Most of Norway is mountainous, but the mountains do not constitute a mountainous system but a series of plateaus that have a height enters 600 900 meters. The origin of the mountainous bulk must to the folding caledonio. In summary, Norway has three orographic factors of north to the south: the plateau of Finmark, the Kjolen mounts and the plateaus of the southwest and depressions of the south-east of Norway. The Galdhøpiggen mount is the highest mount of Norway and Scandinavia. The mountain ranges of Kjolen and the Dofrines form the main orographic system of Norway, which form a series of plateaus

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