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The fjords in Finnmark in Norway, which are fjords in the Scandinavian sense of the term, are not universally considered to be fjords by the scientific community, [38] because although glacially formed, most Finnmark fjords lack the steep-sided valleys of the more southerly Norwegian fjords. The glacial pack was deep enough to cover even the ...
Although fjards and fjords are similar in that they are a glacially-formed topography, they still differ in some key ways: Fjords are characterized by steep high relief cliffs carved by glacial activity and often have split or branching channels. Fjards are glacial depressions or valleys that have much lower reliefs than fjords.
The fjords of western Norway formed in connection to the east-ward tilting of much of Norway during the Cenozoic uplift of the Scandinavian Mountains. This uplift, that occurred long before the Quaternary glaciations , enabled rivers to incise deeply the Paleic relief.
Fjords are particularly common on the coast of Norway. [6] [7] [8] Firths are similar to fjords, but are generally shallower with broader bays in which small islands may be found. [9] The glaciers that formed them influenced the land over a wider area and scraped away larger areas. [10] Firths are to be found on the Scottish coast. [11]
Coniston Water illustrates a typical fjord lake profile with length exceeding width by a factor of 10.. Some freshwater lakes which have formed in long glacially-carved valleys with extensive overdeepening and often with terminal moraines blocking the outlet are called fjords or "fjord lakes" (which follows the Norwegian fjord-naming convention). [3]
The Geiranger Fjord [1] [2] [3] (Norwegian: Geirangerfjorden) is a fjord in the Sunnmøre region of Møre og Romsdal county, Norway. It is located entirely in the Stranda Municipality . It is a 15-kilometre-long ( 9 + 1 ⁄ 2 mi) branch off the Sunnylvsfjorden , which is a branch off the Storfjorden (Great Fjord).
The fjords of western Norway formed in connection to the east-ward tilting of much of Norway during the Cenozoic uplift of the Scandinavian Mountains. This uplift, that occurred long before the Quaternary glaciations, enabled rivers to incise deeply the Paleic relief.
The fjord was carved by the action of glaciers in the ice ages and was flooded by the sea when the later glaciers retreated. The geology of Lysefjorden was thoroughly investigated and described by Professor Bjørn G. Andersen in his Master's thesis (1954) "Om isens tilbaketrekking i området mellom Lysefjorden og Jøsenfjorden i Ryfylke" (On the glacial retreat in the area between the ...