Fic. 54.—A joint terminal moraine formed by the direct opposition of the Tuktoo 
glacier, which is seen on the right, and the Krakokta glacier, which is seen on the 
left. The point of view is opposite the east end of the joint moraine near the Sentinel 
nunatak looking westerly. The photograph shows the stratification of the ice and 
in some measure the upward curving of the layers near the moraine. 
Fic. 55.—View of the northeastern border of the,.Krakokta glacier seen from @ 
point near its junction with the Tuktoo glacier, looking southeasterly. A terminal 
moraine formed by the glacier occupies the right half of the foreground. On the 
left appears the lower part of the talus slope of the Sentinel nunatak. At its base 
and between it and the moraine is a stream which drains this part of the Krakokta 
and a part of the Tuktoo glacier. In the central portion of the figure the glacier is 
seen to have crept out upon its terminal moraine and to be overhanging the valley 
through which the drainage escapes to the Krakokta Cove at the head of Bowdoin 
Bay, which lies just beyond the center of the figure. The heights at the right are 
the northeastern prcmontory of the Redcliff peninsula. 
