Americola

Search:

 

Biographies

Photos

Videos

Auctions

Shopping

 

Incredible offer on domain names with .coms starting at $6.95
www.T-Rex.net    Why Pay More?    Compare Us.    Free Hosting w/Site Builder & more!

Looking for photos of Iceland?
Look no further, you will find them right here!    Click Here!

Iceland biography, high resolution photos and videos by Americola

Iceland

[edit] Americola's celebrity biographies are provided by AmericolaWiki, a celebrity wiki. You can help contribute to Americola and edit this article.

This article is about the country in Europe. For other uses, see Iceland (disambiguation).
Lýðveldið Ísland
Republic of Iceland
Image:Flag of Iceland.svg Image:Skjaldarmerki.png
Flag Coat of arms
Motto
none
Anthem
Lofsöngur
Image:Europe location ISL.png
Location of  Iceland  (orange)

on the European continent  (white)

Capital
(and largest city)
Reykjavík
64°08′N, 21°56′W
Official languages Icelandic (de facto)
Government Constitutional republic
 -  President Ólafur Ragnar Grímsson
 -  Prime Minister Geir H. Haarde
Independence from Denmark 
 -  Home rule 1 February 1904 
 -  Sovereignty 1 December 1918 
 -  Republic 17 June 1944 
Area
 -  Total 103,000 km² (107th)
39,770 sq mi 
 -  Water (%) 2.7
Population
 -  April 2007 estimate 309,6991 (181st)
 -  December 1980 census 229,187 
 -  Density 2.9 /km² (222nd)
7.5 /sq mi
GDP (PPP) 2005 estimate
 -  Total $10.531 billion (135th)
 -  Per capita $35,586 (2005) (5th)
GDP (nominal) 2005 estimate
 -  Total $15.823 billion (90th)
 -  Per capita $52,764 (3rd)
HDI (2004) 0.960 (high) (2nd)
Currency Icelandic króna (ISK)
Time zone GMT (UTC+0)
Internet TLD .is
Calling code +354
1 Statistics Iceland. www.statice.is (1 December 2006). Retrieved on 20 September 2006.

Iceland, officially the Republic of Iceland (Icelandic: Ísland or Lýðveldið Ísland; IPA: [ˈliðvɛltɪð ˈislant]) is a country of northwestern Europe, comprising the island of Iceland and its outlying islets in the North Atlantic Ocean between Greenland, Norway, Ireland,UK and the Faroe Islands.[1] As of April 2007, it had a population of 309,699. Its capital and largest city is Reykjavík.

Iceland has a history of habitation since about the year 874 when, according to Landnámabók, the Norwegian chieftain Ingólfur Arnarson became the first permanent Norwegian settler on the island. Others had visited the island earlier and stayed over winter. Over the next centuries, people of Nordic and Gaelic origin settled in Iceland. Until the twentieth century, the Icelandic population relied on fisheries and agriculture, and was from 1262 to 1944 a part of the Norwegian and later the Danish monarchies.

Today, Iceland is a highly developed country, the world's fifth and second in terms of gross domestic product (GDP) per capita and human development respectively. Iceland is a member of the UN, NATO, EEA, and OECD.

Contents

  • 1 Administrative divisions
    • 1.1 Regions
    • 1.2 Constituencies
    • 1.3 Counties
    • 1.4 Municipalities
    • 1.5 Cities and towns
  • 2 Geography
    • 2.1 Location and topography
    • 2.2 Area
    • 2.3 Geological and volcanic activity
    • 2.4 Largest lakes
    • 2.5 Deepest lakes
    • 2.6 Distance to nearest countries and islands
  • 3 Climate
  • 4 Animal and Plant life
  • 5 History
  • 6 Demographics
  • 7 Politics
  • 8 Military
  • 9 Economy
  • 10 Religion
  • 11 Culture
    • 11.1 Miscellaneous
    • 11.2 Cuisine
    • 11.3 Entertainment
    • 11.4 Technology
  • 12 See also
    • 12.1 Geography
    • 12.2 Politics
    • 12.3 Economy
    • 12.4 Culture
    • 12.5 Other
  • 13 References
  • 14 External links

Administrative divisions

Main article: Administrative and electoral divisions of Iceland

Iceland is divided into regions, constituencies, counties, and municipalities.

Regions

Main article: Regions of Iceland

There are eight regions which are primarily used for statistical purposes; the district court jurisdictions also use an older version of this division.[1]

Constituencies

Main article: Constituencies of Iceland

Until 2003, the constituencies for the parliament elections were the same as the regions, but by an amendment to the constitution, they were changed to the current six constituencies:

  • Reykjavík North and Reykjavík South (city regions);
  • Southwest (three suburb areas around Reykjavík);
  • Northwest and Northeast (north half of Iceland, split); and,
  • South (south half of Iceland, excluding Reykjavík and suburbs).

The redistricting change was made in order to balance the weight of different districts of the country, since a vote cast in the sparsely populated areas around the country would count much more than a vote cast in the Reykjavík city area. The imbalance between districts has been reduced by the new system, but still exists.[1]

Counties

Main article: Counties of Iceland

Iceland's twenty-three counties are for the most part historical divisions. Currently, Iceland is split up among twenty-six magistrates that represent government in various capacities. Among their duties are running the local police (except in Reykjavík, where there is a special office of police commissioner), tax collection, administering bankruptcy declarations, and performing civil marriages.[1]

Municipalities

Main article: Municipalities of Iceland

There are seventy-nine municipalities in Iceland which govern most local matters like schools, transportation and zoning.[1]

Regions of Iceland

Constituencies of Iceland

Counties of Iceland

Municipalities of Iceland

Cities and towns

  • Akranes
  • Akureyri
  • Blönduós
  • Bolungarvík
  • Borgarfjörður
  • Breiðdalsvík
  • Dalvík
  • Djúpivogur
  • Egilsstaðir
  • Eskifjörður
  • Eyrarbakki
  • Garðabær
  • Grenivík
  • Grindavík
  • Hafnarfjörður
  • Hella
  • Höfn í Hornafirði
  • Húsavík
  • Hvammstangi
  • Hveragerði
  • Ísafjörður
  • Keflavík
  • Kirkjubæjarklaustur
  • Kópavogur
  • Mosfellsbær
  • Neskaupstaður
  • Njarðvík
  • Ólafsfjörður
  • Ólafsvík
  • Patreksfjörður
  • Raufarhöfn
  • Reyðarfjörður
  • Reykjavík
  • Sauðárkrókur
  • Selfoss
  • Seltjarnarnes
  • Seyðisfjörður
  • Siglufjörður
  • Skagafjörður
  • Stokkseyri
  • Stykkishólmur
  • Suðureyri
  • Vestmannaeyjar
  • Vopnafjörður
  • Þorlákshöfn

Geography

Image:Iceland CIA map trim.gif
CIA Factbook map of Iceland (magnified).
Image:Nasaicelandimage.jpg
Iceland, as seen from space on January 29, 2004. Source: NASA
Main articles: Geography of Iceland and List of settlements in Iceland

Location and topography

Iceland is located in the North Atlantic Ocean just south of the Arctic Circle, which passes through the small island of Grímsey off Iceland's northern coast, but not through mainland Iceland. Unlike neighbouring Greenland, Iceland is considered to be a part of Europe, not of North America, though geologically, the island belongs to both continents. Because of cultural, economic and linguistic similarities, Iceland in many contexts is also included in Scandinavia. It is the world's eighteenth-largest island, and Europe's second largest island following Great Britain.

Approximately eleven percent of the island is glaciated.[2] Many fjords punctuate its 4,970 kilometre (3,088 mi) long coastline, which is also where most towns are situated because the island's interior, the Highlands of Iceland, is a cold and uninhabitable combination of sands and mountains. The major towns are the capital Reykjavík, Keflavík, where the international airport is situated, and Akureyri. The island of Grímsey on the Arctic Circle contains the northernmost habitation of Iceland.[3]

The only native land mammal when humans arrived was the arctic fox. It came to the island at the end of the ice age, walking over the frozen sea. There are no native reptiles or amphibians on the island. There are around 1,300 known species of insects in Iceland, which is rather low compared with other countries (there are about 925,000 known species in the world). During the last Ice Age almost all of the country was covered by permanent snow and glacier ice. This explains the low number of living species in Iceland.

When humans arrived, birch forest and woodland probably covered 25-40% of Iceland’s land area. But soon the settlers started to remove the trees and forests to create fields and grazing land. During the early twentieth century the forests were at their minimum and were almost wiped out of existence. The planting of new forests has increased the number of trees since, but this can not be compared with the original forests. Some of those planted forests have included new foreign species.

Iceland has four national parks: Jökulsárgljúfur National Park, Skaftafell National Park, Snæfellsjökull National Park, and Þingvellir National Park.

Area

  • Whole country: 103,000 km² (39,768.5 mi²)
  • Vegetation: 23,805 km² (9,191 mi²)
  • Lakes: 2,757 km² (1,065 mi²)
  • Glaciers: 11,922 km² (4,603 mi²)
  • Wasteland: 64,538 km² (24,918 mi²)[4]

Geological and volcanic activity

Image:Iceland Grimsvoetn 1972-B.jpg
The volcanic lake of Grímsvötn on the glacier of Vatnajökull.
Image:Iceland Dettifoss 1972-4.jpg
Dettifoss, the most powerful waterfall in Europe, is located in northeastern Iceland.

Iceland is located on both a geological hot spot, thought to be caused by a mantle plume, and the Mid-Atlantic Ridge, which runs right through it. This combined location means that the island is extremely geologically active, having many volcanoes, notably Hekla, Eldgjá, and Eldfell. The volcanic eruption of Laki in 1783-1784 caused a famine that killed nearly a quarter of the island's population; the eruption caused dust clouds and haze to appear over most of Europe and parts of Asia and Africa for several months after the eruption. There are also geysers (a word derived from the name of one in Iceland, Geysir). With this widespread availability of geothermal power, and also because of the numerous rivers and waterfalls that are harnessed for hydropower, residents of most towns have hot water and home heat for a low price. The island itself is composed primarily of basalt, a low-silica lava associated with effusive volcanism like Hawaii. There are, however, a variety of volcano-types on Iceland that produce more evolved lavas such as rhyolite and andesite.

Iceland controls Surtsey, one of the youngest islands in the world. It rose above the ocean in a series of volcanic eruptions between November 8, 1963 and June 5, 1968.[3]

Largest lakes

  • Þórisvatn (Reservoir): 83-88 km² (32-34 mi²)
  • Þingvallavatn: 82 km² (32 mi²)
  • Lögurinn: 53 km² (21 mi²)
  • Mývatn: 37 km² (14 mi²)
  • Hvítárvatn: 30 km² (12 mi²)
  • Hóp: 30 km² (12 mi²)
  • Langisjór: 11.6 km² (4.5 mi²)[4]

Deepest lakes

  • Öskjuvatn: 220 m (722 ft)
  • Hvalvatn: 160 m (525 ft)
  • Jökulsárlón: 150 m (492 ft)
  • Þingvallavatn: 114 m (374 ft)
  • Þórisvatn (Reservoir): 113 m (371 ft)
  • Lögurinn: 112 m (367 ft)
  • Kleifarvatn: 97 m (318 ft)
  • Hvítárvatn: 84 m (276 ft)
  • Langisjór: 75 m (246 ft)[4]

Distance to nearest countries and islands

  • Greenland: 287 km (178 mi)
  • Faroe Islands: 420 km (261 mi)
  • Jan Mayen (Norway): 550 km (342 mi)
  • United Kingdom: 798 km (496 mi)
  • Norway (mainland): 970 km (603 mi)[4]
  • Ireland: 1480 km (920 mi)

Climate

Image:Img 2678.jpg
Strokkur, a geyser in the process of erupting. Lying on the Mid-Atlantic Ridge, Iceland is one of the most geologically active areas on Earth.

The climate of Iceland's coast is cold oceanic. The warm North Atlantic Current ensures generally higher temperatures than in most places of similar latitude in the world. The winters are mild and windy while the summers are damp and cool. Regions in the world with similar climate are: Aleutian Islands, Alaska Peninsula and Tierra del Fuego.

There are some variations in the climate between different parts of the island. Very generally speaking, the south coast is warmer, wetter and windier than the north. Low lying inland areas in the north are the most arid. Snowfall in winters is more common in the north than the south. The Central Highlands are the coldest part of the country.

The highest air temperature recorded was 30.5°C (86.9°F) on 22 June 1939 at Teigarhorn on the southeastern coast. The lowest temperature was -38°C (-36.4°F) on 22 January 1918 at Grímsstaðir and Möðrudalur in the interior of northeast. The temperature records for Reykjavík are 24.8°C (76.6°F) on 11 August 2004, and -24.5°C (-12.1°F) on 21 January 1918.

Mean daily maximum and minimum temperatures (°C) (1961–1990)[5]
Location Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec All
Reykjavík[6] 1.9 2.8 3.2 5.7 9.4 11.7 13.3 13.0 10.1 6.8 3.4 2.2 High 7.0
-3.0 -2.1 -2.0 0.4 3.6 6.7 8.3 7.9 5.0 2.2 -1.3 -2.8 Low 1.9
Akureyri[7] 0.9 1.7 2.1 5.4 9.5 13.2 14.5 13.9 9.9 5.9 2.6 1.3 High 6.7
-5.5 -4.7 -4.2 -1.5 2.3 6.0 7.5 7.1 3.5 0.4 -3.5 -5.1 Low 0.2

Animal and Plant life

Iceland has very few mineral or agricultural resources. Approximately three-quarters of the island is barren of vegetation, and plant life consists mainly of grassland which is regularly grazed by livestock. The only native tree in Iceland is the northern birch Betula pubescens, whose forests were devastated over the centuries for firewood and building supplies. Deforestation then resulted in a loss of critical top soil due to erosion, greatly reducing the ability for the birches to regrow. Today, only a few small birch stands can be found in isolated drainages. The animals of Iceland are mainly agricultural and include Icelandic sheep, cattle, and the sturdy Icelandic horse. Many varieties of fish live in the ocean waters surrounding Iceland, and the fishing industry is a main contributor to Iceland’s economy, accounting for more than half of Iceland’s total exports. Birds are also a very important part of Iceland's animal life. Most of these birds are sea birds. Puffins, skuas, and kittiwakes all nest on Iceland's sea cliffs.

History

Main article: History of Iceland

Although there is some evidence indicating the early presence of Irish monks, it is generally believed that Iceland was found and settled by Norse explorers. Of these, the first was Ingólfur Arnarson, who built his homestead in Reykjavík, which is now the capital of modern day Iceland. Ingólfur was followed by many other emigrant settlers, largely Norsemen and their Irish slaves. By 930, most arable land had been claimed and the Althing, a legislative and judiciary parliament, was founded as the political hub of the Icelandic Free State. The Free State lasted until 1262, at which point the political system devised by the original settlers proved unable to cope with the increasing consolidation of power amongst the Icelandic chieftains. The internal struggles and civil strife of the Sturlungaöld led to the signing of Old Covenant, which brought Iceland under the Norwegian crown. Possession of Iceland passed to Denmark-Norway in the late 14th century when Norway and Denmark were united via the Kalmar Union.

In 1814 , following the Napoleonic Wars, Denmark-Norway was broken up into two seperate kingdoms via the Treaty of Kiel. Iceland, however, remained a Danish dependency. The country's climate worsened during the 19th century, leading to mass emigrations to North America, largely Canada. Meanwhile, a new independence movement arose under the leadership of Jón Sigurðsson, inspired by the romantic and nationalist ideologies of mainland Europe.

In 1874, Denmark granted Iceland home rule, which was expanded in 1904. The Act of Union, an agreement with Denmark made on December 1, 1918, recognized Iceland as a fully sovereign state united with Denmark under a common king.

During World War II, German occupation of Denmark on April 9, 1940 severed communications between Iceland and Denmark. A month later, British military forces sailed into Reykjavík harbour, beginning the invasion and occupation of Iceland by Allied forces which would last throughout the war. In the summer of 1941, the British left and the occupation was taken over by the United States army. With American assistance, and following a plebiscite, Iceland formally became an independent republic on June 17, 1944. American troops remained stationed in Iceland as part of a defence agreement until the autumn of 2006.

Demographics

Main article: Demographics of Iceland

The original population of Iceland was of Nordic and Celtic origin. This is evident by literary evidence from the settlement period as well as from later scientific studies such as blood type and genetic analysis. One such genetics study has indicated that the majority of the male settlers were of Nordic origin while the majority of the women were of Celtic origin.[8] The modern population of Iceland is often described as a "homogeneous mixture of descendants of Norse and Celts" but some history scholars reject the alleged homogeneity as a myth that fails to take into account the fact that Iceland was never completely isolated from the rest of Europe and actually has had a lot of contact with traders and fishermen from many nations through the ages.

Iceland has extensive genealogical records about its population dating back to the age of settlement. Although the accuracy of these records is debated, biopharmaceutical companies such as deCODE Genetics see them as a valuable tool for conducting research on genetic diseases.

The population of the island is believed to have varied from 40,000 to 60,000 in the period from initial settlement until the mid-19th century. During that time, cold winters, ashfall from volcanic eruptions, and plagues adversely affected the population several times. The first census was carried out in 1703 and revealed that the population of the island was then 50,358. Improving living conditions triggered a rapid increase in population from the mid-19th century to the present day - from about 60,000 in 1850 to 300,000 in 2006.

In 2004, 20,669 people (7% of the total population) who were living in Iceland had been born abroad, including children of Icelandic parents living abroad. 10,636 people (3.6% of the total population) had foreign citizenship. The most populous nationalities are Poles (7,000), Danes (890), ex-Yugoslavians (670), Filipinos (647) and Germans (540).

The island's spoken language is Icelandic, a North Germanic language. In terms of etymology, the Icelandic language is the closest to Old Norse, the language of the Vikings. Today, the closest language still in existence to Icelandic is Faroese. In education, the use of Icelandic Sign Language for the Deaf in Iceland is regulated by the National Curriculum Guide. The predominant religion is Lutheran.

Prominent foreign languages include English, Danish, other Scandinavian languages and German.

The southwest corner of Iceland is the most densely populated region and the location of the capital Reykjavík, the northernmost capital in the world. The largest towns outside the capital region are Akureyri and Reykjanesbær.

Politics

Main article: Politics of Iceland
Image:Ogrimsson.jpg
Ólafur Ragnar Grímsson, President of Iceland.

The modern parliament, called "Alþingi" (English: Althing), was founded in 1845 as an advisory body to the Danish king. It was widely seen as a reestablishment of the assembly founded in 930 in the Commonwealth period and suspended in 1799. It currently has sixty-three members, each of whom is elected by the population every four years. The president of Iceland is a largely ceremonial office that serves as a diplomat, figurehead and head of state. The head of government is the prime minister, who, together with the cabinet, takes care of the executive part of government. The cabinet is appointed by the president after general elections to Althing; however, this process is usually conducted by the leaders of the political parties, who decide among themselves after discussions which parties can form the cabinet and how its seats are to be distributed (under the condition that it has a majority support in Althing). Only when the party leaders are unable to reach a conclusion by themselves in reasonable time does the president exercise this power and appoint the cabinet himself. This has never happened since the republic was founded in 1944, but in 1942 the regent of the country (Sveinn Björnsson, who had been installed in that position by the Althing in 1941) did appoint a non-parliamentary government. The regent had, for all practical purposes, the position of a president, and Björnsson in fact became the country's first president in 1944. The governments of Iceland have almost always been coalitions with two or more parties involved, due to the fact that no single political party has received a majority of seats in Althing in the republic period. The extent of the political powers possessed by the office of the president are disputed by legal scholars in Iceland; several provisions of the constitution appear to give the president some important powers but other provisions and traditions suggest differently. Iceland had elected the first female president ever, Vigdís Finnbogadóttir in 1980 and she retired from office in 1996. Elections for the office of presidency, parliament and in town councils are all held every four years, last held in 2004, 2003 and 2006, respectively.

Military

Image:Icelandic troops.jpg
Two Icelandic sergeants of the ICRU, the only Icelandic military force sent to the International Security Assistance Force, in discussion with General Richards, commander of ISAF peacekeeping mission in Afghanistan.
Main article: Military of Iceland

Iceland, a NATO member, does not have a standing army and hasn't had one since the nineteenth century, although it has an expeditionary military peacekeeping unit known as the Icelandic Crisis Response Unit or Íslenska Friðargæslan.

Iceland has a Coast Guard (Landhelgisgæslan) which operates armed Offshore Patrol Vessels as well as aircraft and a counter-terrorism team named Sérsveit Ríkislögreglustjóra (English: "The Special Operations Task Force of the National Commissioner of the Icelandic Police"), commonly referred to as Víkingasveitin (The Viking Team or Viking Squad) similar to the German GSG 9. The Icelandic National Police consists of over 700 officers and unpaid volunteer Rescue and Civil Defence Units have more than 4,000 active members and have overall 18,000 registered members.

From 1951 until 2006 Military Defenses were provided by a predominantly United States-manned Defense force in the NATO base on Miðnesheiði near Keflavík.[1] This base is now in the hands of the Sheriff of Keflavík Airport. An Air Defence radar network, known as the Iceland Air Defence System (IADS) or Íslenska Loftvarnarkerfið is operated by Ratsjárstofnun.[9]

Economy

Main article: Economy of Iceland

Iceland is the fifth most productive country in the world based on GDP per capita at purchasing power parity. It is also ranked second on the 2005 United Nations Human Development Index. The economy historically depended heavily on the fishing industry, which still provides almost 40% of export earnings and employs 8% of the work force. In the absence of other natural resources (except for abundant hydro-electric and geothermal power), Iceland's economy is vulnerable to changing world fish prices. The economy remains sensitive to declining fish stocks as well as to drops in world prices for its main material exports: fish and fish products, aluminium, and ferrosilicon. Although the Icelandic economy still relies heavily on fishing it is constantly becoming less important as the travel industry and other service, technology, energy intensive and various other industries grow.

Image:Route1(iceland).png
The Ring Road of Iceland and some towns it passes through.

1.Reykjavík, 2.Borgarnes, 3.Blönduós, 4.Akureyri,
5.Egilsstaðir, 6.Höfn, 7.Selfoss

The centre-right government plans to continue its policies of reducing the budget and current account deficits, limiting foreign borrowing, containing inflation, revising agricultural and fishing policies, diversifying the economy, and privatising state-owned industries. The government remains opposed to EU membership, primarily because of Icelanders' concern about losing control over their fishing resources.

Iceland's economy has been diversifying into manufacturing and service industries in the last decade, and new developments in software production, biotechnology, and financial services are taking place. The tourism sector is also expanding, with the recent trends in ecotourism and whale-watching. Growth slowed between 2000 and 2002, but the economy expanded by 4.3% in 2003 and grew by 6.2% in 2004. The unemployment rate of 1.8% (third quarter of 2005) is among the lowest in the European Economic Area.

Over 99% of the country's electricity is produced from hydropower and geothermal energy.[10]

Iceland's agriculture industry consists mainly of potatoes, turnips, green vegetables (in greenhouses), mutton, dairy products and fish.[10] Some are examining the possibility of introducing other crops from South America, where the potato is native. Given that summers in Iceland are not hot enough to produce some other types of food, those plants that are from the same ecological range as the potato (those from a similar climate to Iceland), may very probably be adaptable to Iceland. Those of interest include the quinoa, a pseudocereal; beach strawberry, a fruit ; calafate, a fruit; and the Monkey-puzzle araucaria, a tree that produces edible nuts. Those crops would help the country to reduce imports of food like cereals, fruits, and nuts.

Iceland's stock market, the Iceland Stock Exchange (ISE), was established in 1985.

Borgartún is the name of the financial center in Reykjavik, hosting a large number of companies and three investment banks.

Religion

Image:Reykjavik-leaf-church01.GIF
Hallgrímskirkja, Church of Hallgrímur, in Reykjavík, Iceland.
Main article: Religion in Iceland

Icelanders enjoy freedom of religion as stated by the constitution; however, church and state are not separated and the National Church of Iceland, a Lutheran body, is the state church. The national registry keeps account of the religious affiliation of every Icelandic citizen and according to it, Icelanders in 2005 divided into religious groups as follows:

  • 82.1% members of the National Church of Iceland.
  • 4.7% members of the Free Lutheran Churches of Reykjavík and Hafnarfjörður.
  • 2.6% not members of any religious group.
  • 2.4% members of the Roman Catholic Church, which has a Diocese of Reykjavík
  • 5.5% members of unregistered religious organisations or with no specified religious affiliation

The remaining 2.7% is mostly divided between around 20-25 other Christian denominations and sects, with less than 1% of the population in non-Christian religious organisations including a tiny group of state-sanctioned indigenous Ásatrú adherents in the Íslenska Ásatrúarfélagið.[11]

Culture

Image:Grímsey Iceland.JPG
Cliffs at the island of Grímsey, on the Arctic Circle.
Main article: Culture of Iceland

Miscellaneous

Some famous Icelanders include alternative rock band