. 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 . iiB Burrnor and next cura or?A. I havo no data to bo positive about, Q, How, you Uiink the watere that fall upon the water shedsthat foeds tlieso Vfurious 8tre<4mB, and this watrr-baaringluitd, ti^iatoTer it --tay bo, ^lether underground iviroams orothorwise, will cont* down to Uio point wiiere the cioncf^aaai)pear, so it affect lliom in eix -^OntT^^s*A. Sone, perhaps, but noty aB much aa lu wiil m a yoftr,0


. 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 . iiB Burrnor and next cura or?A. I havo no data to bo positive about, Q, How, you Uiink the watere that fall upon the water shedsthat foeds tlieso Vfurious 8tre<4mB, and this watrr-baaringluitd, ti^iatoTer it --tay bo, ^lether underground iviroams orothorwise, will cont* down to Uio point wiiere the cioncf^aaai)pear, so it affect lliom in eix -^OntT^^s*A. Sone, perhaps, but noty aB much aa lu wiil m a yoftr,0. Veil, tlon from six to twelye months the effect benumifont to tho fiurthest axtont? ?A. ^oll, tho eocond yoia in the sumner, there will be morewater fron tho rainfall th<m there will the first year aftert»!o rains, I think. ?Q, Well, tlien if v,t have a lar^^;© rainfall this season, thissetiaon wl^iich ic called 1899-1900, tlien the increase of theflow of mter will be most -Uinifest in 1901, is that i^atyou mean?. r a 1. o ?=§ -• ir < ui ~ a. a 3 8 91011121314151617 i 19JOJl 2627 28 16 A, I bolieve so; that is notjiing, *Q. Woll, uXter Uiis seuBon, if next Bouaon ..c nnvu u drouth, 80 Uuit there iB u scarcity of ra n, will it t^Jke aa loTV!; to affect tVio flow of iiie vvator in V^ cinnoraa after that yo^r of drouth, jjo (is to reducu uuw, as u hoavy rainfall did to increaoo them? ?A, If th« heaw r&infrdl had filled up the ground caitiroly, it would probably btun; at; lonr- to reduce them, if the f^round was ull. Q« r^eil, t- an, if tve h.^d a heavy rainfall this season, t-ere would bo ari xncro.^sed floi; m IVOl, and if we hi^x! a drouth next BOaBon, v^.y then, t)uit drouth would bo marufeBt in 1902, iB tiibX your neaning^ ?A, Mot to tVie furthest extent; I .avun that propor\.ion; that IB only nodifyinf?; it»; the cruek at Cucwnonf-a on the eaiit cido, ohowB the effectB of rain t?o<jn afterwtirrs^ and drainafi;e naich t;ore tlian the- c


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