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, Norway ]] , Norway ]] A fjord (or '''fiord''') is a long, narrow Estuary with steep sides, made when a glacial valley is flooded by the sea. The seeds of a fjord are laid when a Glacier cuts a U-shaped Valley through Abrasion of the surrounding Bedrock by the rocks and sediment it carries. Many such valleys were formed during recent Ice Age s when the sea was at a much lower level than it is today. At the end of such a period, the Climate warms up again and glaciers retreat. Sea Level rises due to an influx of water from melting Ice Sheet s and glaciers around the world (it rose over 100 m after the last ice age), inundating the vacated valleys with seawater to form fjords. Fjords are often very deep in their upper and middle reaches, in the case of Norway's Hardangerfjord dropping 800 m (2,624 ft) below sea level, although fjords generally have a sill or rise at their mouth associated with the previous glacier's Terminal Moraine . ETYMOLOGY
As a Loanword from Norwegian , it is the only word in the English language to start with the Digraph ''fj''. Scandinavian usage Use of the word fjord (including the eastern Scandinavian form ''fjärd'') is more general in the Scandinavian Languages than in English. In Scandinavia, ''fjord'' is used for a narrow inlet of the sea in Norway, Denmark and western Sweden, but this is not its only application. In Norway, the usage is closest to the Old Norse, with fjord used for both a firth and for a long, narrow inlet. In eastern Norway, the term is also applied to long narrow freshwater lakes (for instance Mjøsa (commonly referred to as ''fjorden''), Randsfjorden and Tyrifjorden ) and sometimes even to rivers (in local usage, for instance in Flå in Hallingdal , the Hallingdal River is referred to as ''fjorden''). In east Sweden, the name ''fjärd'' is used in a synonymous manner for bays, Bights and narrow inlets on the Swedish Baltic Sea coast, and in most Swedish lakes. This latter term is also used for bodies of water off the coast of Finland where Finland Swedish is spoken. In Danish, the word may even apply to shallow Lagoon s. In modern Icelandic, ''fjörður'' is still used with the broader meaning of firth or inlet. In Finnish Language , a word ''vuono'' is used although there is only one fjord in Finland. The German use of the word ''Förde'' on sea-stretches on their Baltic Sea coastline, seems to indicate a common Germanic origin of the word. The landscape consists mainly of moraine heaps, and "real" fjords in the geological sense are not possible. Kieler Förde still fits the same criteria as other fjordnames further north (in Denmark ), while others merely fits the description of ''bugt'' as used in Danish . One may therefore conclude that fjord was one of the names used by Germanic tribes to describe a sea-territory. The name of Wexford in Ireland is originally derived from ''Veisafjǫrðr'' ("inlet of the mud flats") in Old Norse , as used by the Viking settlers — though the place does not have a fjord in the more narrow modern meaning. LOCATIONS .]] The principal mountainous regions where fjords have formed are in the higher Middle Latitudes where, during the glacial period, many valley glaciers descended to the then-lower sea level. The fjords develop best in mountain ranges against which the prevailing Westerly marine winds are Orographically Lifted over the mountainous regions, resulting in abundant snowfall to feed the glaciers. Hence coasts having the most pronounced fjords include the west coast of Europe, the west coast of North America from Puget Sound to Alaska, the west coast of New Zealand, and the west coast of South America. Other areas which have lower altitudes and less pronounced glaciers also have fjords or fjord-like features. West coast of Europe
West coast of New Zealand
West coast of North America
West coast of South America Other glaciated regions ]] Other regions have fjords, but many of these are less pronounced due to more limited exposure to westerly winds and less pronounced relief. Areas include:
Extreme fjords , Norway]] The longest fjords in the world are: # Scoresby Sund in Greenland - 350 km (220 mi) # Sognefjord in Norway - 203 km (126 mi) # Hardangerfjord in Norway - 179 km (111 mi) Deep fjords include: # Skelton Inlet in Antarctica - 1,933 m (6,342 ft) # Sognefjord in Norway - ~1,308 m (4,291 ft) (the mountains then rise to up to 1,000 m) # Messier Channel in Chile, South America - 1,288 m (4,226 ft) Even deeper is the Vanderford Valley (2,287 m or 7,503 ft), carved by the Antarctica's Vanderford Glacier. This undersea valley lies offshore, however, and so is not a fjord. FJORD FEATURES AND VARIATIONS Coral reefs As late as 2000, some of the world's largest coral reefs were discovered along the bottoms of the Norwegian fjords. These reefs were found in fjords all the way from the north of Norway to the south. The marine life on the reefs is believed to be one of the most important reasons why the Norwegian coastline is such a generous fishing ground. Since this discovery is fairly new, little research has yet been done. So far, only the deep sea diver who discovered the first reef at 60 meters has visited it, and even he has only been down three times. The reefs are host to thousands of lifeforms such as plankton, coral, Anemones , fish, several species of sharks, and many more one would expect to find on a reef. However most are specially adapted to life under the greater pressure of the water column above it, and the total darkness of the deep sea. New Zealand's fiords are also host to deep sea corals, but a surface layer of dark fresh water allows these corals to grow in much shallower water than usual. An underwater observatory in Milford Sound allows tourists to view them without diving. Skerries In some places near the seaward margins of areas with fjords, the ice-scoured channels are so numerous and varied in direction that the rocky coast is divided into thousands of island blocks, some large & mountainous while others a merely rocky points or rock Reef s, menacing navigation. These are called Skerries . The term skerry is derived from the Old Norse ''sker'', which means a rock in the sea. Skerries are most commonly formed at the outlet of fjords where submerged glacially formed valleys at right angles with the coast join with other cross valleys in a complex array. The island fringe of Norway is such a group of skerries (called a ''skjærgård''); many of the cross fjords are so arranged that they parallel the coast and provide a protected channel behind an almost unbroken succession of mountainous islands and skerries. By this channel one can travel through a protected passage almost the entire 1,600 km route from Stavanger to North Cape , Norway. The Blindleia is a skerry-protected waterway that starts near Kristiansand in southern Norway , and continues past Lillesand . The Swedish coast along Bohuslän is likewise skerry guarded. The “inside passage” provides a similar route from Seattle , Washington to Skagway , Alaska. Yet another such skerry protected passage extends from the Straits Of Magellan north for 800 km. FALSE FJORDS The differences in usage between the English and the Scandinavian languages have contributed to confusion in the use of the term fjord. Bodies of water which are clearly fjords in Scandinavian languages are not considered fjords in English; similarly bodies of water which would clearly not be fjords in the Scandinavian sense have been named or suggested to be fjords. Examples of this confused usage follow. The Gulf Of Kotor in Montenegro has been suggested by some to be a fjord, but is in fact a drowned river canyon or Ria . Similarly the Lim bay in Istria , Croatia , is sometimes called "Lim fjord" although it is not actually a fjord carved by glacial erosion but instead a ria dug by the river Pazinčica. The Croat s call it ''Limski kanal'' which does not transliterate precisely to the English equivalent either. Limfjord in the north of Denmark is a fjord in the Scandinavian sense, but is not a fjord in the English sense. In English it would be called a Channel , since it separates the island of Vendsyssel-Thy from the rest of Jutland . While the long fjord-like bays of the New England coast are sometimes referred to as "fiards", the only glacially-formed fjord-like feature in New England is Somes Sound in Maine. The fjords in Finnmark (Norway), which are fjords in the Scandinavian sense of the term, are considered by some to be false fjords. Although glacially formed, most Finnmark fjords lack the classic hallmark steep-sided valleys of the more southerly Norwegian fjords since the glacial pack was deep enough to cover even the high grounds when they were formed. Some Norwegian freshwater lakes which have formed in long glacially carved valleys with terminal Moraines blocking the outlet follow the Norwegian naming convention; they are named fjords. Outside of Norway, the three western arms of New Zealand's Lake Te Anau are named North Fiord, Middle Fiord and South Fiord. Another freshwater "fjord" in a larger lake is Baie Fine, located on the northeastern coast of Georgian Bay of Lake Huron in Ontario . Western Brook Pond, in Newfoundland's Gros Morne National Park , is also often described as a fjord, but is actually a freshwater lake cut off from the sea, so is not a fjord in the English sense of the term. Such lakes are sometimes called "fjord lakes". Okanagan Lake was the first North American lake to be so described, in 1962 . The bedrock there has been eroded up to 650 m ''below'' sea level, which is 2000 m below the surrounding regional topography - deeper than the Grand Canyon . FJORDS IN CULTURE AND HISTORY Fjord horse There is an ancient breed of horse from the western Norway fjord regions called the Fjord Horse . Fjords in literature and popular culture
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