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Geological Formation

Svalbard

Structural and Tectonic Formations

Svalbard is a Norwegian archipelago in the high Arctic, positioned where the Arctic Ocean meets the Atlantic roughly halfway between mainland Norway and the North Pole. Its largest island, Spitsbergen, covers about 37,673 square kilometers, with Nordaustlandet, Edgeoya and Barentsoya among the other principal islands. About 60 percent of the archipelago is covered by glaciers, the largest being Austfonna, and repeated ice ages have carved the ancient plateau into mountains and fjords, including the highest peak, Newtontoppen, at 1,717 meters. Svalbard forms part of the High Arctic Large Igneous Province and remains seismically active, having recorded the strongest known earthquake in Norway there in 2009. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Facts
Classification
Protected Status
National Park or Reserve 1
Connections

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Svalbard

Long-Form Articles

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Same As

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Source Svalbard (Wikipedia)Lead section
Quote, Lead section
Svalbard (US: SVAHL-bar(d), UK: also SVAL-, Urban East Norwegian: [ˈsvɑ̂ːɫbɑr]), formerly Spitsbergen or Spitzbergen, is a Norwegian archipelago that lies at the convergence of the Arctic Ocean with the Atlantic Ocean.

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Source Wikidata: Svalbard
Sources
1. Wikidata: Svalbard
  • Wikidata Q25231, class allow-list match (w-wdresolver-0926)
  • Seven national parks and 23 nature reserves cover two-thirds of the archipelago
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Svalbard (Wikipedia)
Lead section
Quote, Lead section
Svalbard (US: SVAHL-bar(d), UK: also SVAL-, Urban East Norwegian: [ˈsvɑ̂ːɫbɑr]), formerly Spitsbergen or Spitzbergen, is a Norwegian archipelago that lies at the convergence of the Arctic Ocean with the Atlantic Ocean.
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