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<br /> <br />co <br /> <br /> <br />!~XPL^N^'nON <br /> <br />D...7~':; ... <br />.. . .. <br />.". " <br /> <br /> <br />CEn <br /> <br />SANDSTONE. MUDSTONE, AND <br />SliM.!: OF TERTIAx.Y A(ii: <br /> <br />S/\NI>STONI:, MUDSTONI', AND <br />SIIALE Of: CRI'TAC! ':OUS ,-\(;J ': <br /> <br />SAt~DSTONI:. L!\II':STllNI:" <br />.(,HI..\KT7:ITI', 1\1\1> SIIAI.l' 01' <br />I'ALI:UZOIC ;\(iE <br /> <br />GNEISS AND SCHIST 0;; PRY- <br />CAMBRIAN At,!: <br /> <br />CONTACT <br /> <br />~I <br /> <br />~, <br /> <br />~i <br /> <br />o <br />I <br />o <br /> <br />\\i:'.' <br /> <br />10 <br />I <br />I <br />20 <br /> <br />20 30MILES <br />I I J <br />30 KILOMETERS <br /> <br />.- <br />10 <br /> <br />Figure ?--(ielleralizc<.l bedrock geologyof the Yampa River basin (adaple<.l <br />from Steele and others, !lJ7X,. Formations of similar litlllllogy and age <br />have been grouped (0 form IInils with similar l~rodibiJity. <br /> <br />~ <br /> <br /> <br /> <br />