204 WALTER HOWCHIN 
from these highlands, the most striking features are developed 
within the valley proper. The spurs of the ranges are rounded, 
truncated, and shouldered in a very characteristic manner. The 
prominent points of the piedmonts, as well as the inliers of hard 
rock showing above the glacial deposits of the valley, are strongly 
glaciated, exhibiting roche moutonnée outlines on a large scale, 
and in many places showing polished and deeply scored surfaces 
(see Fig. 4). The crag and tail outline is always present in these 
Frc. 5.—Permo-Carboniferous roche moutonnées, of quartzite (partly quarried) 
at the entrance to the Inman Valley. The intermediate country, of scrub land, con- 
sists of glacial deposits, and, in the distance, is seen the gigantic roche moutonnée of 
Crozier’s Hill. W. Howchin, photo. 
rounded hummocks. The Stossseife maintains a gradual slope 
while the Leeseite is abrupt and broken, as when “plucked” by 
ice movements. The southern entrance to the valley is marked 
by two striking roches moutonnées surrounded by glacial till with 
granite bowlders, partly exposed, up to 9 feet in diameter (see Fig. 5). 
Crozier’s Hill, 520 feet high, situated: near: the middle, of the 
valley, is another striking example of the same kind. Strangways 
Hill, a prominent spur, nearly goo feet high, on the northern side 
of the valley, was in the direct path of the glacier, but failed to 
divert its flow, as evidenced by powerfully glaciated pavements 
