Geologically, a fjord (// or i//; also spelt fiord) 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 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. Most fjords are deeper than the adjacent sea; Sognefjord, Norway, reaches as much as 1,300 m (4,265 ft) below sea level. Fjords generally have a sill or rise at their mouth caused by the previous glacier's terminal moraine, in many cases causing extreme currents and large saltwater rapids (seeskookumchuck). Saltstraumen in Norway is often described as the world's strongest tidal current. These characteristics distinguish fjords from rias (e.g. the Bay of Kotor), which are drowned valleys flooded by the rising sea.