. 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. e vatf r comes into those ducts? A These ducts are the old ohan els of gravel laid downthroui^ the fine silts, and while the friction is consider-able in these channels, the hi, her elevation of the ductsabove, where they first begin to accumulate pressure, issuch that in spite of this friction the head is sufficientto discharf^ the water as naturally rieing water fromthe cienegp, or as flowing wells at the Red Hill.
. 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. e vatf r comes into those ducts? A These ducts are the old ohan els of gravel laid downthroui^ the fine silts, and while the friction is consider-able in these channels, the hi, her elevation of the ductsabove, where they first begin to accumulate pressure, issuch that in spite of this friction the head is sufficientto discharf^ the water as naturally rieing water fromthe cienegp, or as flowing wells at the Red Hill. The ductsare not as open as a pipe lS?ne, but they may be likenedto a pipe line filled with gravel or a flame filled withgravel, having impervious sides around it. ^ what is your opinion as to howthose strata lay,—lying horizontal, or uplifted, or in what way do they lie? A Those strata are at a point where the waters are takeninto them, upturned by reason of the uplift of somewhatmany thousand, of feet which occurred in the laain mountainrange at the end of the ohaiiQ)lain period in geolO{3r» cuid -ftliiO Ihp Rflf>nnrl;qry npliff. whinh in ihfk Rfljnft. period inien the Red Hill terrene was created, Tliat uplift created a synclinal condition between the .lain mountain range and the Hed Hill fold, which synclinal condition i s benda.^fadai±, as illustrated on the geological eections in this case, and roay be licened to an inverted siphon ,the bend being caused by the uplift, the mountains onone side and the Hed Hills on the other, and in tl:ie processof uplifting the flat layers of this ancient alluvium whichare in contact with the older rock of the foothills,would be turned upand their ends raised by that localuplift of the mountain range, A nd in that way therecent gravels would coLie down and deposit on the upturnedends of the old formation so tliKt the water passing downthrou^ the recent gravels and sinkingrawould enter theseupturn d ends much in the sam
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