Fjord Og Kystcentret
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Fjord Og Kystcentret
In physical geography, a fjord (also spelled fiord in New Zealand English; ) is a long, narrow sea inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Antarctica, the Arctic, and surrounding landmasses of the northern and southern hemispheres. Norway's coastline is estimated to be long with its nearly 1,200 fjords, but only long excluding the fjords. Formation A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. 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. Such valleys are fjords when flooded by the ocean. Thresholds above sea level create freshwater lakes. Glacial melting is accompanied by the rebounding of Earth's crust as the ice load and eroded sediment is removed (also called isostasy or glacia ...
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Geirangerfjord (6-2007)
or is a fjord in the Sunnmøre region of Møre og Romsdal county, Norway. It is located entirely in Stranda Municipality. It is a branch off the Sunnylvsfjorden, which itself is a branch off the Storfjorden (). The small village of Geiranger is located at the end of the fjord where the Geirangelva river empties into it. The fjord The fjord is one of Norway's most visited tourist sites. In 2005, it was listed as a UNESCO World Heritage Site, jointly with the Nærøyfjorden as the " West Norwegian Fjords" site. This status was challenged by the disputed plans to build power lines across the fjord. The Geiranger - Hellesylt Ferry, a car ferry which doubles as a sightseeing trip, is operated by Fjord1 Nordvestlandske. It runs lengthwise along the fjord between the small towns of Geiranger and Hellesylt. The fjord is scheduled to require zero-emissions ships in 2026. Along the fjord's sides there lie a number of now-abandoned farms. Some restoration has been made ...
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