. 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. pieces of the olu pipe rhich had beenta):on out; jio you reijemb<ir waich vrell 1,iiat was? I recall thu circuujetance, but 1 donb reLi^iuner wnichone It. v;:l5; 1 r 3ull the cirourastance you mention, but Ithiak you J iiaw to obtain the fact as to which wellEih-at was froia sorae of the officials of tne oau Antonio .< , as 1 never Made any note as to wnicH well that .^cKinley: 1 tiiin


. 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. pieces of the olu pipe rhich had beenta):on out; jio you reijemb<ir waich vrell 1,iiat was? I recall thu circuujetance, but 1 donb reLi^iuner wnichone It. v;:l5; 1 r 3ull the cirourastance you mention, but Ithiak you J iiaw to obtain the fact as to which wellEih-at was froia sorae of the officials of tne oau Antonio .< , as 1 never Made any note as to wnicH well that .^cKinley: 1 tiiink probably Mr Tr(*,sk ^oula knoi that; 1?Will enuuu,vor to supply tiio incarnation lo ioiir a-mor;i T/iil endeavor to su-nply the inforiaat-ion to the 0 urt. Jhe Court: Viie nmson 1 inqjire for that is uecause of tkiefact that it indicated 8, very coarse foniiation ajn©whereb-^low - lar{;;e boulders, ...r Crcodcell, ^^ Then you have liaskell well locatedif IunderoLajTid you, in vKat -^oulC px-actically at nearly alll^imes, be on tne sice, or in the eady of the stream, andnot in tne line of any ciiamiel. u Motin the liuo of the nuiin flow; undoubtedly side criaii-. nels have pc^ssid throufli tlriat area from the main stream, butowin^: to the peculiar strike of tho ancient formation there,that would be in a more quiescent part Oi the b. sin, and theviolent flows of water which brought do7m the very coarsegravels could not have passed through that lo ation, but fur-ther to the west. u Nov., as the location is represented here on DefendantsExnibit h, that v/ell is practically in a corner, a cornerthat is bounded on tho south and on the east by the ^^dAlluvium, as on the exhibit. i- Yes, 1 see it ia; but I hardly taink that triat is a cor-ner; I it is isore of a curve, and on this map the is broi^;ht f. little too far to the north, on thewesterly r-ortion; I uiade tpothfT drawing which niore nearlyexpressed uy own ideas ; i forget ^hat exhibit that


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