SMITHSONIAN MISCELLANEOUS COLLECTIONS 



VOL. 75, NO. 5, PL. 32 



Fig. I. — Looking north over Johnston-Wild Flower Canyon Pass. The high point on the left is the upturned northeastern 

 side of the Castle Mountain syncline ; it is formed oi Middle and Lower Camlirian strata thrust over the Canadian (Sarhach 

 beds) in the pass. The ridges on the right of the pass are formed of L'pper Camljrian and Ozarkian beds (see lig. 25). 



Locality. — .About () miles (9.7 km.) southeast of F on map, plate 2f). .^t the head of Johnston Creek, 12 miles (19.3 km.) 

 (.•:isl-soiitheast in an air line from Lake Louise Station, and 22 miles (35.4 km.) northwest of IBanff, Alberta, Canada. 



Fig. 2. — Upturned Canadian (Sarbach), Ozarkian (Mens), Cambrian (Bosworth and Eldon), and Devonian (Messines) formations southwest of Badger Pass. Ai the left, the 

 Middle Cambrian Eldon limestones have been pushed over the Devonian. 



Lo(-a/;7.v.— About 9 miles (14.5 km.) southeast of F on map, plate 26. Southeast side of canyon leading up from Johnston Creek to Badger Pass in Sawback Range. Position 

 of camera about 10 iniles (16.1 km.) in air line east of Lake Louise Station, and 16 miles (25.7 km.) northwest of Banff, .Alberta, Canada. 



