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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 Gudbrandsdalen valley includes the most arid area in Norway. At Skjåk the average annual precipitation is only 278 millimetres (10.9 in). [12] The valley sits in the rain shadow of the mountains west (including Jotunheimen), north, and east of the valley. [13] The valley is less incised than the valleys of western Norway. [14]
Geological Survey of Norway (Norwegian: Norges geologiske undersøkelse), abbreviation: NGU, is a Norwegian government agency responsible for geologic mapping and research. The agency is located in Trondheim with an office in Tromsø , with about 200 employees.
The routes cover 1,850 kilometres (1,150 mi) and are located along the West Coast, in Northern Norway and in the mountains of Southern Norway. [2] The authorities have coordinated the establishment of accommodation, cultural activities, dining, sale of local arts and crafts, and natural experiences along the tourist roads. [2]
The Caledonian Wilson cycle commenced with the continental break-up of Rodinia [17] and the opening of the Iapetus ocean about 616–583 Ma ago. [18] [19] [20] The Iapetus was at its widest in the Late Cambrian–Early Ordovician [21] [1] before it began to close by subduction of Iapetus oceanic crust along the Gondawanan and Laurentian margins starting between 500 and 488 Ma ago.
This page was last edited on 11 January 2022, at 01:48 (UTC).; Text is available under the Creative Commons Attribution-ShareAlike 4.0 License; additional terms may apply.
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