cross-cuts the southern slope. It is in the continuation of the river Festningselva that drains the glacier Vardebreen (Figure 1C). Svensksunddjupet is surrounded by drainage areas with 56 % gla-cier cover in the north and 16 % in the south (Hagen et al., 1993). The drainage areas have alpine morpho...
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1031.4233 http://hol.sagepub.com/content/17/6/707.full.pdf |