Iceland

Iceland ; Icelandic: Ísland pronounced is a Nordic island country of Europe located in the North Atlantic Ocean. It has a population of 332,529 and an area of 103,000 km2 (40,000 sq mi), making it the most sparsely populated country in Europe. The capital and largest city is Reykjavík. Reykjavík and the surrounding areas in the southwest of the country are home to over two-thirds of the population.

Iceland is volcanically and geologically active. The interior consists of a plateau characterised by sand and lava fields, mountains and glaciers, while many glacial rivers flow to the sea through the lowlands. Iceland is warmed by the Gulf Stream and has a temperate climate, despite a high latitude just outside the Arctic Circle. Its high latitude and marine influence keep summers chilly, with most of the archipelago having a tundra climate.

According to the ancient manuscript Landnámabók, the settlement of Iceland began in 874 AD when the Norwegian chieftain Ingólfr Arnarson became the first permanent settler on the island. In the following centuries, Norwegians, and to a lesser extent other Scandinavians, emigrated to Iceland, bringing with them thralls of Gaelic origin. The island was governed as an independent commonwealth under the Althing, one of the world's oldest functioning legislative assemblies. Following a period of civil strife, Iceland acceded to Norwegian rule in the 13th century. The establishment of the Kalmar Union in 1397 united the kingdoms of Norway, Denmark and Sweden. Iceland thus followed Norway's integration to that Union and came under Danish rule after Sweden's secession from that union in 1523. Although the Danish kingdom introduced Lutheranism forcefully in 1550, Iceland remained a distant semi-colonial territory in which Danish institutions and infrastructures were conspicuous by their absence. In the wake of the French revolution and the Napoleonic wars, Iceland's struggle for independence took form and culminated in independence in 1918 and the founding of a republic in 1944. Until the 20th century, Iceland relied largely on subsistence fishing and agriculture, and was among the poorest in Europe. Industrialisation of the fisheries and Marshall Plan aid following World War II brought prosperity, and Iceland became one of the wealthiest and most developed nations in the world. In 1994, it became a part of the European Economic Area, which further diversified the economy into sectors such as finance, biotechnology, and manufacturing.

Iceland has a market economy with relatively low taxes compared to other OECD countries. It maintains a Nordic social welfare system that provides universal health care and tertiary education for its citizens. Iceland ranks high in economic, political and social stability and equality. In 2016, it was ranked as the 9th most developed country in the world by the United Nations' Human Development Index, and ranks first on the Global Peace Index. Iceland runs almost completely on renewable energy. Affected by the ongoing worldwide financial crisis, the nation's entire banking system systemically failed in October 2008, leading to a severe depression, substantial political unrest, the Icesave dispute, and the institution of capital controls. Some bankers were jailed. Since then, the economy has made a significant recovery, in large part due to a surge in tourism.

Icelandic culture is founded upon the nation's Scandinavian heritage. Most Icelanders are descendants of Germanic and Gaelic settlers. Icelandic, a North Germanic language, is descended from Old Norse and is closely related to Faroese and West Norwegian dialects. The country's cultural heritage includes traditional Icelandic cuisine, Icelandic literature and medieval sagas. Iceland has the smallest population of any NATO member and is the only one with no standing army, with the lightly armed coast guard in charge of defence.

History

Settlement and Commonwealth 874–1262

According to both Landnámabók and Íslendingabók, Celtic monks known as the Papar lived in Iceland before Scandinavian settlers arrived, possibly members of a Hiberno-Scottish mission. Recent archaeological excavations have revealed the ruins of a cabin in Hafnir on the Reykjanes peninsula. Carbon dating indicates that it was abandoned sometime between 770 and 880. In 2016, archeologists uncovered a longhouse in Stöðvarfjörður that has been dated to as early as 800.

Swedish Viking explorer Garðar Svavarsson was the first to circumnavigate Iceland in 870 and establish that it was an island. He stayed over winter and built a house in Húsavík. Garðar departed the following summer but one of his men, Náttfari, decided to stay behind with two slaves. Náttfari settled in what is now known as Náttfaravík and he and his slaves became the first permanent residents of Iceland.

The Norwegian-Norse chieftain Ingólfr Arnarson built his homestead in present-day Reykjavík in 874. Ingólfr was followed by many other emigrant settlers, largely Scandinavians and their thralls, many of whom were Irish or Scottish. By 930, most arable land on the island had been claimed; the Althing, a legislative and judicial assembly, was initiated to regulate the Icelandic Commonwealth. Lack of arable land also served impetus to the settlement of Greenland starting in 986. The period of these early settlements coincided with the Medieval Warm Period, when temperatures were similar to those of the early 20th century. At this time, about 25% of Iceland was covered with forest, compared to 1% in the present day. Christianity was adopted by consensus around 999–1000, although Norse paganism persisted among some segments of the population for some years afterwards.

The Middle Ages

The Icelandic Commonwealth lasted until the 13th century, when the political system devised by the original settlers proved unable to cope with the increasing power of Icelandic chieftains. The internal struggles and civil strife of the Age of the Sturlungs led to the signing of the Old Covenant in 1262, which ended the Commonwealth and brought Iceland under the Norwegian crown. Possession of Iceland passed from the Norwegian Empire to the Kalmar Union in 1415, when the kingdoms of Norway, Denmark and Sweden were united. After the break-up of the union in 1523, it remained a Norwegian dependency, as a part of Denmark–Norway.

In the ensuing centuries, Iceland became one of the poorest countries in Europe. Infertile soil, volcanic eruptions, deforestation and an unforgiving climate made for harsh life in a society where subsistence depended almost entirely on agriculture. The Black Death swept Iceland twice, first in 1402–1404 and again in 1494–1495. The former outbreak killed 50% to 60% of the population, and the latter 30% to 50%.

Reformation and the Early Modern period

Around the middle of the 16th century, as part of the Protestant Reformation, King Christian III of Denmark began to impose Lutheranism on all his subjects. Jón Arason, the last Catholic bishop of Hólar, was beheaded in 1550 along with two of his sons. The country subsequently became officially Lutheran and Lutheranism has since remained the dominant religion.

In the 17th and 18th centuries, Denmark imposed harsh trade restrictions on Iceland. Natural disasters, including volcanic eruption and disease, contributed to a decreasing population. Pirates from several countries, including the Barbary Coast, raided Iceland's coastal settlements and abducted people into slavery. A great smallpox epidemic in the 18th century killed around a third of the population. In 1783 the Laki volcano erupted, with devastating effects. In the years following the eruption, known as the Mist Hardships (Icelandic: Móðuharðindin), over half of all livestock died in the country. Around a quarter of the population died in the ensuing famine.

Independence movement 1814–1918

In 1814, following the Napoleonic Wars, Denmark-Norway was broken up into two separate kingdoms via the Treaty of Kiel but Iceland remained a Danish dependency. Throughout the 19th century, the country's climate continued to grow colder, resulting in mass emigration to the New World, particularly to the region of Gimli, Manitoba in Canada, which was sometimes referred to as New Iceland. About 15,000 people emigrated, out of a total population of 70,000.

A national consciousness arose in the first half of the 19th century, inspired by romantic and nationalist ideas from mainland Europe. An Icelandic independence movement took shape in the 1850s under the leadership of Jón Sigurðsson, based on the burgeoning Icelandic nationalism inspired by the Fjölnismenn and other Danish-educated Icelandic intellectuals. In 1874, Denmark granted Iceland a constitution and limited home rule. This was expanded in 1904, and Hannes Hafstein served as the first Minister for Iceland in the Danish cabinet.

Kingdom of Iceland 1918–1944

The Danish–Icelandic Act of Union, an agreement with Denmark signed on 1 December 1918 and valid for 25 years, recognised Iceland as a fully sovereign state in a personal union with Denmark. The Government of Iceland established an embassy in Copenhagen and requested that Denmark handle Icelandic foreign policy. Danish embassies around the world displayed two coats of arms and two flags: those of the Kingdom of Denmark and those of the Kingdom of Iceland.

During World War II, Iceland joined Denmark in asserting neutrality. After the German occupation of Denmark on 9 April 1940, the Althing replaced the King with a regent and declared that the Icelandic government would take control of foreign affairs and other matters previously handled by Denmark. A month later, British armed forces invaded and occupied the country, violating Icelandic neutrality. In 1941, the occupation was taken over by the United States so that Britain could use its troops elsewhere.

Independent republic 1944–present

On 31 December 1943, the Danish–Icelandic Act of Union expired after 25 years. Beginning on 20 May 1944, Icelanders voted in a four-day plebiscite on whether to terminate the personal union with Denmark, abolish the monarchy, and establish a republic. The vote was 97% to end the union, and 95% in favour of the new republican constitution. Iceland formally became a republic on 17 June 1944, with Sveinn Björnsson as its first president.

In 1946, the Allied occupation force left Iceland. The nation formally became a member of NATO on 30 March 1949, amid domestic controversy and riots. On 5 May 1951, a defence agreement was signed with the United States. American troops returned to Iceland as the Iceland Defence Force, and remained throughout the Cold War. The US withdrew the last of its forces on 30 September 2006.

Iceland had prospered during the war. The immediate post-war period was followed by substantial economic growth, driven by industrialisation of the fishing industry and the US Marshall Plan programme, through which Icelanders received the most aid per capita of any European country (at USD 209, with the war-ravaged Netherlands a distant second at USD 109).

The 1970s were marked by the Cod Wars — several disputes with the United Kingdom over Iceland's extension of its fishing limits to 200 nmi (370 km) offshore. Iceland hosted a summit in Reykjavík in 1986 between United States President Ronald Reagan and Soviet Premier Mikhail Gorbachev, during which they took significant steps toward nuclear disarmament. A few years later, Iceland became the first country to recognize the independence of Estonia, Latvia, and Lithuania as they broke away from the USSR. Throughout the 1990s, the country expanded its international role and developed a foreign policy oriented toward humanitarian and peacekeeping causes. To that end, Iceland provided aid and expertise to various NATO-led interventions in Bosnia, Kosovo, and Iraq.

Iceland joined the European Economic Area in 1994, after which the economy was greatly diversified and liberalised. International economic relations increased further after 2001, when Iceland's newly deregulated banks began to raise massive amounts of external debt, contributing to a 32% increase in Iceland's gross national income between 2002 and 2007.

Economic boom and crisis

In 2003–2007, following the privatisation of the banking sector under the government of Davíð Oddsson, Iceland moved toward having an economy based on international investment banking and financial services. It was quickly becoming one of the most prosperous countries in the world but was hit hard by a major financial crisis. The crisis resulted in the greatest migration from Iceland since 1887, with a net emigration of 5,000 people in 2009. Iceland's economy stabilised under the government of Jóhanna Sigurðardóttir, and grew by 1.6% in 2012. Many Icelanders, however, have remained unhappy with the state of the economy and government austerity policies. The centre-right Independence Party was returned to power in coalition with the Progressive Party in the 2013 elections. In the following years, Iceland saw a surge in tourism as the country became a popular holiday destination. In 2016, Prime Minister Sigmundur David Gunnlaugsson resigned after being implicated in the Panama Papers scandal. Early elections in 2016 resulted in a right-wing coalition government of the Independence Party, the Reform Party and Bright Future.

Geography

For more details on this topic, see Geography of Iceland.

Iceland is at the juncture of the North Atlantic and Arctic Oceans. The main island is entirely south of the Arctic Circle, which passes through the small Icelandic island of Grímsey off the main island's northern coast. The country lies between latitudes 63 and 68°N, and longitudes 25 and 13°W.

Iceland is closer to continental Europe than to mainland North America; thus, the island is generally included in Europe for historical, political, cultural, and practical reasons. Geologically, the island includes parts of both continental plates. The closest body of land is Greenland (290 km, 180 mi). The closest bodies of land in Europe are the Faroe Islands (420 km, 260 mi); Jan Mayen Island (570 km, 350 mi); Shetland and the Outer Hebrides, both about 740 km (460 mi); and the Scottish mainland and Orkney, both about 750 km (470 mi). The mainland of Norway is about 970 km (600 mi) away.

Iceland is the world's 18th largest island, and Europe's second-largest island after Great Britain. The main island is 101,826 km2 (39,315 sq mi), but the entire country is 103,000 km2 (39,768.5 sq mi) in size, of which 62.7% is tundra. About 30 minor islands are in Iceland, including the lightly populated Grímsey and the Vestmannaeyjar archipelago. Lakes and glaciers cover 14.3% of its surface; only 23% is vegetated. The largest lakes are Þórisvatn reservoir: 83–88 km2 (32–34 sq mi) and Þingvallavatn: 82 km2 (32 sq mi); other important lakes include Lagarfljót and Mývatn. Jökulsárlón is the deepest lake, at 248 m (814 ft).

Geologically, Iceland is part of the Mid-Atlantic Ridge, a ridge along which the oceanic crust spreads and forms new oceanic crust. This part of the mid-ocean ridge is located above a mantle plume, causing Iceland to be subaerial (above the surface of the sea). The ridge marks the boundary between the Eurasian and North American Plates, and Iceland was created by rifting and accretion through volcanism along the ridge.

Many fjords punctuate Iceland's 4,970-km-long (3,088-mi) coastline, which is also where most settlements are situated. The island's interior, the Highlands of Iceland, is a cold and uninhabitable combination of sand, mountains, and lava fields. The major towns are the capital city of Reykjavík, along with its outlying towns of Kópavogur, Hafnarfjörður, and Garðabær, nearby Reykjanesbær where the international airport is located, and the town of Akureyri in northern Iceland. The island of Grímsey on the Arctic Circle contains the northernmost habitation of Iceland, whereas Kolbeinsey contains the northernmost point of Iceland. Iceland has three national parks: Vatnajökull National Park, Snæfellsjökull National Park, and Þingvellir National Park. The country is considered a "strong performer" in environmental protection, having been ranked 13th in Yale University's Environmental Performance Index of 2012.

• Iceland as seen from space on 29 January 2004

• Suðureyri

• Norðfjörður

• The eruption of Eyjafjallajökull

• South of Iceland, off the Ring Road, looking north, late afternoon in winter 2001

Geology

A geologically young land, Iceland is located on both the Iceland hotspot and the Mid-Atlantic Ridge, which runs right through it. This location means that the island is highly geologically active with many volcanoes, notably Hekla, Eldgjá, Herðubreið, and Eldfell. The volcanic eruption of Laki in 1783–1784 caused a famine that killed nearly a quarter of the island's population. In addition, the eruption caused dust clouds and haze to appear over most of Europe and parts of Asia and Africa for several months afterward, and affected climates in other areas.

Iceland has many geysers, including Geysir, from which the English word is derived, and the famous Strokkur, which erupts every 8–10 minutes. After a phase of inactivity, Geysir started erupting again after a series of earthquakes in 2000. Geysir has since grown quieter and does not erupt often.

With the widespread availability of geothermal power, and the harnessing of many rivers and waterfalls for hydroelectricity, most residents have access to inexpensive hot water, heating, and electricity. The island is composed primarily of basalt, a low-silica lava associated with effusive volcanism as has occurred also in Hawaii. Iceland, however, has a variety of volcanic types (composite and fissure), many producing more evolved lavas such as rhyolite and andesite. Iceland has hundreds of volcanoes with about 30 active volcanic systems.

Surtsey, one of the youngest islands in the world, is part of Iceland. Named after Surtr, it rose above the ocean in a series of volcanic eruptions between 8 November 1963 and 5 June 1968. Only scientists researching the growth of new life are allowed to visit the island.

On 21 March 2010, a volcano in Eyjafjallajökull in the south of Iceland erupted for the first time since 1821, forcing 600 people to flee their homes. Additional eruptions on 14 April forced hundreds of people to abandon their homes. The resultant cloud of volcanic ash brought major disruption to air travel across Europe.

Another large eruption occurred on 21 May 2011. This time it was the Grímsvötn volcano, located under the thick ice of Europe's largest glacier, Vatnajökull. Grímsvötn is one of Iceland's most active volcanoes, and this eruption was much more powerful than the 2010 Eyjafjallajökull activity, with ash and lava hurled 20 km (12 mi) into the atmosphere, creating a large cloud.

The highest elevation for Iceland is listed as 2,110 m (6,923 ft) at Hvannadalshnúkur (64°00′N 16°39′W).

Biodiversity

Around 1,300 species of insects are known in Iceland, which is low compared with other countries (over one million species have been described worldwide). Notably, Iceland is essentially free of mosquitoes. The only native land mammal when humans arrived was the Arctic fox, which came to the island at the end of the ice age, walking over the frozen sea. On rare occasions, bats have been carried to the island with the winds, but they are not able to breed there. Polar bears occasionally come over from Greenland, but they are just visitors, and no Icelandic populations exist. No native or free-living reptiles or amphibians are on the island.

Phytogeographically, Iceland belongs to the Arctic province of the Circumboreal Region within the Boreal Kingdom. Around three-quarters of the island is barren of vegetation; plant life consists mainly of grassland, which is regularly grazed by livestock. The most common tree native to Iceland is the northern birch (Betula pubescens), which formerly formed forests over much of Iceland, along with aspens (Populus tremula), rowans (Sorbus aucuparia), common junipers (Juniperus communis), and other smaller trees, mainly willows.

When the island was first settled, it was extensively forested. In the late 12th century, Ari the Wise described it in the Íslendingabók as "forested from mountain to sea shore". Permanent human settlement greatly disturbed the isolated ecosystem of thin, volcanic soils and limited species diversity. The forests were heavily exploited over the centuries for firewood and timber. Deforestation, climatic deterioration during the Little Ice Age, and overgrazing by sheep imported by settlers caused a loss of critical topsoil due to erosion. Today, many farms have been abandoned. Three-quarters of Iceland's 100,000 square kilometres is affected by soil erosion, 18,000 km2 (6,900 sq mi) serious enough to make the land useless. Only a few small birch stands now exist in isolated reserves. The planting of new forests has increased the number of trees, but the result does not compare to the original forests. Some of the planted forests include introduced species. The tallest tree in Iceland is a sitka spruce planted in 1949 in Kirkjubæjarklaustur; it was measured at 25.2 m (83 ft) in 2013.

The animals of Iceland include the Icelandic sheep, cattle, chickens, goats, the sturdy Icelandic horse, and the Icelandic Sheepdog, all descendants of animals imported by Europeans. Wild mammals include the Arctic fox, mink, mice, rats, rabbits, and reindeer. Polar bears occasionally visit the island, travelling on icebergs from Greenland. In June 2008, two polar bears arrived in the same month. Marine mammals include the grey seal (Halichoerus grypus) and harbor seal (Phoca vitulina). Many species of fish live in the ocean waters surrounding Iceland, and the fishing industry is a major part of Iceland's economy, accounting for roughly half of the country's total exports. Birds, especially seabirds, are an important part of Iceland's animal life. Puffins, skuas, and kittiwakes nest on its sea cliffs.

Commercial whaling is practised intermittently along with scientific whale hunts. Whale watching has become an important part of Iceland's economy since 1997.

Culture

Icelandic culture has its roots in North Germanic traditions. Icelandic literature is popular, in particular the sagas and eddas that were written during the High and Late Middle Ages. Centuries of isolation have helped to insulate the country's Nordic culture from external influence; a prominent example is the preservation of the Icelandic language, which remains the closest to Old Norse of all modern Nordic languages.

In contrast to other Nordic countries, Icelanders place relatively great importance on independence and self-sufficiency; in a public opinion analysis conducted by the European Commission, over 85% of Icelanders believe independence is "very important," compared to 47% of Norwegians, 49% of Danes, and an average of 53% for the EU25. Icelanders also have a very strong work ethic, working some of the longest hours of any industrialised nation.

According to a poll conducted by the OECD, 66% of Icelanders were satisfied with their lives, while 70% believed that their lives will be satisfying in the future. Similarly, 83% reported having more positive experiences in an average day than negative ones, compared to an OECD average of 72%, which makes Iceland one of the happiest countries in the OECD. A more recent 2012 survey found that around three quarters of respondents stated they were satisfied with their lives, compared to a global average of about 53%.

Iceland is liberal with regard to LGBT rights issues. In 1996, the Icelandic parliament passed legislation to create registered partnerships for same-sex couples, conferring nearly all the rights and benefits of marriage. In 2006, parliament voted unanimously to grant same-sex couples the same rights as heterosexual couples in adoption, parenting and assisted insemination treatment. On 11 June 2010, the Icelandic parliament amended the marriage law, making it gender neutral and defining marriage as between two individuals, making Iceland one of the first countries in the world to legalise same-sex marriages. The law took effect on 27 June 2010. The amendment to the law also means registered partnerships for same-sex couples are now no longer possible, and marriage is their only option—identical to the existing situation for opposite-sex couples.

Icelanders are known for their deep sense of community: an OECD survey found that 98% believe they know someone they could rely on in a time of need, higher than in any other industrialised country. Similarly, only 6% reported "rarely" or "never" socializing with others. This high level of social cohesion is attributed to the small size and homogeneity of the population, as well as to a long history of harsh survival in an isolated environment, which reinforced the importance of unity and cooperation.

Egalitarianism is highly valued among the people of Iceland, with income inequality being among the lowest in the world. The constitution explicitly prohibits the enactment of noble privileges, titles, and ranks. Everyone is addressed by their first name. As in other Nordic countries, equality between the sexes is very high; Iceland is consistently ranked among the top three countries in the world for women to live in.

Art

The distinctive rendition of the Icelandic landscape by its painters can be linked to nationalism and the movement for home rule and independence, which was very active in the mid-19th century.

Contemporary Icelandic painting is typically traced to the work of Þórarinn Þorláksson, who, following formal training in art in the 1890s in Copenhagen, returned to Iceland to paint and exhibit works from 1900 to his death in 1924, almost exclusively portraying the Icelandic landscape. Several other Icelandic men and women artists studied at Royal Danish Academy of Fine Arts at that time, including Ásgrímur Jónsson, who together with Þórarinn created a distinctive portrayal of Iceland's landscape in a romantic naturalistic style. Other landscape artists quickly followed in the footsteps of Þórarinn and Ásgrímur. These included Jóhannes Kjarval and Júlíana Sveinsdóttir. Kjarval in particular is noted for the distinct techniques in the application of paint that he developed in a concerted effort to render the characteristic volcanic rock that dominates the Icelandic environment. Einar Hákonarson is an expressionistic and figurative painter who by some is considered to have brought the figure back into Icelandic painting. In the 1980s, many Icelandic artists worked with the subject of the new painting in their work.

In the recent years artistic practice has multiplied, and the Icelandic art scene has become a setting for many large scale projects and exhibitions. The artist run gallery space Kling og Bang, members of which later ran the studio complex and exhibition venue Klink og Bank, has been a significant part of the trend of self-organised spaces, exhibitions and projects. The Living Art Museum, Reykjavík Municipal Art Museum, Reykjavík Art Museum and the National Gallery of Iceland are the larger, more established institutions, curating shows and festivals.

• Þingvellir by Þórarinn B. Þorláksson

• Statue of Thorfinn Karlsefni by Icelandic sculptor Einar Jónsson in Philadelphia

• The writer Halldór Laxness by Einar Hákonarson, 1984

• Traditional Icelandic turf houses. Until the 20th century, the vast majority of Icelanders lived in rural areas

• The old building (Gamli Skóli) of the Menntaskóli, i.e. High School precinct in Akureyri

Music

Much Icelandic music is related to Nordic music, and includes folk and pop traditions, medieval music group Voces Thules, alternative and indie rock bands The Sugarcubes and Of Monsters and Men, jazz fusion band Mezzoforte, musicians Björk, Hafdís Huld, Sóley, and Emilíana Torrini, and post-rock band Sigur Rós. The national anthem of Iceland is Lofsöngur, written by Matthías Jochumsson, with music by Sveinbjörn Sveinbjörnsson.

Traditional Icelandic music is strongly religious. Hymns, both religious and secular, are a particularly well-developed form of music, due to the scarcity of musical instruments throughout much of Iceland's history. Hallgrímur Pétursson wrote many Protestant hymns in the 17th century. Icelandic music was modernised in the 19th century, when Magnús Stephensen brought pipe organs, which were followed by harmoniums. Other vital traditions of Icelandic music are epic alliterative and rhyming ballads called rímur. Rímur are epic tales, usually a cappella, which can be traced back to skaldic poetry, using complex metaphors and elaborate rhyme schemes. The best known rímur poet of the 19th century was Sigurður Breiðfjörð (1798–1846). A modern revitalisation of the tradition began in 1929 with the formation of Iðunn.[clarification needed]

Icelandic contemporary music consists of bands ranging from pop-rock groups such as Bang Gang, Quarashi and Amiina to solo ballad singers like Bubbi Morthens. Independent music is strong in Iceland, with bands such as múm and solo artists.

Some Icelandic jazz musicians and jazz bands have earned a reputation outside Iceland. Perhaps best known is the jazz fusion band Mezzoforte and vocalist Anna Mjöll. Many Icelandic artists and bands have enjoyed international success, most notably Björk and Sigur Rós but also Quarashi, Hera, Ampop, Mínus and múm. The main music festival is arguably Iceland Airwaves, an annual event on the Icelandic music scene, where Icelandic bands along with foreign ones play in the clubs of Reykjavík for a week. Electronic musicians include ones such as Thor and GusGus.

Among Iceland's best-known classical composers are Daníel Bjarnason and Anna S. Þorvaldsdóttir (Anna Thorvaldsdottir), who in 2012 received the Nordic Council Music Prize and in 2015 was chosen as the New York Philharmonic's Kravis Emerging Composer, an honor that includes a $50,000 cash prize and a commission to write a composition for the orchestra; she is the second recipient.

Cuisine

Much of Iceland's cuisine is based on fish, lamb, and dairy products, with little to no utilization of herbs or spices. Due to the island's climate, fruits and vegetables are not generally a component of traditional dishes, although the use of greenhouses has made them more common in contemporary food. Þorramatur is a selection of traditional cuisine consisting of many dishes, and is usually consumed around the month of Þorri, which begins on the first Friday after 19 January. Traditional dishes also include skyr, hákarl (cured shark), cured ram, singed sheep heads, and black pudding, Flatkaka (flat bread), dried fish and dark rye bread traditionally baked in the ground in geothermal areas. Puffin is considered a local delicacy that is often prepared through broiling.

Breakfast usually consists of pancakes, cereal, fruit, and coffee, while lunch may take the form of a smörgåsbord. The main meal of the day for most Icelanders is dinner, which usually involves fish or lamb as the main course. Seafood is central to most Icelandic cooking, particularly cod and haddock but also salmon, herring, and halibut. It is often prepared in a wide variety of ways, either smoked, pickled, boiled, or dried. Lamb is by far the most common meat, and it tends to be either smoke-cured (known as hangikjöt) or salt-preserved (saltkjöt). Many older dishes make use of every part of the sheep, such as slátur, which consists of offal (internal organs and entrails) minced together with blood and served in sheep stomach. Additionally, boiled or mashed potatoes, pickled cabbage, green beans, and rye bread are prevalent side dishes.

Coffee is a popular beverage in Iceland, and is drunk at breakfast, after meals, and with a light snack in mid-afternoon. Coca-Cola is also widely consumed, to the extent that the country is said to have one of the highest per capita consumption rates in the world. Iceland's signature alcoholic beverage is Brennivín (literally "burnt (i.e. distilled wine"), which is similar to Scandinavian akvavit. It is a type of vodka made from distilled potatoes and flavoured with either caraway seeds or angelica. Its potency has earned it the nickname svarti dauði ("Black Death").