Fjords of Norway

Thursday, 16 August 2012

Geologically, a fjord is a long, narrow inlet with steep sides or cliffs, created in a valley carved by glacial activity. The word comes to English from Norwegian, but related words are used in several Scandinavian languages - in many cases to refer to any long narrow body of water, rather than the more specific meaning it has in English. The island of Greenland in particular has many fjords. A fjord is formed when a glacier cuts a U-shaped or oblong valley by abrasion of the surrounding bedrock. Glacial melting is accompanied by rebound of Earth's crust as the ice load and eroded sediment is removed (also called isostasy or glacial rebound). In some cases this rebound is faster than sea level rise.


 Fjords of Norway
 Fjords of Norway
 Fjords of Norway
Fjords of Norway

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