GLACIAL STUDIES IN (GREE NIEAND: 673 
of the glacier. A view from the southeast would show a very 
similar face and the two combined would make up the extended 
terminal curve of the ice lobe. Fig. 46 is a nearer view in 
the middle of the valley, and Fig. 47 is a still nearer one on the 
Fic. 47. Portion of front wall of South Point glacier near center of valley, seen 
looking northwesterly. The dark shading brings out prominently the stratification of 
the upper part, which is obscure in most of the views presented, because of the light 
color of all parts. The dark layer at the base and the talus slope are continuous with 
those of the preceding figure. 
southeast face, looking in the reversed or northerly direction. 
These views, particularly Fig. 47, show the pronounced stratif- 
cation of the glacier, the presence of débris between the layers, 
the development of a vertical and even overhanging face, and 
the formation of a notable talus slope in front. The stratifica- 
tion is much the same as that of the Bryant glacier, but more 
regular and pronounced in the upper portion where the débris is 
slight. It is worthy of note that these lines of stratification appear 
upon the upper surface also and may be traced consecutively 
