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The Scandinavian Mountains or the Scandes is a mountain range that runs through the Scandinavian Peninsula. The western sides of the mountains drop precipitously into the North Sea and Norwegian Sea , forming the fjords of Norway , whereas to the northeast they gradually curve towards Finland .
The history of Scandinavia is the history of the geographical region of Scandinavia and its peoples. The region is located in Northern Europe , and consists of Denmark , Norway and Sweden . Finland and Iceland are at times, especially in English-speaking contexts, considered part of Scandinavia.
Scandinavian Peninsula in relation to the larger Fennoscandia. The largest peninsula in Europe, the Scandinavian Peninsula is approximately 1,850 kilometres (1,150 mi) long with a width varying approximately from 370 to 805 km (230 to 500 mi). The Scandinavian mountain range generally defines the border between Norway and Sweden.
Galdhøpiggen is the highest point in Scandinavia and is a part of the Scandinavian Mountains.. The geography of Scandinavia is extremely varied. Notable are the Norwegian fjords, the Scandinavian Mountains covering much of Norway and parts of Sweden, the flat, low areas in Denmark and the archipelagos of Finland, Norway and Sweden.
The geology of Norway encompasses the history of Earth that can be interpreted by rock types found in Norway, and the associated sedimentological history of soils and rock types. The Norwegian mountains were formed around 400 million years ago (Ma) during the Caledonian orogeny .
The overlap between the Scandinavian Caledonides and the Scandinavian Mountains has led to various suggestions that the modern Scandinavian Mountains are a remnant of the Caledonide mountains. [ 14 ] [ 30 ] A version of this argument was put forward in 2009 with the claim that the uplift of the mountains was attained by buoyancy of the ...
This is an accepted version of this page This is the latest accepted revision, reviewed on 26 January 2025. Period of European history (about 800–1050) Viking Age picture stone, Gotland, Sweden. Part of a series on Scandinavia Countries Denmark Finland Iceland Norway Sweden History History by country Åland Denmark Faroe Islands Finland Greenland Iceland Norway Scotland Sweden Chronological ...
Later in geological history, the Atlantic Ocean opened and the different parts of the orogenic belt moved apart. [1] See also Iapetus Suture and Trans-European Suture Zone . The Caledonian orogeny was a mountain-building cycle recorded in the northern parts of the British Isles , the Scandinavian Caledonides , Svalbard , eastern Greenland and ...