• Corpus ID: 226225485

Deep weathering, neotectonics and strandflat formation in Nordland, northern Norway

@inproceedings{Olesen2014DeepWN,
  title={Deep weathering, neotectonics and strandflat formation in Nordland, northern Norway},
  author={Odleiv Olesen and Halfdan Pascal Kierulf and Marco Br{\"o}nner and Einar Dalsegg and O. Fredin and Terje Solbakk},
  year={2014}
}
The strandflat as a geomorphological element was defined by Reusch (1894). The timing and mechanism of its formation have been discussed at great length over the last century. The strandflat is mainly developed between Stavanger and Magerøya in Finnmark (Holtedahl, 1998) and its width varies from 50–60 km along parts of the Nordland and Møre coasts to more or less zero in the Stad area (Fig. 1). The strandflat is an uneven and partly submerged bedrock platform extending seawards from the… 

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