344 TRANSACTIONS OF THE CANADIAN INSTITUTE. [Vou. VII. 
In the neighborhood of Clear Lake there are morainic hills rising 
from 35 ft. to a much higher elevation in the distance, and low sand plains 
from 6 ft. to 10 ft. above the lake, while around Wendigokan the sand 
plains rise from 15 to 30 ft. above that lake. To the north of the latter 
green schist hills rise about 125 ft. and to the westward 175 ft. above its 
surface, while to the south moraine covered hills reach an elevation of 
Lower Falls in Long Rapid on Sturgeon River. 
from 80 to 240 ft. Much swamp and many small lakes lie to the south 
of Wendigokan. 
Watson or Rocky Lake, as the latter name might indicate, lies in a 
rocky hollow surrounded by green schist hills, which are rather low on 
the south side, but on the north have an elevation of about 135 ft. above 
the lake. This lake drains south-westward, and probably by Sand Creek. 
There is little difference in the elevations of Watson, Wendigokan and 
Tallon Lakes. 
' The country as a whole is not nearly so rough as most of the region 
nearer the coast of Lake Superior, and it seems to grow less rough towards 
