A 

 eooo'- 



North Tintic Anticline 



Hannifin PeaK 



Tintic Syncline 



6000'- 

 4000'- 

 2000' ■ 



Pinyon Peok 



Cm | 



Cm Jj Um 



.* "^Inferred position and relotions 

 of Allen's Ranch thrust fault 



A 



-»ood 



eood 



-*ood 



20O0' 



Fig. 22.24. Cross section of the East Tintic Range. By Morris, Disbrow, Lovering, and Proctor. Reproduced 

 from Morris, 1957. Section 19, Fig. 22.1. 



LION HILL THRUST 

 Cw, 



BUTCH PEAK 



pCsIs 



p€slq 



/- v V';4i l \0 - - - _ _ - T ar _ . 







lo?^^^^-= pC " QTp 9, 



FAULT 



OTpj 



/_\ /_\ /> / 

 rwwO 



"/ "/ w \" 



V/\/\,\AT/T'.— .— » 



'S'S'S'S'Z'. Tm" 



"-'- f„- / ,-„'V.-.,-.. - -5»'-C,," M '"' f POSITION OF SHEEPROCK THRUST^ 

 ' -. - .-^— T.^—. - -\"yt- — ^ PRIOR TO INTRUSION 



Fig. 22.25. Cross section of the Sheeprock Mountains. After Cohenour, 1959. Section 18, Fig. 22.1. 



Pk 



G/endale thrust fragment 



Ths Tmc 



iooo' datum 



PK * -ftm ' T?m KTof 



G fen dole thrust 



WiJ/owTank thrust KTof 

 J a ~) Kwt 



Fig. 22.26. West to east sections through northern Muddy Mountains, after Longwell, 1949, 

 showing Glendale and Willow Tank thrust sheets. Glendale thrust sheet is made up of Cambrian 

 to Pennsylvanian strata. Prb, Permian red beds; Pk, Permian Kaibab Is.; "Em, Moenkopi fm.; lis, 



Shinarump congl.; Tic, Chinle fm.; Ja, Aztec ss.; Kwt, Willow Tank congl.; Kb, baseline ss.; Ktof, 

 Overton fm.; Ths, Horse Spring fm.; Tmc, Miocene (?) Muddy Creek fm. Section 20 of Fig. 22.2. 



