Geology Of Svalbard
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Geology Of Svalbard
The geology of Svalbard encompasses the geological description of rock types found in Svalbard, and the associated tectonics and sedimentological history of soils and rocks. The geological exploration of Svalbard is an ongoing activity, and recent understandings may differ from earlier interpretations. Geological Basement Geological basement dated from Precambrian, Cambrian, Ordovician and Silurian, originally termed ''Hecla Hoek'', is found in three different provinces. The southwestern terrain comprises Prins Karls Forland, Oscar II Land, Nordenskiöld Land west of Grønfjorden and Wedel Jarlsberg Land . The northwestern terrain includes Haakon VII Land and Albert I Land. The northeastern terrain comprises Nordaustlandet and the northeastern parts of Spitsbergen. Devonian Devonian age sediments are exposed in Andrée Land, James I Land and Dickson Land. Orogeny took place in late Devon. Carboniferous and Permian During Carboniferous and Permian, rift basins were formed. Car ...
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Svalbard Geology V2
Svalbard ( , ), also known as Spitsbergen, or Spitzbergen, is a Norwegian archipelago in the Arctic Ocean. North of mainland Europe, it is about midway between the northern coast of Norway and the North Pole. The islands of the group range from 74° to 81° north latitude, and from 10° to 35° east longitude. The largest island is Spitsbergen, followed by Nordaustlandet and . The largest settlement is Longyearbyen. The islands were first used as a base by the whalers who sailed far north in the 17th and 18th centuries, after which they were abandoned. Coal mining started at the beginning of the 20th century, and several permanent communities were established. The Svalbard Treaty of 1920 recognizes Norwegian sovereignty, and the 1925 Svalbard Act made Svalbard a full part of the Kingdom of Norway. They also established Svalbard as a free economic zone and a demilitarized zone. The Norwegian Store Norske and the Russian remain the only mining companies in place. R ...
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