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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 Hudson River fjord in New York is recognized as the only true Fjord in the eastern coast of the United States [1] [2] Somes Sound, a fjard located within Acadia National Park, is often mistaken for being another fjord located along the eastern coast of the United States. [3] [4]
Fjard and fjord were originally the same word, and they generally meant sailable waterway. In Scandinavia , fjords dominate along the North Sea coast while fjards dominate the Baltic Sea coast. Fjards vs. fjords vs. förden vs. rias
When a U-shaped valley extends into saltwater, becoming an inlet of the sea, it is called a fjord, from the Norwegian word for these features that are common in Norway. Outside of Norway, a classic U-shaped valley that is also a fjord is the Western Brook Pond Fjord in Gros Morne National Park in Newfoundland, Canada.
Rands Fjord: Length 3 km. Up to 19th century it was a real bay; then a dam was built to separate it from the sea. Now the former fjord is used as a reserve of fresh water. Kolding Fjord: Length 10 km. A branch of the narrow part of the Little Belt. Haderslev Fjord: Length 15 km. The narrowest fjord. Åbenrå Fjord: Length 10 km, width 3 – 4 km.
According to the definition, fjord, Western Brook Pond and Trout River Big Pond in Newfoundland's Gros Morne National Park, are also often described as a fjords, but are actually freshwater lakes cut off from the sea, so are not fjords in the English sense of the term. Such lakes are sometimes called "fjord lakes". [27]
The "fjord" lies between the Lofoten archipelago and the Salten district of mainland Norway. The term fjord (from the old Norse fjördr meaning firth or inlet) is used in a more general way for bodies of water in the western Scandinavian languages than the more narrow usage commonly used in English. [4] [5]
The fjord starts as runoff from the Jostedalsbreen, Europe's largest mainland glacier, in the east and it flows west, emptying into the ocean just south of the Stadlandet peninsula. The mouth of the fjord lies between the large islands of Vågsøy and Bremangerlandet (with the smaller island of Husevågøy lying in the middle of the mouth).