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Other low relief landforms that are only associated with fjards, such as mud flats, salt marshes, and flood plains, [1] further characterize the difference between fjords and fjards. "Förden" of the German coast and the fjords of Danish eastern Jutland together form a third type of glacial inlet. They tend to occur along older 'beheaded' river ...
In physical geography, a fjord (also spelled fiord in New Zealand English; (/ ˈ f j ɔːr d, f iː ˈ ɔːr d / ⓘ [1]) is a long, narrow sea inlet with steep sides or cliffs, created by a glacier. [2] Fjords exist on the coasts of Antarctica, the Arctic, and surrounding landmasses of the northern and southern hemispheres. [3]
A fiord is a narrow inlet of the sea between cliffs or steep slopes, which results from marine inundation of a glaciated valley. The spelling fiord is used in New Zealand rather than fjord , although all the maritime fiords instead use the word sound in their name.
Because Sund Rock is a conservation area, no hunting or gathering of any kind is permitted. Two ways exist of entering the waters in the area. One option involves a somewhat steep but short hike and surface swim of 250 to 600 metres (820 to 1,970 ft). An alternative method is to access a private beach nearby. The boundaries of the area are
In Scandinavia and around the Baltic Sea, there are more than a hundred straits named Sund, mostly named for the island they separate from the continent or a larger island. In contrast, the Sound is the common international [ 3 ] short name for Øresund, the narrow stretch of water that separates Denmark and Sweden , and is the main waterway ...
If the sill depth is deep, water circulation is less restricted, and there is a slow but steady exchange of water between the estuary and the ocean. Fjord-type estuaries can be found along the coasts of Alaska, the Puget Sound region of western Washington state, British Columbia, eastern Canada, Greenland, Iceland, New Zealand, Chile, and Norway.
Scoresby Sound (Danish: Scoresby Sund, Greenlandic: Kangertittivaq) is a large fjord system of the Greenland Sea on the eastern coast of Greenland. It has a tree-like structure, with a main body approximately 110 km (68 mi) [2] long that branches into a system of fjords covering an area of about 38,000 km 2 (14,700 sq mi).
The two fjords, among the world's longest and deepest, are considered as archetypical fjord landscapes and among the most scenically outstanding anywhere. Their exceptional natural beauty is derived from their narrow and steep-sided crystalline rock walls that rise up to 1,400 m from the Norwegian Sea and extend 500 m below sea level.