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Geology and Crustal Structure of the Faeroe Islands - A Review

  • P. Hedebol Nielsen
Part of the Nato Conference Series book series (NATOCS, volume 8)

Abstract

The Faeroe Islands consist of plateau basalts extruded during the opening of the Norwegian-Greenland Sea in the early Tertiary. On the shelf outside the 200 m contour line the basalts are overlain by sediments reaching a thickness of 2 km. The shelf is separated from the Iceland-Faeroe Ridge by a scarp with a gravimetric anomaly, and the Faeroese crust has lower velocities (6.2 km/s or less) than the crust of the ridge (6.7 km/s). The Faeroese crust is more than 25 km thick and is probably continental.

Keywords

Bouguer Anomaly Faeroe Island Plateau Basalt Reykjanes Ridge Lava Pile 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Springer Science+Business Media New York 1983

Authors and Affiliations

  • P. Hedebol Nielsen
    • 1
  1. 1.Faeroe BranchGeological Survey of DenmarkThorshavnFaeroe Islands

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