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A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. [6] According to the standard model, glaciers formed in pre-glacial valleys with a gently sloping valley floor. The work of the glacier then left an overdeepened U-shaped valley that ends abruptly at a valley or trough end ...
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. Its highest elevation was Glittertinden in Norway at 2,470 m (8,104 ft) above ...
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. To the north they form the border between Norway and ...
Max. depth. 1,308 m (4,291 ft) The Sognefjord or Sognefjorden (Urban East Norwegian: [ˈsɔ̂ŋnəˌfjuːɳ], English: Sogn Fjord[1][2][3]), nicknamed the King of the Fjords (Norwegian: Fjordenes konge), is the largest and deepest fjord in Norway. [4] Located in Vestland county in Western Norway, it stretches 205 kilometres (127 mi) inland from ...
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.
Geology of Norway. 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.
The German North Sea coast. The coastline of the North Sea has been evolving since the end of the last ice age. The coastline varies from fjords, river estuaries to mudflats. The eastern and western coasts of the North Sea are jagged, as they were stripped by glaciers during the ice ages. The coastlines along the southernmost part are soft ...
Ilulissat Icefjord (Greenlandic: Ilulissat Kangerlua) is a fjord in western Greenland. Located 250 km north of the Arctic Circle, the Ilulissat Icefjord runs west 40 km (25 mi) from the Greenland ice sheet to Disko Bay just south of the town of Ilulissat. [1] Ilulissat Icefjord was declared a UNESCO World Heritage Site in 2004 because of its ...