SMITHSONIAN JNIISCEI.I.ANEOUS COLLECTIONS 



\I)L. 66 



and early fall of 1916 in field investigations on the Continental 

 Divide forming the boundarv between Alberta and Uuitish Columl)ia. 



Fig. 2. — -Cliffs of massive bedded quartzites at north end of ridge of Wedg- 

 wood Peak rising 2.000 feet (6097 m.) above the small lake in foreground. 

 Note the enormous fans at the base of the cliff, as well as the geological 

 structure of the rock wall above. Photograph by Walcott, 1916. 



south ot the Canadian Pacific Railway. The very heavv snowfall 

 of the ])revi()us winter together with freijuent snow and rain sfjualls 



