SMITIISOXJ AX M ISCELLAXKOLS COLIJXTIOXS 



VOL. 72 



The character of the motmtains aljout the liead-waters of the 

 jNIiddle Fork of the Saskatchewan is ilKistrated hy figure 2. where a 

 glacial stream flows out through a dee])]}' eroded valley Avith high 

 ridges and ])eaks rising in stee]) slopes and cliti's. The ])osition of 

 the camp in Glacier Lake canyon is shown in figure 3. and the outlook 

 to the west toward the glacier from the cam]) l)v tigure 5, and to the 



Fig. 2. — View looking up the Middle Fork (Howse River) of the Sas- 

 katchewan River to Howse Pass (5,000') on the Continental Divide. 



hi the distance Ijeyond Howse Pass the peaks of the Van Home Range 

 and Mount Vaux of the Ottertail Range, and on the right and ahove the 

 Pass Mount Conway, and to the extreme right the eastern ridge of Mount 

 Outram. 



Locality. — View taken from the upper slope of Survey Peak ahove 

 Glacier Lake, about 48 miles (76.8 km.) northwest of Lake Louise station 

 on the Canadian Pacific Railroad, Alberta, Canada. 



Photograph by Air. and Mrs. C. D. Walcott, 1919. 



east hy figure 4, where the dark massive hulk of Blount Murchison 

 rises in clifTs ahove the can\on of the Alistaya l\i\'er along which the 

 trail from Bow Pass descends. 



The measured geological section hegins at the foot of the ridge 

 at the extreme left of figure i, and was measured in the clitts and 

 slopes, and thus carried to the side of the ?\lons glacier shown in 



