_^ lake extended■r tr o-rt ,f t.up v-.UoYt ^-^ -hnt t)m T.ytle Hreek dtmosita
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10 11 1213 §15 O m 16 17 18 19 20 21 22 23 24 25 26 27 28 29 _02 ±dlIlL S..0T7 ti.ul ii, v/as a Oijare of that lako: .. Certainly, ;.r, iiasi:ell. If you Trill rolloct a uanont,you will cee that UiQrG is not .in^: inconsistent^(WUiutiiat.In uliQ early quaternary deposit — wiioa the early quatc:.Tiaryclepooit at the Hed Hills wa& laid do ad. thero 7i3,a no 3an l^erl-nardino :iountaiii ran^^ in oj^istonce. Vhat \b.b all under ?»t€r.iho tirsw tix.ie the Can i.eniardino inountain rango eaae intoax-istence v/as during the latter part or c?<.ose oi Uie uuan*-plain period iieri tiie lake condition v/as auout disappwarinoHowever, during tiie champlain period the only etreara i*iichwao running: into the valley vae the most easterly stream,Lytle Jreek, c. fro:-x the San /jntotiio peak. lytle Creek at t)iat tiine, during; Uie close oi the droaoplain period, de-posited not only Uio ^.javels \riiiCi. you see in the Tcxaa Point ine, but also deposited tiie Material which wide the fi\l

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