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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]
The branches of Sognefjord are much shallower than the main fjord. The mouth of Fjærlandsfjord is about 400 meters (1,300 ft) deep while the main fjord nearby is 1,200 meters (3,900 ft) deep. The mouth of Ikjefjord is only 50 meters (160 ft) deep while the main fjord is around 1,300 meters (4,300 ft) at the same point. [8]
Fjord (fiord) a narrow inlet of the sea between cliffs or steep slopes. [27] Scandinavian Gill or Ghyll: a narrow stream or rivulet; brook; narrow mountain stream. [31] The north of England and Kent and Surrey influenced by Old Norse; The variant "ghyll" is used in the Lake District and appears to have been an invention of William Wordsworth ...
The Grand Canyon, Arizona, at the confluence of the Colorado River and Little Colorado River.. A canyon (from Spanish: cañón; archaic British English spelling: cañon), [1] gorge or chasm, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. [2]
Coastal zones are regions where interactions between terrestrial and marine processes occur. Compare shore. coastal bench See wave-cut platform. col. Also gap or notch. The lowest point on a mountain ridge between two peaks. colatitude The complementary angle of a given latitude; i.e. the arithmetic difference between 90 degrees and the given ...
It’s true that Diablo Canyon has been running for roughly 40 years without a major incident — but that’s no guarantee there won’t be a major earthquake or another catastrophe in the future.
A certain kind of inlet created by past glaciation is a fjord, typically but not always in mountainous coastlines and also in montane lakes. Multi-arm complexes of large inlets or fjords may be called sounds, e.g., Puget Sound, Howe Sound, Karmsund (sund is Scandinavian for "sound").