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Kangerlussuaq occupies an alluvial flatland on the far end of the 190 km long [5] Kangerlussuaq Fjord, straddling both sides of the Qinnguata Kuussua river estuary. On the East of Kangerlussuaq is a confluence of the two major regional rivers, the Qinnguata Kuussua and Akuliarusiarsuup Kuua. The valley of the latter forms large quicksand plains.
Russell Fiord, also spelled Russell Fjord, is a fjord in the U.S. state of Alaska. It extends north to Disenchantment Bay , the terminus of Hubbard Glacier , at the head of Yakutat Bay . The fjord was named in 1901 by Marcus Baker of the U.S. Geological Survey for explorer Israel Russell , who discovered the estuary in 1891 while exploring the ...
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.
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]
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 ...
The fjord head at approximately is formed by the estuary of a river flowing from the glacial outflow lake in Johan Dahl At approximately 61°04′00″N 45°26′30″W / 61.06667°N 45.44167°W / 61.06667; -45.44167 , south of the Narsarsuaq settlement, the fjord is joined by its tributary Qooroq Fjord from the northeast, changing ...