THE QUEEN'S RIVER MORAINE 



697 



which has formed in the lower part of the hollows and not from 

 the soil proper of the surface on which the belt rests. One large 

 oak has grown out of a crevice in a large bowlder, with a result 

 in the end fatal to the tree. 



Fig. 5- — View of the Queen's River moraine. " Cat Rocks," from the intra- 

 glacial field north of it, looking at the inner edge of the bowlder wall and showing the 

 line along which the mural (?) front of the glacier stood. 



The bowlders in many places along the frontal aspect of the 

 moraine, as shown in Fig. 5, exhibit a mode of piling which 

 seem to the writers accountable only on the supposition of 

 addition from the north. Some of the bowlders may owe their 

 peculiar orientation to a slight forward shoving movement. The 

 general scheme of arrangement is shown in the annexed dia- 



