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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]
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.
"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 channels and open into the tideless Baltic sea. Rias are drowned valleys, such as the estuaries of Thames, Severn and Humber and the firths of Tay and Forth.
The Lim estuary has the appearance of a canyon. The side rises to 150 m, sinking to 20 m when they reach the sea; they are overgrown with maquis and have some special characteristics. The south bank, facing the north, is covered with deciduous trees ( oak and ash ), while the north bank, facing the sun, has more evergreen flora.
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, covered with the remains of deposited glacial sediment, which was left directly by the ice or has been redeposited ...
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]