SMITHSONIAN MISCELLANEOUS COLLECTIONS NiO, (6) 
By) 
and early fall of 1916 in field investigations on the Continental 
Divide forming the boundary between Alberta and British Columbia, 
Fic. 2.—Cliffs of massive bedded quartzites at north end of ridge of Wedg- 
wood Peak rising 2,000 feet (609.7 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, 1910. 
south of the Canadian Pacific Railway. The very heavy snowfall 
of the previous winter together with frequent snow and rain squalls 
