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Thse selb"mc ske bm near the,=Mw ortlre V'ml0cir f3cimx-obwc Province OrC� This <br /> prmvinr-e is,-baokcmwizcd by tmusa m Mr ramal degsxsits trema tk-'Sierns Nevada�N€r7rtn.aatr, <br /> KAaSc,8[uc#t Mede'the Great V'aWey to the-a%, '1'��erako�y 01 e he area est sis s ur."txx3ae. <br /> uxvWsctng a91tavW phains that have bean domtedi.shy weanaf srtvch draur rise Sierra Nlevaddra. <br /> �khxtxda rt Rmmge. These reoml alrvitl plrims ant uaraerWm by older alluvial d•Wotsias of <br /> TeaEiary arad t MaatCFMJry age <br /> Che stradg aplac wquence in tlrs Ceattal Vak-f area coct%sVs of a pie=Te¢taa¢y bEw'W-tnr. <br /> :s gplex ovedawn bN canwAdataed rod and memrine wbin erYs, Cretacecsus Of F kQQerne is <br /> age, im-i sofidatd dcpasirs amapnw tate upper 600 to 800 fact orthe stratigraphit; vtigvrc+xr <br /> bAvunth rax:mlt w site. <br /> Sods'Pro tie <br /> Basel err'txe exploraofy arnil llmvvyia, enols benrcath ttv--site appear to be cwiposoxl pafimeranlw <br /> or Sandy Sim acrd`lands. I[v-soils obsvwed in our cr ihrorutorysoil barings we r"-til car' <br /> ;nn A-Eviu m and tIaxxd-1 a.drr depo!%ift <br /> A description orths;soil maeteriarts encountered is preventedbdaw- <br /> as.. Bnasvn 5Hcu1p Sih (lVCL; <br /> 'T1ti3 is the surouse:so I. 'This soul eras a membered in the rollowitag borirW at alae <br /> CbRo+ ing depths: <br /> Be oPloth <br /> P_1 0.01 -3-51 <br /> P-2 0-0'-4_5' <br /> R Tan.'Sandy Srik (ML) <br /> This wN is dcswb*i,zs dater:. This sM waaW be descr6 d by snare m"dyad pae- <br /> Tics sail ceras eaavn named in d6c ioHoaiog bmiqp at the 6siowing depths- <br /> BDCOA <br /> P--1 3.S' -24.0' <br /> P_2 t2-O' - 151' <br /> (2) <br />