V. s. (lEOLOoicAL srr;vFY 



rrtnFEssTAyAL PArFR 1:1 n.ATE X 



A. VIKW NOinilWAUD TdWMU) ^MlrllS MKSA KltOM A I'UINT JU.ST .SdUl'H 1)K XIUCIN CITY. UTAH. 



lienohns in forBground arc llie VirKin limestoiio member of Ihe Moeakopi formiilinn. ClilVs in liinksroniid are the Mnenkopi for- 

 mation enpped by the Shiriammp cf)nf,'!om(Tale and snpportiny an outlier of the Chinle forma liuu. The wiiite Shnabkaib ahale 

 member of the !\toeiikopi forms a conspienons baTid. 



-^V 



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li. I'AiNoHAMA ALONt; KA.ST SIDE OF COAI.I'ITS WASH, NEAR GRAFTON. UTAH. 



The Shnabkaib member of the Moenkopi form.ation forms the foreground, with the upper dark-red member of the Moenkopi and 

 the Shinarump conglomerate .ilwive il Tliis is followed by the Chinle formation and the m;issive red and wliile burnssic sand- 

 stone, which forms the West 'l'i-ui[»le of the \ir;.'in (Steamboat Mountain 1 in the ba<k^'round. 



