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Fjord. In physical geography, a fjord or fiord (/ ˈfjɔːrd, fiːˈɔːrd / ⓘ [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]
Sound (geography) The Aldersund in Helgeland, Norway, separates the island of Aldra (left side) from the continent. In geography, a sound is a smaller body of water usually connected to a sea or an ocean. A sound may be an inlet that is deeper than a bight and wider than a fjord; or a narrow sea channel or an ocean channel between two land ...
Limestone pavement – Natural karst landform consisting of a flat, incised surface of exposed limestone. Mesa – Elevated area of land with a flat top and sides, usually much wider than buttes. Mushroom rock – Naturally occurring rock whose shape resembles a mushroom. Natural arch – Arch-shaped natural rock formation.
Scoresby Sound. 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).
Fjords and channels of Chile. Route map: The southern coast of Chile presents a large number of fjords and fjord-like channels from the latitudes of Cape Horn (55° S) to Reloncaví Estuary (42° S). Some fjords and channels are important navigable channels providing access to ports like Punta Arenas, Puerto Chacabuco and Puerto Natales.
Max. depth. 1,308 m (4,291 ft) The Sognefjord or Sognefjorden (Urban East Norwegian: [ˈsɔ̂ŋnəˌfjuːɳ], English: Sogn Fjord[1][2][3]), nicknamed the King of the Fjords (Norwegian: Fjordenes konge), is the largest and deepest fjord in Norway. [4] Located in Vestland county in Western Norway, it stretches 205 kilometres (127 mi) inland from ...
U-shaped valley with lake in Myklebustdalen, Nordfjord, Sogn og Fjordane, Norway. U-shaped valleys, also called trough valleys or glacial troughs, are formed by the process of glaciation. They are characteristic of mountain glaciation in particular. [1] They have a characteristic U shape in cross-section, with steep, straight sides and a flat ...
The fjard of Somes Sound, Maine, USA.. A fjard (Swedish: fjärd, IPA:) is a large open space of water between groups of islands or mainland in archipelagos.Fjards can be found along sea coasts, in freshwater lakes or in rivers.