Search results
Results from the WOW.Com Content Network
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]
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 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.
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.
Category: Fjords of Europe by country. 2 languages. ... Fjords of the United Kingdom (2 C) This page was last edited on 16 December 2016, at 18:12 (UTC). ...
Gabriel Escobar backpacked across 13 countries in Europe after graduating from college, taking random suggestions from people on the internet. I crowdsourced travel tips for my 3-month European ...
However the definition of ria was later expanded to other flooded river valleys regardless of the structure of the country rock. [citation needed] For a time European geomorphologists [5] considered rias to include any broad estuarine river mouth, including fjords.
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 ...