Abstract
The terraces of the Dale valley, south of Dalsfjord on the west coast of Norway, have been mapped and the elevations established. Five stages of downcutting have been identified, for which the evidence is discussed in detail and compared with general conclusions postulated in the literature on isostatic displacement of postglacial terraces in Norway.
GeoRef, Copyright 2004, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States
