440 HAPAKOCE: 
forms must be classed Moskusoksefjeldene (the musk-ox mountains) 
the greatest altitude of which is 578 m, and which, as shown on the 
map, form a natural continuation of Store Koldewey. 
Among landforms dating from the glacial period should still be 
mentioned the moraine deposits along the west side of Germania 
Land and Hvalsletten. | 
Generally the moraines along the ice margin consist of 
deposits with a heavy mixture of clay, which however in a few 
places, for instance at the interior of the ice fjord of Storstrommen, 
may assume the character of a wall. The deposits along the ice 
margin, as nearly everywhere in Germania Land, consist of the 
Fig. 132. From the eastern tracts of Germania Land. August. - 
ground moraine which remained after the melting of the ice. The 
peculiar characteristic of the latter is only that they are to be found 
in greater quantities than in most of the other places, that they are 
less washed out and disintegrated and less overgrown, and so generally 
speaking present a fresher and more original appearance. 
Characteristic features of the landforms along the ice margin are 
the 20—40 m high, as a rule inaccessible, wall of ice, which is nearly 
everywhere black with moraine slush, the clayey marginal lakes and 
the marginal streams. 
Northwest of Annekssoen the moraine landforms are of quite a 
peculiar character, which has been described in details and illustrated 
in “Die glaciol. Beobacht. d. Danmark-Expedition”, pp. 43—48 of the 
present volume. That which takes place at the ice margin north- 
west of Annekssgen, in the characteristic and to us so heterogenous 
landform, is the melting off of the remains of the ice streams, 
which once worked their way through the valley of Annekssoen and 
through the valleys on either side of Kap Récamier. The ground 
