A preliminary study of Lofoten as a potential World Heritage Site based on natural criteria
(Forkortet)\rThe geology of the Lofoten region has been described with the aim of assessing whether or not the area would qualify as a candidate for the World Heritage List based on its natural properties.\rThe Lofoten archipelago consists mainly of Palaeoproterozoic rocks, including paragneisses an...
Main Authors: | , , , , |
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Format: | Report |
Language: | English |
Published: |
2005
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Subjects: | |
Online Access: | https://hdl.handle.net/11250/2664958 |
Summary: | (Forkortet)\rThe geology of the Lofoten region has been described with the aim of assessing whether or not the area would qualify as a candidate for the World Heritage List based on its natural properties.\rThe Lofoten archipelago consists mainly of Palaeoproterozoic rocks, including paragneisses and younger plutons (ca 1800 Ma) of the anorthosite-mangerite-charnokite-granite (AMCG) suite. The Precambiran basement of the Lofoten and the adjoining Vesterålen islands is part of a NNE-trending basement high that is overlain to the east by a stack of allochthonous nappes occupying the central axis of the Scandinavian Caledonides. 52637 |
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