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Randers Fjord: Length 30 km. Entrance from the north, branching in the south, with eastern branch. Grund Fjord: Less obstructed by sand than the main fjord. Norsminde Fjord: Hardly 3 km long. Now a lake due to silting. Horsens Fjord: Length 16 km. The entrance between the islands of Alrø and Hjarnø is called Alrø Sund. Vejle Fjord: Length 12 km.
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. Fjard and fjord were originally the same word, and they generally meant sailable waterway.
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]
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 masses, such as a strait; or also a lagoon between a barrier island and the mainland. [1] [2]
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).
The Germanic word "sound" has the same root as the verb to sunder in the meaning of "to separate". The Old Norse form of that verb is sundr. In Norway hundreds of narrow straits separating islands and combining fjords or outer parts of fjords are named "Sund". Another explanation derives "sound" from an ancient verb "sund" in the meaning of to ...
Europe has less precipitation in the east than in central and western Europe. The temperature difference between summer and winter gradually increases from coastal northwest Europe to southeast inland Europe, ranging from Ireland, with a temperature difference of only 10 °C from the warmest to the coldest month, to the area north of the ...
Fjord – a long bay with steep sides, typically formed by a glacier; Bight – a bay that is typically shallower than a sound; Sound – a large, wide bay which is typically deeper than a bight, or a strait; Cove – a small, typically sheltered bay with a relatively narrow entrance