Proc. Roy. Socy. of Edin.] 
[Yol. XXX. 
Fig. 43. — Loch Dungeon from the north-west side, looking east, showing the burn 
from the North Garry top entering the loch. The flat foreground on either 
side of the burn is an alluvial cone, and consists of detrital gravel from a 
large moraine through which the burn has cut its way. Previous to this 
reduction there must have been another loch of considerable extent, because 
the moraine formed a dam across the glen through which the burn flows. 
Fig. 44. — Loch Dungeon from the north-east corner, looking south towards 
Meikle Millyea, showing the large association of Phragmites communis at 
this corner of the loch. 
Mr George West. 
[Plate 22 . — Referred to on page 125. 
