paw 
Fic. 56.—View of the edge of the Krakokta glacier within the moraine seen in 
Fig. 55, showing a sloping, slightly concave border, and remarkably parallel stratifica- 
tion. 
Fic. 57.—Near view of a portion of the sloping border of the Krakokta glacier, 
showing the strong individuality of the layers, and erhaps their individuality of 
motion. 
