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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 .
Norway is a country located in Northern Europe in the northern and western parts of the Scandinavian Peninsula.The majority of the country borders water, including the Skagerrak inlet to the south, the North Sea to the southwest, the North Atlantic Ocean (Norwegian Sea) to the west, and the Barents Sea to the north.
The northernmost is in the Dovre area, meaning there are no 2000 m peaks in northern Norway, even though there are some almost 2000 m there, and some above 2000 m in Sweden near the border. Most of the difficult summits were ascended in the late 19th and early 20th century by a combination of Norwegian explorers, local guides (in particular the ...
The geography of Norway is dominated by vast mountain ranges broken up by valleys and fjords. Less than 10% of the country's area is arable , and the rest is mountainous. Glaciers are the major cause for erosion, so the terrain in the Norwegian mountains consists of plateaus and lakes with peaks.
The Scandinavian mountain range generally defines the border between Norway and Sweden. Its highest elevation was Glittertinden in Norway at 2,470 m (8,104 ft) above sea level, but since the glacier at its summit partially melted, [ 5 ] the highest elevation is at 2,469 m (8,100 ft) at Galdhøpiggen , also in Norway.
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.
Geological map of Fennoscandia. 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.
Jotunheimen (Norwegian pronunciation: [ˈjôːtʉnˌhæɪmn̩]; "the home of the Jötunn") is a mountainous area of roughly 3,500 square kilometres (1,400 sq mi) [3] in southern Norway and is part of the long range known as the Scandinavian Mountains.