|Møre og Romsdal|
|o Total||58,582 km2 (22,619 sq mi)|
|o Land||55,411 km2 (21,394 sq mi)|
|o Density||25/km2 (64/sq mi)|
|Nominal GDP (2013)||$57 billion|
|Nominal GDP per capita (2013)||$41,000|
Western Norway (Bokmål: Vestlandet, Vest-Norge; Nynorsk: Vest-Noreg) is the region along the Atlantic coast of southern Norway. It consists of the counties Rogaland, Vestland, and Møre og Romsdal. The region has no official or political-administrative function. The region has a population of approximately 1.4 million people. The largest city is Bergen and the second-largest is Stavanger. Historically the regions of Agder, Vest-Telemark, Hallingdal, Valdres, and northern parts of Gudbrandsdal have been included in Western Norway.
Western Norway, as well as other parts of historical regions of Norway, shares a common history with Denmark, the Faroe Islands and Iceland and to a lesser extent the Netherlands and Britain. For example, the Icelandic horse is a close relative of the Fjord horse and both the Faroese and Icelandic languages are based on the Old West Norse.
In early Norse times, people from Western Norway became settlers at the Western Isles in the Northern Atlantic, so that Orkney, Shetland, the Faroe Islands and Iceland. During the Viking Age settlements were made at the Hebrides, Man and Ireland proper.
In early modern time, Western Norway has had much emigration to the United States, Canada, and to a lesser extent to the United Kingdom. This applies particularly to the US states of Minnesota, North and South Dakota, Wisconsin, Montana, and the Canadian province of Manitoba. The Icelandic and Faroese people, and many people in the British Isles, are descendants of Norsemen and Vikings who emigrated from Western Norway during the Viking Age. On the other hand, thousands of Western Norwegians are descendants of Dutch and German traders who arrived in the 16th and the 17th centuries, especially in Bergen.
Western Norway has the lowest unemployment rates, lowest crime rates, smallest public sector, fewest people on welfare and the most innovative economy in the country. It is generally regarded as Norway's most functional region.
Vestland is also the name of a county consisting of two former counties, viz. Hordaland and Sogn og Fjordane. The two counties were re-merged after having been split in 1763 (then called Søndre Bergenhus and Nordre Bergenhus, respectively).
Norway's history begins on the west coast, particularly in Rogaland. Excavations and rock art tells us that it was in Rogaland that the first humans settled in Norway, when the ice retreated after the last ice age ca. 10,000 years ago. There are many artifacts from the Stone Age in Rogaland. The preliminary oldest traces of humans are found in a settlement on Galta, Rennesøy, near the ferry terminal Mortavika and Vista on Randaberg. In the beginning there has been sure short visits by people from the south who hunted along the coast. It is thought that people came from Doggerland, the North Sea land area between Denmark and England, which disappeared when the ice retreated and sea levels rose. The people who lived there must now find a new land. Some retreated south again, while a few passed the Norwegian Trench (which was considerably smaller than now) in its hunt for deer and the new country.
The region includes most of the scope of the old Gulating, which was founded around the year 900. The Gulating Act divided the country into the Western counties, which consisted of the former småkongedømmene that existed in the area before the unification of the 800's and then was converted to jarle judge. These were Sunnmørafylke (Sunnmøre), Firda County (Fjordane), Sygna County (Sogn), Hordafylke (Hordaland), Rygjafylke (Rogaland) and Egdafylke (Agder).
Harald Hairfair united Norway and parts of Sweden west of Lake Vänern and Götaälv in the 9th century from his Castle Avaldsnes on Karmöy at Haugesund. Norway was named from the Way North by seafaring.
Before the millennium, iron was introduced and used in agriculture, and there was a shortage of land to cultivate. In the same period, the kings' power increased, and large tax claims caused many to seek freedom and fortune abroad. Many emigrated, and looting became an alternative source of income. Effective boats and weapons made the Vikings feared among contemporary Christian Europeans. But the images of Vikings as bloodthirsty plunderers are not always representative. The Vikings were involved in a wealthy merchant trade, not only in Europe but also including the Byzantine Empire and the Baghdad Caliphate.
Historically Vikings are often introduced with the Viking attack on Lindisfarne in 793, when they really made their mark in European history. The era ends with the Battle of Stamford Bridge in 1066. Vikings' seaworthiness and wanderlust resulted in new areas being developed. Norwegian settlers moved into the North Sea westward to Iceland, the Faroe Islands, Greenland, Shetland, Orkney, Isle of Man and the Hebrides. Settlements were established in the southeast corner of Ireland including in Dublin, Waterford and Wexford. Norwegians settled along the northwest area of England, principally in the area of modern-day Cumbria. The Norwegian Vikings also discovered Vinland, present-day America, long before Christopher Columbus.
Christianity (Catholicism) became the dominant religion in Norway in the 11th century, but the religion was probably known among Norwegians already in the 7th century.
While Eastern Norway was introduced to Christianity by missionaries and monks from Germany and Friesland, Western Norway was mainly introduced to the religion by English, Scottish, Irish people and Vikings who had converted to Christianity. Norse paganism existed in some areas in Western Norway until they were totally replaced by Christianity in the 13th century. The coastal areas were the first to introduce the new faith, and then the inland areas. Churches were planted everywhere.
The main source of information about the settlement period in Iceland is the Book of Settlements (Landnámabók), written in the 12th century, which gives a detailed account of the first settlers. According to this book, Western Norwegian sailors accidentally discovered the country. A few voyages of exploration were made soon after that and then the settlement started. Ingólfur Arnarson was said to be the first settler. He was a chieftain from Norway, arriving in Iceland with his family and dependents in 874. He built his farm in Reykjavík, the site of the present capital. During the next 60 years or so, Viking settlers from Scandinavia and also from Norse colonies in the British Isles--Ireland, Scotland and the Scottish Isles--settled in the country. There was therefore a Celtic element among the first inhabitants. The settlement of Iceland may also be viewed in the context of the general Viking expansion of the period, plausibly linked to population pressure in Western Norway and increasing scarcity of farming land.
It has thus left few traces in the archaeological record, nor has it contributed more than a handful of words to the Icelandic language, which was a Scandinavian dialect, more or less identical with the Viking Age Norse spoken in Western Norway, the Faroes, Shetland, Orkney, etc. Today it is estimated that 60% of the Icelandic population are descendants of people from Western Norway.
For a century emigration was a central aspect of Norwegian history and more than 800,000 Norwegians emigrated to the United States. The first organized group of emigrants left Stavanger on the sloop Restoration on 4 July 1825. In 1837, Ægir left Bergen as the first ship with emigrants from Hordaland.
The Emigration Center of Western Norway is a memorial to those who left and to their descendants. The emigrant archives now include 96,000 names of emigrants from the two counties of Hordaland and Sogn og Fjordane up to 1924. This has been possible thanks to the work of many years by Jahn Sjursen, who has also collected books and other publications, pictures and objects related to Norwegian emigrants in the United States. He officially donated his collections to the Emigration Center at the opening in 1997. The Center continues to receive publications and objects for its collection. Via the internet we are linked to the national digital records of emigrants from Norway to the United States that have been developed by the University of Bergen and the Bergen Public Archives. The Center's Emigrant Church was originally the Brampton Lutheran Church in Sargent County, North Dakota, built by Norwegian emigrants at the turn of the 19th century. The Brampton congregation was formed 1 July 1908. and 22 June 1996, the congregation donated their fully furnished church to the Emigration Center. It was taken down, transported to Sletta and reconstructed there by volunteers from Radøy. The church was reconsecrated by the Bishop of Bjørgvin, Ole Danholt Hagesæther, 6 July 1997.
|o Total||58,582 km2 (22,619 sq mi)|
|Coastline||26,592 km (16,524 mi)|
|Highest point||Store Skagastølstind|
|Lowest point||North Sea|
Western Norway is the third largest region in Norway by area. It covers an area of 58,582 km2 (22,619 sq mi).
The United Kingdom and the Faroe Islands lie to the west across the North Sea, while Denmark lies south of its southern tip across the North Sea. It is 675 km (419 mi) from the Faroe Islands to Western Norway while Unst in the Shetland Islands is about 300 km (190 mi) away. Western Norway has a 26,592 km (16,524 mi) long coastline.
The southern part of the region is called Jæren. This is one of the major agricultural areas in Norway. Farms in other areas of Western Norway are often small. The total area of agricultural in Western Norway is 2 650 square kilometers, which is 5.3% of the total area in the region.
Western Norway is highly mountainous; in less than 10 kilometers from the Sognefjord, there are peaks that are over 2000 meters in height. The highest point is Store Skagastølstind (also known as Storen), which is 2,405 meters high. It is situated on the border between the municipality of Luster and Årdal and is part of the Hurrungane range. The summit is a destination for mountaineers but is fairly difficult. First ascent by William Cecil Slingsby on 21 July 1876. There are a number of different routes, the most common being Heftye's renne (Heftye's couloir). Another route of ascent is via Andrew's renne (Andrew's couloir), first ascent A. W. Andrews and party in 1899. Store Skagastølstind and the mountaineering of the late 19th century in Norway is traditionally linked to the historical hotel Turtagrø.
There are many fjords in Western Norway, Hardangerfjorden, Boknafjorden and Sognefjorden is the longest. The Sognefjord (Sognefjorden) is the largest fjord in Norway, and the second longest in the world, after Scoresby Sund on Greenland. Located in Sogn og Fjordane it stretches 205 km (127 mi) inland to the small village of Skjolden.
Providing the most spectacular fjord and mountain scenery in Norway, the region has been a tourist mecca for centuries. Except for the Jæren plain located at the extreme southern end of the region, Vestlandet is mountainous, with the Jotunheim Mountains and the Hardanger Plateau being the highest areas. The Jostedals Glacier, the largest glacier in Europe, is located in the north-central part of the region, while Hardanger Icecap (Hardangerjøkulen) and the Folgefonna Glacier are smaller ice fields in the south. Norway's longest fjord, Sogn Fjord (205 km [127 mi]), located in the central part of the region, nearly divides Vestlandet in two; farther south Hardanger Fjord stretches inland for 179 km (111 mi). Many waterfalls flow into the fjords, with the Syv Systre, Toka Gorge, and Vørings Falls (Vøringsfossen) among the best known. The rugged coastline is protected by thousands of offshore islands in a nearly continuous line. Occasionally, the northern parts of Møre og Romsdal are considered to be part of Trøndelag.
Map references: Europe
total: 58,582 km2
Coastline: 26,592 km
contiguous zone: 10 nmi (18.5 km; 11.5 mi)
continental shelf: 200 nmi (370.4 km; 230.2 mi)
exclusive economic zone: 200 nmi (370.4 km; 230.2 mi)
territorial sea: 12 nmi (22.2 km; 13.8 mi)
Rivers running westward acquired tremendous erosive power. Following fracture lines marking weaknesses in the Earth's crust, they dug out gorges and canyons that knifed deep into the jagged coast. To the east the land sloped more gently, and broader valleys were formed. During repeated periods of glaciation in the Great Ice Age of the Quaternary Period (i.e., about the last 2.6 million years), the scouring action of glaciers tonguing down the V-shaped valleys that were then part of the landscape created the magnificent U-shaped drowned fjords that now grace the western coast of Norway. Enormous masses of soil, gravel, and stone were also carried by glacial action as far south as present-day Denmark and northern Germany. The bedrock, exposed in about 40 percent of the area, was scoured and polished by the movements of these materials.
From the southernmost point a swelling complex of ranges, collectively called Langfjellene, runs northward to divide eastern Norway, or Østlandet, from western Norway. The narrow coastal zone of Vestlandet has many islands, and steep-walled, narrow fjords cut deep into the interior mountain region. The major exception is the wide Jæren Plain, south of Stavanger.
Glaciation and other forces wore down the surface and created thick sandstone, conglomerate, and limestone deposits known as sparagmite. Numerous extensive areas called peneplains, whose relief has been largely eroded away, also were formed. Remains of these include the Hardanger Plateau--1,100 m (3,600 ft) above sea level--Europe's largest mountain plateau, covering about 6,500 km2 (2,500 sq mi).
Glaciated; mostly high plateaus and rugged mountains broken by fertile valleys; small, scattered plains; coastline deeply indented by fjords. Frozen ground all-year can also be found in the higher mountain areas. Numerous glaciers are still found in Western Norway.
The fjords of western Norway formed in connection to the east-ward tilting of much of Norway during the Cenozoic uplift of the Scandinavian Mountains. This uplift, that occurred long before the Quaternary glaciations, enabled rivers to incise deeply the Paleic relief. A study of Sognefjord suggest that the fluvial and glacial erosion that made the fjords has followed structural weaknesses in the crust. The headvalleys in particular seem to located at structural weakness zones. Western Norway bears some resemblance to other passive margins at lower latitudes like eastern Australia. In both cases a table land is dissected by valleys forming a great escarpment. The main differences is that in Norway valley and fjord bottoms have been widened by glacier erosion, valley sides steepened, and the outer regions of valleys straightened, also by glacier erosion.
The deglaciation patterns of the Bergen and Nordfjord-Sunnmøre areas in western Norway are described and correlated. In the Bergen area the coast was first deglaciated at 12,600 B.P., with a succeeding re-advance into the North Sea around 12,200 B.P. Later, during the Allerød, the inland ice retreated at least 50 km, but nearly reached the sea again during the Younger Dryas re-advance, ending at 10,000 B.P. Sunnmøre was ice-free during an interstadial 28,000-38,000 B.P. Later the inland ice reached the sea. The final deglaciation is poorly dated in Sunnmøre, while further south in Nordfjord, it started slightly before 12,300 B.P., followed by a major retreat. No large re-advance of the inland ice occurred during the Younger Dryas. However, in the Sunnmøre-Nordfjord area many local glaciers formed outside the inland ice during the Younger Dryas. Limnic sediments outside one such cirque glacier have been cored and dated, proving that the glacier did not exist at 12,300-11,000 B.P., and that it was formed and disappeared in the time interval 11,000-10,000 B.P. (Younger Dryas). The erosion rate of the cirque glacier was 0.9 mm/year.
Western Norway has similar flora and fauna as the rest of Norway, but there are some major differences. While almost all red deer in Norway are found here, there are few moose. Reindeer are a common sight on the Hardangervidda and in other large mountain areas. The whole of the Hardangervidda is above the tree line. Its alpine climate means that many species of Arctic animals and plants are found here, further south than anywhere else in Europe. Its wild reindeer herds are among the largest in the world, with some 15,000 animals recorded in 1996 and about 8,000 in 2008. They migrate across the plateau during the year, moving from their winter grazing lands on the east side of the Hardangervidda, where they graze on lichen, to their breeding grounds in the more fertile west of the plateau.
30,000 years ago glaciers covered vast areas of the Northern Hemisphere. As so much water was trapped on land, in the form of glacial ice, the sea lay 120 metres below its present level. This meant that the North Sea was dry land, a treeless tundra, with long, winding rivers, endless stretches of boggy land and wide, sandy heaths. Only as far south as the Mediterranean and the Black Sea were there any forests.
As the climate slowly improved and the Scandinavian peninsula rose from the grip of the ice, plants and animals started to invade the new territory. As soon as there was dry land the first plants took root and with them came animals, birds and insects. The first of these were the Arctic animals such as wild reindeer, Arctic fox and wolverine (glutton), who followed the edge of the glacier up to the mountains. The trees came later, accompanied by a rich flora and fauna including bears, elk, marten, fox, hare, European beaver and otter.
This influx reached its climax around 3000 BC when the climate improved considerably, giving rise to the postglacial period of warmth. The average temperature rose 3 degrees. This may not sound very much, but in the mountains the tree line rises about 100 metres up the mountainside for each degree M so the consequences were dramatic. Most of the mountains of Western Norway which today occupy about three quarters of the land mass M became covered with dense forests of pine and birch. The glaciers had thawed and vanished, and extensive oak forests, not unlike those we see today in Central Europe, spread over the low-lying land. Life was hard for the animals and plants in the high mountains, as they were pressed up towards the highest peaks, which rose like islands from a sea of forest.
Along the west coast the winter is mild and snowfalls rare. Here are a number of the plants which cannot tolerate frost, for example the star hyacinth (scilla verna) and the purple heather (erica purpurea), which are otherwise only found in England, Ireland and further south. A little further inland we come upon the species which can withstand short periods of frost and snow in winter. These are found both a little further north, and in the fjords. Typical examples are the foxglove (digitalis purpurea) and the holly (ilex aquifolium), which in Norway grow only in the southwest.
Animals found in Western Norway
Western Norway is one of the wettest regions in Europe, with precipitation in the mountains near the coast of about 3,500 mm per year on average, and exceeding 5,000 mm in peak years. In Bergen city the average precipitation is 2,250 mm per year . The wet climate is partly due to the Gulf Stream, which also gives this region a milder winter than other parts of Norway, with rain being more common than snow in the winter.
Late June to early August is when summer is at its peak. This is when the weather is at its most stable and warmest with sunny, long and bright days. It is not unusual with temperatures reaching 25 °C (77 °F) and above.
During the course of September the landscape is painted in golden colours. Red clusters of rowan berries hang on naked branches. Autumn also means harvest time along the fjords.
Gales, rain and cloud are likely along the west coast and the rainfall is frequent and heavy. Thanks to the warming Gulf Stream, the Norwegian fjords enjoy a relatively mild climate and remain virtually ice-free even during the winter. Wintertime, usually from November, turns the mountain areas of Western Norway into highly favourable skiing conditions.
During springtime the most amazing colours burst forth to honour the warmth of the rising sun. Orchards of flowering fruit trees can be seen along the Hardangerfjord in May.
Western Norway is a very rich region. The region generates around 70% of the total Gross National Product of Norway--Europe's richest country. Today is Stavanger the capital of oil in Norway. Before petroleum, fishing and agriculture were the most important economic activities in Western Norway. The region was responsible for 51% of aquaculture and fishing domestic product in Norway. Western Norway, Jæren, Karmøy, Vindafjord, Voss, Sunnfjord and Fræna comprises a rich agricultural area. The inland fjord areas of Hardanger are more sheltered, with rich fruit districts specializing in apples and cherries.
Along the coast fishing plays the same role that forestry does elsewhere. At the same time, it forms the basis of a large fish-processing industry and offers seasonal employment for many farmers. Of all fishermen only half fish as their sole occupation. Most vessels are owned by the fishermen themselves, the necessary crew members being paid by shares of gross income in a continuation of a centuries-old tradition of the sea. A critical problem is how to avoid depleting the fish resources while maintaining the volume. About half the catch goes into fish meal and oil, but some is processed for human consumption in freezing plants. Fish offal is used as feed at mink farms. In the northwest the city of Ålesund thrives on fishing. Ålesund is one of the world's largest and most important ports for cod.
By the mid-1990s Norway had become the world's second largest oil exporter (behind Saudi Arabia). The first commercially important discovery of petroleum on Norway's continental shelf was made at the Ekofisk field in the North Sea late in 1969, just as foreign oil companies were about to give up after four years of exploratory drilling. Intensified exploration increased reserves faster than production. Nevertheless, by the mid-1990s about half of export earnings and nearly one-tenth of government revenues came from offshore oil and gas, and these revenues continued to increase as the end of the century approached. It was estimated that the high rate of oil production could be sustained at least into the second decade of the 21st century, while that of natural gas was projected to increase dramatically and be sustained much longer.
More than one-fourth of the huge investment made in Norwegian offshore operations by the mid-1990s went toward the development of the Troll gas field just west of Bergen, one of the largest offshore gas fields ever found. Its development ranked as one of the world's largest energy projects. With a water displacement of one million tons and a height of nearly 1,550 feet (475 m), the Troll A platform was the tallest concrete structure ever moved when it was towed into place in 1995. Gas deliveries from the Troll field made Norway a leading supplier of natural gas to continental Europe.
Western Norway has one of the highest population growth rate in Norway for 2009, 1.44%, while the country as a whole is 1.20%. The population 1. January 2010 is 1,263,464. 37.7% of the population lived in Hordaland, 33.8% in Rogaland, 19.8% in Møre og Romsdal, and 8.4% in Sogn og Fjordane. 60% of the population are under 40 years old, and 30% are under 20 years old. Many of the historical immigrants in Western Norway came from countries like Scotland, England, Netherlands, Germany, Denmark and Sweden, and Western Norway is still the part of Norway who has the largest immigration from the western world.
|Country of origin||Norway||Immigrants||Eastern Europe||Asia||Western Europe||Africa||Nordic countries||Latin America||North America||Oceania||Total|
Western Norway is also notable for the extensive use of the Nynorsk variant of the Norwegian language: Most of the Nynorsk users in Norway (87%) live in Western Norway. But in spite of this the majority of the inhabitants here (56%) use Bokmål (because Bokmål is predominant in the cities). In Sogn og Fjordane (without larger cities) the use of Nynorsk is predominant (97%), and the users of Nynorsk is also a majority in Møre og Romsdal (54%). But in Hordaland and Rogaland the users of Nynorsk are a minority (42% and 26%, respectively). The percentage would be higher if the numbers excluded the northern areas of Møre og Romsdal and the southern areas of Rogaland. Every single municipality in Sogn og Fjordane, Sunnmøre (except Ålesund), Hordaland (except Bergen, Askøy and Odda) and Ryfylke (except Strand and Kvitsøy) have selected Nynorsk as the official written language form.
In many cases Nynorsk is more similar to Icelandic than Bokmål:
Christianity is the largest religion. 1,050,559 people are members of the Church of Norway. There are also 55,621 members in other Christian churches. Islam has 11,655 adherents in Western Norway. Buddhism has 2,452 members. 1,557 are from Bahá'í Faith, Judaism, Sikhism and other related religions. Religion is often more important for the inhabitants than the rest of Norway.
The name "Bible Belt" has been applied historically to the Southern and Western parts of Norway. The region thus defined included most of Western Norway, especially Rogaland, Møre og Romsdal and some parts of Hordaland. Notably absent from this belt are bigger cities like Bergen and Stavanger where many people identify themselves as non-religious or with other religions. In these areas the conservative branch of the Church of Norway has a stronghold and the members usually associate themselves to Indremisjonen (Inner Mission). There are also numerous Pentecostals and members of the Free Churches, but these movements are also strongly represented in the rest of the country. The Bible Belt in Norway traditionally reflects the support for the Christian Democratic Party. However, especially since the first decade of the 21st century, conservative bible belt Christians unhappy with the more liberal development of the party have increasingly turned to the Progress Party.
Several locations are occasionally referred to as the "Buckle of the Bible Belt":
Bergen has one university, the University of Bergen, and one university college, Bergen University College, with a total of 22,000 students and 3,600 staff. With approximately 16,000 students and 3,000 staff, the University of Bergen (Norwegian: Universitetet i Bergen) is the third largest university in Norway, after the University of Oslo and the Norwegian University of Science and Technology. Although it was founded as late as 1946, academic activity had been taking place at Bergen Museum since 1825. The university's academic profile focuses on marine research and co-operation with developing countries. In 2002, the university was awarded three national centres of excellence in climate research, petroleum research and medieval studies. In December 2004, billionaire Trond Mohn donated 250 million NOK to the University as research funding. In addition, he has given the university several individual gifts of 50 million NOK. Bergen University College (Norwegian: Høgskolen i Bergen) is one of 24 state-owned university colleges in Norway. As of 2007, it has approximately 6,000 students and 600 staff. The university college offers studies directed towards specific professions. The college is organised in 3 faculties: the Faculty of Education, the Faculty of Engineering, and the Faculty of Health and Social Sciences.
The Norwegian School of Economics and Business Administration (Norwegian: Norges Handelshøyskole) is a leading school of business and economics in Norway. Finn E. Kydland, the most recent (2004) of three Norwegian laureates of the Economy Nobel Prize, has studied and lectured at the school. The school has approximately 2,700 students and 350 staff. As the result of a resolution passed by the Norwegian storting in 1917, the school was founded in 1936 as the first business school in Norway. As of 2007, the school's MSc programme is ranked by the Financial Times as the 36th best in Europe. The Bergen School of Architecture (Bergen Arkitekt Skole), founded in 1986 by architect Svein Hatløy, has alternative programs, with graduates like 3RW arkitekter and Tommie Wilhemsen. The Bergen National Academy of the Arts (Kunsthøgskolen i Bergen, approximately 300 students and 100 staff) is one of the two independent institutions of higher learning in the visual arts and design in Norway. Students can take a three-year bachelor's degree and a two-year master's degree in the following areas: Visual Art, Interior Architecture, Furniture Design, Room Design, Visual Communications, Photography, Printmaking, Ceramics and Textiles. The Naval Academy (Sjøkrigsskolen) of the Royal Norwegian Navy is located at Laksevåg in Bergen.
Stavanger has several schools for the expatriate community including the British International School of Stavanger and the International School of Stavanger. Stavanger has one university, the University of Stavanger with about 8,000 students. The university was formerly a university college. It was granted status as University on 1 January 2005. The population of Stavanger has a high percentage of university educated persons, with 31.3% of those above the age of 16 having higher education, compared to the national average of 24.2% (2006 figures).
Traditionally there was only one university in Western Norway, located in Bergen (1948). Since 2005 any college offering five master programs and four doctoral programs can title itself a university, leading to the Stavanger University College converting to a university.
The public universities of Western Norway are:
Currently there are no private universities in Western Norway, although BI Norwegian Business School in Bergen and Stavanger have tried to advance to a full university.
There are one public and three private specialised universities in Western Norway, each functioning as a national competence centre for the field they represent.
The public specialised universities in Western Norway are:
The private specialised universities are:
The 7 university colleges in Western Norway are responsible for regional education of primarily bachelor level education within the fields of nursing, teaching, business management, engineering and information technology, though most colleges also offer a number of other educations as well.
The public university colleges in Western Norway consist of:
Western Norway is famous for much of the cuisine in Norway. In its traditional form is based largely on the raw materials readily available in Norway and its mountains, wilderness and coast. It differs in many respects from its continental counterparts with a stronger focus on game and fish.
Modern Norwegian cuisine, although still strongly influenced by its traditional background, now bears the marks of globalization: Pastas, pizzas and the like are as common as meatballs and cod as staple foods, and urban restaurants sport the same selection one would expect to find in any western European city.
Lamb's meat and mutton is popular in autumn, mainly used in fårikål (mutton stew with cabbage). Pinnekjøtt, cured and sometimes smoked mutton ribs that is steamed for several hours, is traditionally served as Christmas dinner in the western parts of Norway. Another Western specialty is smalahove, a smoked lamb's head.
Music based on traditional Norwegian form usually includes minor or modal scales (sometimes mixed with major scales), making a sober and haunting sound. Pure major key dance music forms also exist. Prior to the 18th century, there is scant written record of what kind of music was played in Norway, but there is a large aural tradition. In 1380, Norway had come under Danish rule, and thus had no royal house or nobility of its own; as a result, for 450 years, Norway did not participate as much in the musical development which occurred in royal (or "cultured") circles throughout the rest of Europe. Religious and traditional (folk) music were dominant throughout this era in rural areas, though again scant records exist to document their nature. In the last half of the 20th century, Norway, like many other countries in the world, underwent a roots revival that saw indigenous music being revived.
From about 1831, traditional Norwegian music began to influence the classical scene, especially through Ole Bull, who befriended the traditional Hardanger fiddle player Myllarguten and through the friendship gained better understanding of traditional music. Bull himself started playing the Hardanger fiddle, and was the first to present folk tunes to the public in urban areas. He also saw to that Myllarguten played with him in concert, presenting a rural traditional musician to an urban audience for the very first time, in February 1849, at the very height of Norwegian romantic nationalism. This later inspired Edvard Grieg to look for folk musical sources. But urban audiences were slow to gain an appreciation and understanding of traditional (rural) music.
Western Norway is famous for many writers. Ludvig Holberg was one of them. He was born in Bergen, but he moved to Copenhagen when he was young. He was influenced by Humanism, the Enlightenment and the Baroque. Other notable writers from Western Norway include Alexander Kielland, Arne Garborg, Bjørnstjerne Bjørnson, Arnulf Øverland and Inger Hagerup.
In the early Middle Ages, stave churches were constructed throughout Norway. Many of them remain to this day and represent Norway's most important contribution to architectural history. A fine example is The Stave Church at Urnes which is now on UNESCO's World Heritage List. Another notable example of wooden architecture is the Bryggen Wharf in Bergen, consisting of a row of narrow wooden structures along the quayside. At the beginning of the 20th century, the city of Ålesund was rebuilt in the Art Nouveau style. The 1930s, when functionalism dominated, became a strong period for Norwegian architecture, but it is only in recent decades that Norwegian architects have truly achieved international renown.
Kitty Kielland, the sister to A. Kielland and Nikolai Astrup are famous painters from Western Norway. Brudeferden i Hardanger is the best known art from Western Norway. This is painted by the Norwegian painters Adolph Tidemand and Hans Gude.
Of the 26 airports in Western Norway, 15 are public, and 11 are operated by the state-owned Avinor. Two airports have more than one million passengers annually. 41,089,675 passengers passed through Norwegian airports in 2007, of which 13,397,458 were international.
The regional airport service was introduced in the 1960s, with 30 airports being served by short take-off and landing aircraft. These are located mainly in Sogn og Fjordane, in areas with long distances to large cities and with too little traffic to support commercial flights. The airports, which typically have an 800 metres (2,600 ft) runway, are run by Avinor, while the airplanes are operated based on subsidized public service obligation contracts with the Norwegian Ministry of Transport and Communications. By far the largest contractor is Widerøe with their fleet of de Havilland Canada Dash 8 aircraft, but also Danish Air Transport, Lufttransport and Kato Air have won bids.
The main long-haul network consists of lines from Bergen eastwards to Voss and over the mountains to Oslo and a line connecting Stavanger to Oslo via Kristiansand. There is also a line from Åndalsnes in Romsdal to Oslo. In Bergen there is a funicular and a light rail line. There are also plans for a light rail system further south in the region of Nord-Jæren.
The most important national routes are part of the European route scheme, and the most prominent are the E39 going north-south through the entire region. National and county roads are managed by the Norwegian Public Roads Administration.
Fast ferries operate many places where fjords and islands make it quicker to follow the waterways than the roads; some small islands are served by water buses. Public transport by ship transported eight million passengers 273 million passenger kilometers in 2007 in whole the country. The Coastal Express (known as Hurtigruten) operates daily cruiseferries from Bergen to Kirkenes, calling at 35 ports. International cruiseferries operate from Bergen and Stavanger to the United Kingdom and Denmark.
The petroleum and natural gas production on the Norwegian continental shelf uses pipelines to transport produce to processing plants on mainland Norway and other European countries; total length is 9,481 kilometres (5,891 mi). The government-owned Gassco operates all natural gas pipelines; in 2006, 88 billion cubic meters were transported, or 15% of European consumption
Vestlandet and Sørlandet have always been the two regions of Norway with the greatest preponderance of secular voters. The election in 2007 gave the non-socialist parliamentary parties 65.4% of the vote against the socialist parties' 29.7%. The government party had collected 39.5% against 55.6% parliamentary opposition.
The election in 2007 had the following vote distribution:
The elections from 2001 to 2009 had the following vote distribution:
|Norwegian Labour Party||13||11||8|
|Conservative Party of Norway||8||6||10|
|Christian Democratic Party||3||5||8|
|Socialist Left Party||2||3||5|
|Liberal Party of Norway||0||4||1|
Western Norway has 22 cities/towns. Three of the cities in Western Norway, Bergen and Stavanger, Sandnes, are among the ten most populous cities in the country. Cities and towns in the region in descending order by population:
These are traditional districts that only partially coincide with present-day administrative divisions. Arranged from North to South.
|Coat of arms||County||Adm. center||Largest city||Population (2021)||Area (km2)||Density||Mayor||Party||Governor||Language form|
|Vestland||Bergen||Bergen||638,821||34,062||18,76||Anne Gine Hestetun||Labour Party||Lars Sponheim||Nynorsk|
|Rogaland||Stavanger||Stavanger||482,645||9,377||51,47||Solveig Ege Tengesdal||Christian Democratic Party||Magnhild Meltveit Kleppa||Bokmål|
|Møre og Romsdal||Molde||Ålesund||265,544||15,121||17,56||Jon Aasen||Labour Party||Lodve Solholm||Nynorsk|