SMI 



THSONIAN MISCELLANEOUS COLLECTIONS 



VOL. 75, NO. 5, PL. 100 



Fig. I. — Panoramic view from Shio Point, looking southeast down Moose River Valle)-. The strata of Tah Mountain on tlie riglit of the Pass are of Lower Canihrian age, and those 

 of Tokana Mountains on the left, of Upper Cambrian age. A fault line with a throw of about 9,000 feet (2,743.2 m. ) has thrust the Lower Cambrian over the Upper Cambrian on the 

 line of the Pass. 



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Fig. 2.-Panoramic view of Tah Peak, Mahto Mountain (Ma), and Calumet Creek (C). Tah Peak slopes to the northwest merging into Mahto Mountain (Ma) Xl-l^^(°Mr^' Ind 

 distance are Lynx Mountain (Z,), Titkana Peak (7). and Robson Peak (R). On the right, Calumet Creek (C), Mumm Peak (M), to the right of the Peak Mural glacier (MG), and 

 Gendarme Mountain {G). At the lower left is Moose Pass (MP). 



Locality.— Shio Point is 11 miles (17.7 km.) north-northeast of the summit ni Robson Peak. 

 Peak District, Jasper Park, Alberta, and Pjritish Columbia. 



It overlooks Aloose Pass to the south and the headwaters of Calumet Creek, Robson 



