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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 .
All the peaks are to be found in 14 topographical maps (Norge 1:50000) published by the Norwegian government cartography office, of which 21 peaks are in 1518 II Galdhøpiggen, 18 in 1618 III Glittertinden, and 13 in 1617 IV Gjende. The northernmost is in the Dovre area, meaning there are no 2000 m peaks in northern Norway, even though there ...
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.
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 Scandinavian mountains includes the largest glaciers on the European mainland (Jostedalsbreen, Svartisen), Northern Europe's highest mountains (Jotunheimen) and largest mountain plateau. The mountain chain itself creates a rain shadow, and the eastern part of the mountain chain receive less precipitation than the western part. The ecoregion ...
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.
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.