541 
of Edinburgh^ Session 1865-66. 
moraine at Fondalen is a further proof that when the ice formerly 
filled the valley, its surface received abundant detritus from the 
mountain slopes on either side. 
Opposite Fondalen, the Holands Fjord, passing through a deep 
and narrow channel on its northern bank, trends in an east-north-eas- 
terly direction, but just before taking this course, it sends eastward 
Fig. 4. — Sketch-map of lower end of larger Glacier, Fondalen. 
r 
1. Holands Fjord. 2. Small lake at end of glacier. 3. Glacier. 4. Alluvial plain rising into 
moraine mounds as it approaches the foot of the glacier. 5. Line of marine terrace or “ raised 
heach,” about 250 feet above sea-level. 6. Present course of stream. 7. Old course of stream. 
a bay which terminates at the mouth of a valley about a mile above 
the hamlet. This valley is considerably larger than that just de- 
