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The Lofoten Drift, Norwegian Sea
Geological Society, London, Memoirs, 2002Abstract The Lofoten Contourite Drift is located below c . 1000 m water depth on the continental slope off northern Norway. It has a maximum thickness of about 360 m and correlation to published seismic stratigraphy implies a Neogene age.
Jan Sverre Laberg +2 more
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The Andøya Canyon, Norwegian Sea
Geological Society, London, Memoirs, 2016The relatively steep continental slope offshore north Norway (3–7°) is dissected by several valleys (e.g. Taylor et al. 2000; Rise et al. 2013), none of which is related to coastal rivers opening into the fjords dominating the coast (Corner 2005). Two end-member valley forms have been identified: (1) classical submarine canyons characterized by a V ...
J. S. Laberg +2 more
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Norwegian-Greenland Sea thermal field
Geological Society, London, Special Publications, 2000Abstract Thermal gradient and thermal conductivity measurements carried out in the Norwegian-Greenland Sea and in the western Eurasia Basin from 1967 to 1996 have yielded 436 heat-flow values which have been stored on a UNIX-platform database, heat , to facilitate retrieval, documentation and display.
Eirik Sundvor +3 more
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1990
Abstract Generation of oceanic crust at the boundary between the Greenland/North American and the northwestern part of the Eurasian plates has created the Norwegian-Greenland Sea. This relatively young ocean comprises a number of separate basins, plateaus, and ridges revealing that the break-up and separation of the two major plates have
Olav Eldholm +3 more
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Abstract Generation of oceanic crust at the boundary between the Greenland/North American and the northwestern part of the Eurasian plates has created the Norwegian-Greenland Sea. This relatively young ocean comprises a number of separate basins, plateaus, and ridges revealing that the break-up and separation of the two major plates have
Olav Eldholm +3 more
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Norwegian Sea ecoregion – fisheries overview
2019The largest landings in this ecoregion are by Norway, the Russian Federation (Russia henceforth), Faroe Islands, and Iceland, mainly by pelagic fisheries. Other nations also have fisheries in the area. The number of fishing vessels is declining while the size of the remaining vessels is increasing.
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Weichselian land-sea interactions: Western Norway-Norwegian sea
Quaternary Science Reviews, 1990Abstract Six major Weichselian glacier expansions (including the Younger Dryas) are recorded in western Norway. Three of the advances reached the continental shelf while the others were restricted to the coastal areas. During the Upper Weichselian glacial maximum (18–20 ka) there was an ice-free corridor between the British and the Scandinavian ice ...
Eiliv Larsen, Hans Petter Sejrup
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Barents Sea and the Norwegian Sea ecoregion overviews
2022This Section has not been updated in 2011.
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Sea surface temperature mapping flights—Norwegian sea, summer 1968
Remote Sensing of Environment, 1970Abstract Sea surface temperature mapping flights were carried out with Naval Oceanographic Office research aircraft from April 1968 through September 1968. These flights, carried out in the interest of the Icelandic herring fishery, defined the boundary between the tongue of polar water projecting southward to the east of Iceland and the warmer ...
V.E. Noble, J.C. Wilkerson
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Southern Norwegian Sea Surveys.
1995Abstract : The study of processes of crustal formation and the structural and morphologic expression of seafloor created at mid-oceanic spreading centers is a focus of research by marine geologists, geophysicists and acousticians, and is of direct relevance as well to studies of physical oceanography, marine chemistry, and marine biology.
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