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GFS L GEOMOOC. soy coNO TIONS <br /> The subjeet stye dies fear the canter of tho.- Valley Geomorphic P,"Awx nfifaliNcLmm This <br /> province is ehm3ctareedl by ect+ercwo- ai mfW4 derma u% ftorm rah Sierra iY--�;�Nfa i)kmatain <br /> Range which fonder the Cain 'V&Fk y to trite rmt TEte ge(AL t y of the arra a xtV.-3 ufbruad, <br /> asmlr-icing afijv l platers[EtatIrim: been dis: a ted by strwms whichdntiu die Siam Nevada <br /> Moulmein,Range, 'These mcect allu rid pdauis are undedaan by older Whnial dgmvift of <br /> Tertiary'amf age <br /> The vxmrigtzspi . sa quuetace it*IJVi- Ceatsad valley area cortsists of Fre-Tertian/bavt mens <br /> complex atvt [alta by cowmsoliaiated rorrmaatad and amarine sefimeints, Cretaccaus or Pq<ooene in <br /> mgr, uixxm oledated de pos a comprise the upper 60) to IM fed of the stratigrnpMc soxervoe <br /> baacnh the vd*a site. <br /> Suds Pmlide <br /> Bawd on the emplacaaory soil boring,so&6meatft the site appear to be eompmed primarily <br /> of Sidry .Sauafs and Sandy Silts. The.sols observed in uac explonamy sod bovig3 arc typical of <br /> "ing,xEEraveum and dimA-ba pai deposits. <br /> A w�nerad dcsoVtiun of the soil oastertith encountered is pr rented below- <br /> s. Bre%,vt 3M Sand i(SPA", <br /> This to the s dace sail This sal oras eammtr car!'at the burmg, at.. rhe <br /> fAOWtI8 deptin' <br /> DWIh <br /> P-1 <br /> B raft Sandy Sift JML) <br /> This end is described ivi danse_ This sod would be desxabed by 3orna as"hard pare' <br /> This soil was a acm Bred in rhe fello% mg Ixaruups at the 66%owing depths <br /> Dmtb <br /> P-( 5.0' -24-0' <br /> (gvuml Water eras coat cocouitered.. <br /> (2) <br />