Abstract
Longitudinal depressions along parts of the continental platform of Norway are interpreted as formerly sub-aerially eroded fault zones, and transverse channels as relics of glaciated river valleys. Comparison is made with certain similar features which can be detected off the western coasts of Scotland and the Outer Hebrides. These are less regular and of less marked relief, and complications have been introduced by the Tertiary volcanic zone and the prevalence of NE-SW faults.
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