Greenland facts for kids
Quick facts for kids
Greenland
Kalaallit Nunaat (Greenlandic) Grønland (Danish)
|
|||
|---|---|---|---|
|
|||
| Anthem: "Nunarput, utoqqarsuanngoravit" (Greenlandic) "Vort ældgamle land under isblinkens bavn" (Danish) "You Our Ancient Land" |
|||
| Kalaallit song: "Nuna asiilasooq" (Greenlandic) "The Land of Great Length" Royal anthems: Der er et yndigt land (Danish) (English: "There is a lovely country") |
|||
.svg)
Location of Greenland (dark green)
in the Kingdom of Denmark (light green) |
|||
| Sovereign state | Kingdom of Denmark | ||
| Union with Norway | 1262 | ||
| Danish-Norwegian recolonization | 1721 | ||
| Unification with Denmark | 14 January 1814 | ||
| Home rule | 1 May 1979 | ||
| Further autonomy and self rule | 21 June 2009 | ||
| Capital
and largest city
|
Nuuk 64°10′N 51°44′W / 64.167°N 51.733°W |
||
| Official languages | Greenlandic |
||
| Recognized languages | Danish, English, and other languages if necessary | ||
| Ethnic groups
(2020)
|
|
||
| Religion | Christianity (Church of Greenland) | ||
| Demonym(s) |
|
||
| Government | Devolved government within a parliamentary constitutional monarchy | ||
|
• Monarch
|
Frederik X | ||
| Mette Frederiksen | |||
|
• High Commissioner
|
Julie Præst Wilche | ||
| Jens-Frederik Nielsen | |||
|
• Speaker of the Inatsisartut
|
Mimi Karlsen | ||
| Legislature | Folketinget (Realm legislature) Inatsisartut (Local legislature) |
||
| National representation | |||
|
• Folketing
(2 members) |
|
||
| Area | |||
|
• Total
|
2,166,086 km2 (836,330 sq mi) | ||
|
• Water (%)
|
83.1 | ||
| Highest elevation | 3,700 m (12,100 ft) | ||
| Population | |||
|
• 2022 estimate
|
 56,583 (210th) |
||
|
• Density
|
0.028/km2 (0.1/sq mi) | ||
| GDP (PPP) | 2021 estimate | ||
|
• Total
|
 $3.85 billion |
||
|
• Per capita
|
$68,100 |
||
| GDP (nominal) | 2021 estimate | ||
|
• Total
|
$3.24 billion |
||
|
• Per capita
|
$57,116 |
||
| Gini (2015) |  33.9medium |
||
| HDI (2010) | 0.786 high · 61st |
||
| Currency | Danish krone (DKK) | ||
| Time zone | UTC±00:00 to UTC-04:00 | ||
| Date format | dd-mm-yyyy | ||
| Driving side | right | ||
| Calling code | +299 | ||
| Postal codes |
39xx
|
||
| ISO 3166 code | GL | ||
| Internet TLD | .gl | ||
Greenland (Greenlandic: Kalaallit Nunaat Danish: Grønland) is a North American island autonomous territory of the Kingdom of Denmark. It is the larger of two autonomous territories within the Kingdom, the other being the Faroe Islands; the citizens of both territories are full citizens of Denmark. As Greenland is one of the Overseas Countries and Territories of the European Union, citizens of Greenland are European Union citizens. The capital and largest city of Greenland is Nuuk. Greenland lies between the Arctic and Atlantic oceans, east of the Canadian Arctic Archipelago. It is the world's largest island, and is the location of the northernmost point of land in the world – Kaffeklubben Island off the northern coast is the world's northernmost undisputed point of land, and Cape Morris Jesup on the mainland was thought to be so until the 1960s.
Though a part of the continent of North America, Greenland has been politically and culturally associated with Europe (specifically Norway and Denmark, the colonial powers) for more than a millennium, beginning in 986. Greenland has been inhabited at intervals over at least the last 4,500 years by circumpolar peoples whose forebears migrated there from what is now Canada. Norsemen settled the uninhabited southern part of Greenland beginning in the 10th century (having previously settled Iceland), and the 13th century saw the arrival of Inuit.
In the early 17th century, Dano-Norwegian explorers reached Greenland again. When Denmark and Norway separated in 1814, Greenland was transferred to the Danish crown, and was fully integrated in the Danish state in 1953 under the Constitution of Denmark, which made the people in Greenland citizens of Denmark. In the 1979 Greenlandic home rule referendum, Denmark granted home rule to Greenland; in the 2008 Greenlandic self-government referendum, Greenlanders voted for the Self-Government Act, which transferred more power from the Danish government to the local Naalakkersuisut (Greenlandic government). Under this structure, Greenland gradually assumed responsibility for a number of governmental services and areas of competence. The Danish government retains control of citizenship, monetary policy, and foreign affairs, including defence. Most residents of Greenland are Inuit. With the melting of the ice due to global warming, its abundance of mineral wealth and its strategic position between Europe, North America and the Arctic zone, Greenland is of interest to the great powers including China, Russia and the United States. The Pituffik Space Base is therefore a military zone under the control of the United States.
The population is concentrated mainly on the southwest coast, and the rest of the island is sparsely populated. Three-quarters of Greenland is covered by the only permanent ice sheet outside Antarctica. With a population of 56,583 (2022), Greenland is the least densely populated region in the world. Sixty-seven percent of its electricity production comes from renewable energy, mostly from hydropower.
Contents
Etymology
The early Norse settlers named the island Greenland. In the Icelandic sagas, the Norwegian Erik the Red was exiled from Iceland with his father, Thorvald, who had committed manslaughter. With his extended family and his thralls (slaves or serfs), he set out in ships to explore an icy land known to lie to the northwest. After finding a habitable area and settling there, he named it Grœnland (translated as "Greenland"), supposedly in the hope that the pleasant name would attract settlers. The Saga of Erik the Red states: "In the summer, Erik left to settle in the country he had found, which he called Greenland, as he said people would be attracted there if it had a favorable name."
The name of the territory in the Greenlandic language is Kalaallit Nunaat 'land of the Kalaallit'. The Kalaallit are the Greenlandic Inuit who inhabit the territory's western region.
History
Early Paleo-Inuit cultures
In prehistoric times, Greenland was home to several successive Paleo-Inuit cultures known primarily through archaeological finds. The earliest entry of the Paleo-Inuit into Greenland is thought to have occurred about 2500 BC. From about 2500 BC to 800 BC, southern and western Greenland was inhabited by the Saqqaq culture. Most finds of remains from that period have been around Disko Bay, including the site of Saqqaq, for which the culture is named.
From 2400 BC to 1300 BC, the Independence I culture existed in northern Greenland. It was a part of the Arctic small-tool tradition. Towns, including Deltaterrasserne, appeared. About 800 BC, the Saqqaq culture disappeared and the Early Dorset culture emerged in western Greenland and the Independence II culture in northern Greenland. The Dorset culture was the first culture to extend throughout the Greenlandic coastal areas, in the west and the east. It lasted until the total onset of the Thule culture, in AD 1500. The people of the Dorset culture lived mainly by hunting whales and reindeer.
Norse settlement
From 986, the west coast was settled by Icelanders and Norwegians, through a contingent of 14 boats led by Erik the Red. They formed three settlements—the Eastern Settlement, the Western Settlement, and the Middle Settlement—on fjords near the southwestern tip of the island. They shared the island with the late Dorset culture inhabitants, who occupied the northern and western parts, and later with those of the Thule culture, who entered from the north. Norse Greenlanders submitted to Norwegian rule in 1261 under the Kingdom of Norway. The Kingdom of Norway entered a personal union with Denmark in 1380, and from 1397 was a part of the Kalmar Union.
The Norse settlements, such as Brattahlíð, thrived for centuries, before disappearing in the 15th century, perhaps at the onset of the Little Ice Age. Except some runic inscriptions, the only contemporary records or historiography that survives from the Norse settlements is of their contact with Iceland or Norway. Medieval Norwegian sagas and historical works mention Greenland's economy, the bishops of Gardar, and the collection of tithes. A chapter in the Konungs skuggsjá (The King's Mirror) describes Norse Greenland's exports, imports, and grain cultivation.
Icelandic saga accounts of life in Greenland were composed in the 13th century and later, and are not primary sources for the history of early Norse Greenland. Those accounts are closer to primary for more contemporaneous accounts of late Norse Greenland. Modern understanding therefore mostly depends on the physical data from archeological sites. Interpretation of ice-core and clam-shell data suggests that between AD 800 and 1300 the regions around the fjords of southern Greenland had a relatively mild climate, several degrees Celsius warmer than usual in the North Atlantic with trees and herbaceous plants growing and livestock being farmed. Barley was grown as a crop up to the 70th parallel. The ice cores show that Greenland has had dramatic temperature shifts many times in the past 100,000 years. Similarly the Icelandic Book of Settlements records famines during the winters.
These Norse settlements vanished during the 14th and early 15th centuries. The demise of the Western Settlement coincides with a decrease in summer and winter temperatures. A study of North Atlantic seasonal temperature variability during the Little Ice Age showed a significant decrease in maximum summer temperatures beginning about the turn of the 14th century—as much as 6 to 8 °C (11 to 14 °F) lower than modern summer temperatures. The study also found that the lowest winter temperatures of the last 2,000 years occurred in the late 14th century and early 15th century. The Eastern Settlement was probably abandoned in the early to mid-15th century, during this cold period.
.png)
Theories drawn from archeological excavations at Herjolfsnes in the 1920s suggest that the condition of human bones from this period indicates that the Norse population was malnourished, possibly because of soil erosion resulting from the Norsemen's destruction of natural vegetation in the course of farming, turf-cutting, and wood-cutting. Malnutrition may also have resulted from widespread deaths from pandemic plague; the decline in temperatures during the Little Ice Age; and armed conflicts with the Skrælings (Norse word for Inuit, meaning "wretches"). Recent archeological studies somewhat challenge the general assumption that the Norse colonization had a dramatic negative environmental effect on the vegetation. Data support traces of a possible Norse soil amendment strategy. More recent evidence suggests that the Norse, who never numbered more than about 2,500, gradually abandoned the Greenland settlements over the 15th century as walrus ivory, the most valuable export from Greenland, decreased in price because of competition with other sources of higher-quality ivory, and that there was actually little evidence of starvation or difficulties.
Other explanations of the disappearance of the Norse settlements have been proposed:
- Lack of support from the homeland.
- Ship-borne marauders (such as Basque, English, or German pirates) rather than Skrælings, could have plundered and displaced the Greenlanders.
- They were "the victims of hidebound thinking and of a hierarchical society dominated by the Church and the biggest land owners. In their reluctance to see themselves as anything but Europeans, the Greenlanders failed to adopt the kind of apparel that the Inuit employed as protection against the cold and damp or to borrow any of the Inuit hunting gear."
- That portion of the Greenlander population willing to adopt Inuit ways and means intermarried with and assimilated into the Inuit community. Much of the Greenland population is mixed Inuit and European ancestry. It was impossible in 1938 when Stefansson wrote his book to distinguish between intermarriage before the European loss of contact and after the contact was restored.
- "Norse society's structure created a conflict between the short-term interests of those in power, and the long-term interests of the society as a whole."
Thule culture (1300–present)
The Thule people are the ancestors of the current Greenlandic population. No genes from the Paleo-Inuit have been found in the present population of Greenland. The Thule culture migrated eastward from what is now known as Alaska around 1000 AD, reaching Greenland around 1300. The Thule culture was the first to introduce to Greenland such technological innovations as dog sleds and toggling harpoons.
There is an account of contact and conflict with the Norse population, as told by the Inuit. It is republished in The Norse Atlantic Sagas, by Gwyn Jones. Jones reports that there is also an account of perhaps the same incident, of more doubtful provenance, told by the Norse side.
1500–1814
In 1500, King Manuel I of Portugal sent Gaspar Corte-Real to Greenland in search of a Northwest Passage to Asia which, according to the Treaty of Tordesillas, was part of Portugal's sphere of influence. In 1501, Corte-Real returned with his brother, Miguel Corte-Real. Finding the sea frozen, they headed south and arrived in Labrador and Newfoundland. Upon the brothers' return to Portugal, the cartographic information supplied by Corte-Real was incorporated into a new map of the world which was presented to Ercole I d'Este, Duke of Ferrara, by Alberto Cantino in 1502. The Cantino planisphere, made in Lisbon, accurately depicts the southern coastline of Greenland.
In 1605–1607, King Christian IV of Denmark and Norway sent a series of expeditions to Greenland and Arctic waterways to locate the lost eastern Norse settlement and assert Danish-Norwegian sovereignty over Greenland. The expeditions were mostly unsuccessful, partly due to leaders who lacked experience with the difficult Arctic ice and weather conditions, and partly because the expedition leaders were given instructions to search for the Eastern Settlement on the east coast of Greenland just north of Cape Farewell, which is almost inaccessible due to southward drifting ice. The pilot on all three trips was English explorer James Hall.
.jpg)
After the Norse settlements died off, Greenland came under the de facto control of various Inuit groups, but the Dano-Norwegian government never forgot or relinquished the claims to Greenland that it had inherited from the Norse. When it re-established contact with Greenland in the early 17th century, Denmark-Norway asserted its sovereignty over the island. In 1721 a joint mercantile and clerical expedition led by Dano-Norwegian missionary Hans Egede was sent to Greenland, not knowing whether a Norse civilization remained there. This expedition is part of the Dano-Norwegian colonization of the Americas. After 15 years in Greenland, Hans Egede left his son Paul Egede in charge of the mission there and returned to Denmark, where he established a Greenland Seminary. This new colony was centred at Godthåb ("Good Hope") on the southwest coast. Gradually, Greenland was opened up to Danish merchants, but closed to those from other countries.
Treaty of Kiel to World War II (1814–1945)
When the union between the crowns of Denmark and Norway was dissolved in 1814, the Treaty of Kiel severed Norway's former colonies and left them under the control of the Danish monarch. Norway occupied then-uninhabited eastern Greenland as Erik the Red's Land in July 1931, claiming that it constituted terra nullius. Norway and Denmark agreed to submit the matter in 1933 to the Permanent Court of International Justice, which decided against Norway.
Greenland's connection to Denmark was severed on 9 April 1940, early in World War II, after Denmark was occupied by Nazi Germany. On 8 April 1941, the United States occupied Greenland to defend it against a possible invasion by Germany. The United States' occupation of Greenland continued until 1945. Greenland was able to buy goods from the United States and Canada by selling cryolite from the mine at Ivittuut. In World War II, the United States military used Bluie as a code name for Greenland, where they kept several bases named "Bluie (East or West) (sequential numeral)". The major air bases were Bluie West-1 at Narsarsuaq and Bluie West-8 at Søndre Strømfjord (Kangerlussuaq), both of which are still used as Greenland's major international airports.
During this war, the system of government changed: Governor Eske Brun ruled the island under a law of 1925 that allowed governors to take control under extreme circumstances; Governor Aksel Svane was transferred to the United States to lead the commission to supply Greenland. The Danish Sirius Patrol guarded the northeastern shores of Greenland in 1942 using dog sleds. They detected several German weather stations and alerted American troops, who destroyed the facilities. After the collapse of the Third Reich, Albert Speer briefly considered escaping in a small aeroplane to hide out in Greenland, but changed his mind and decided to surrender to the United States Armed Forces.
Greenland had been a protected and very isolated society until 1940. The Danish government had maintained a strict monopoly of Greenlandic trade, allowing no more than small scale barter trading with British whalers. In wartime Greenland developed a sense of self-reliance through self-government and independent communication with the outside world. Despite this change, in 1946 a commission including the highest Greenlandic council, the Landsrådene, recommended patience and no radical reform of the system. Two years later, the first step towards a change of government was initiated when a grand commission was established. A final report (G-50) was presented in 1950, which recommended the introduction of a modern welfare state with Denmark's development as sponsor and model. In 1953, Greenland was made an equal part of the Danish Kingdom. Home rule was granted in 1979.
Home rule and self-rule
In 1867, United States Secretary of State William H. Seward worked with former senator Robert J. Walker to explore the possibility of buying Greenland and, perhaps, Iceland. Opposition in Congress ended this project. Following World War II, the United States developed a geopolitical interest in Greenland and in 1946 offered to buy the island from Denmark for $100,000,000; the Danish rejected the offer.
In 1950, Denmark agreed to allow the US to regain the use of Thule Air Base; it was greatly expanded between 1951 and 1953 as part of a unified NATO Cold War defence strategy. The local population of three nearby villages was moved more than 100 km (62 miles) away in the winter. The United States tried to construct a subterranean network of secret nuclear missile launch sites in the Greenlandic ice cap, named Project Iceworm. According to documents declassified in 1996, this project was managed from Camp Century from 1960 to 1966 before abandonment as unworkable. The missiles were never fielded, and necessary consent from the Danish Government to do so was never sought. The Danish government did not become aware of the programme's mission until 1997, when they discovered it while looking, in the declassified documents, for records related to the crash of a nuclear equipped B-52 bomber at Thule in 1968.
With the 1953 Danish constitution, Greenland's colonial status ended as the island was incorporated into the Danish realm as an amt (county). Danish citizenship was extended to Greenlanders. Danish policies toward Greenland consisted of a strategy of cultural assimilation — or de-Greenlandification. During this period, the Danish government promoted the exclusive use of the Danish language in official matters, and required Greenlanders to go to Denmark for their post-secondary education. Many Greenlandic children grew up in boarding schools in southern Denmark, and a number lost their cultural ties to Greenland. While the policies "succeeded" in the sense of shifting Greenlanders from being primarily subsistence hunters into being urbanized wage earners, the Greenlandic elite began to reassert a Greenlandic cultural identity. A movement developed in favour of independence, reaching its peak in the 1970s. As a consequence of political complications in relation to Denmark's entry into the European Common Market in 1972, Denmark began to seek a different status for Greenland, resulting in the Home Rule Act of 1979.
.jpg)
This gave Greenland limited autonomy with its own legislature taking control of some internal policies, while the Parliament of Denmark maintained full control of external policies, security, and natural resources. The law came into effect on 1 May 1979. The King of Denmark, Frederik X, remains Greenland's head of state. In 1985, Greenland left the European Economic Community (EEC) upon achieving self-rule, as it did not agree with the EEC's commercial fishing regulations and an EEC ban on seal skin products. Greenland voters approved a referendum on greater autonomy on 25 November 2008. According to one study, the 2008 vote created what "can be seen as a system between home rule and full independence".
On 21 June 2009, Greenland gained self-rule with provisions for assuming responsibility for self-government of judicial affairs, policing, and natural resources. Also, Greenlanders were recognized as a separate people under international law. Denmark maintains control of foreign affairs and defence matters. Denmark upholds the annual block grant of 3.2 billion Danish kroner, but as Greenland begins to collect revenues of its natural resources, the grant will gradually be diminished. This is generally considered to be a step toward eventual full independence from Denmark. Greenlandic was declared the sole official language of Greenland at the historic ceremony.
A century and a half after its first proposition, in August 2019, and again in 2024, prior to taking office after his re-election; United States President Donald Trump stated that the U.S. again wanted to buy the country. In December 2024, Prime Minister Múte Egede wrote: "Greenland is ours. We are not for sale and will never be for sale. We must not lose our long struggle for freedom".
Tourism
Tourism increased significantly between 2015 and 2019, with the number of visitors increasing from 77,000 per year to 105,000. One source estimated that in 2019 the revenue from this aspect of the economy was about 450 million kroner (US$67 million). Like many aspects of the economy, this slowed dramatically in 2020 and into 2021, due to restrictions required as a result of the COVID-19 pandemic; one source describes it as being the "biggest economic victim of the coronavirus" (the overall economy did not suffer too severely as of mid-2020, thanks to the fisheries "and a hefty subsidy from Copenhagen"). Greenland's goal for returning tourism is to develop it "right" and to "build a more sustainable tourism for the long run".
Geography and climate
Greenland is the world's largest non-continental island and the third largest area in North America after Canada and the United States. It is between latitudes 59° and 83°N, and longitudes 11° and 74°W. Greenland is bordered by the Arctic Ocean to the north, the Greenland Sea to the east, the North Atlantic Ocean to the southeast, the Davis Strait to the southwest, Baffin Bay to the west, the Nares Strait and Lincoln Sea to the northwest. The nearest countries to Greenland are Canada, with which it shares a maritime border, to the west and southwest across Nares Strait and Baffin Bay, as well as a shared land border on Hans Island; and Iceland, southeast of Greenland in the Atlantic Ocean. Greenland also contains the world's largest national park, and it is the largest constituent country by area in the world, and is the fourth largest country subdivision in the world, after Sakha Republic in Russia, Australia's state of Western Australia, and Russia's Krasnoyarsk Krai, and the largest in North America.
The lowest temperature ever recorded in the Northern Hemisphere was recorded in Greenland, near the topographic summit of the Greenland Ice Sheet, on 22 December 1991, when the temperature reached −69.6 °C (−93.3 °F). In Nuuk, the average daily temperature varies over the seasons from −5.1 to 9.9 °C (22.8 to 49.8 °F). The total area of Greenland is 2,166,086 km2 (836,330 sq mi) (including other offshore minor islands), of which the Greenland ice sheet covers 1,755,637 km2 (677,855 sq mi) (81%) and has a volume of approximately 2,850,000 km3 (680,000 cu mi). The highest point on Greenland is Gunnbjørn Fjeld at 3,700 m (12,100 ft) of the Watkins Range (East Greenland mountain range). The majority of Greenland, however, is less than 1,500 m (4,900 ft) in elevation.
Below the ice there is a series of canyons, the biggest called Greenland’s Grand Canyon which was formed by flowing rivers of water from the repeated cycle of ice melting and new ice forming. Near the coast elevations rise suddenly and steeply.
The ice flows generally to the coast from the centre of the island. A survey led by French scientist Paul-Emile Victor in 1951 concluded that, under the ice sheet, Greenland is composed of three large islands. This is disputed, but if it is so, they would be separated by narrow straits, reaching the sea at Ilulissat Icefjord, at Greenland's Grand Canyon and south of Nordostrundingen.
All towns and settlements of Greenland are situated along the ice-free coast, with the population being concentrated along the west coast. The northeastern part of Greenland is not part of any municipality, but it is the site of the world's largest national park, Northeast Greenland National Park.
At least four scientific expedition stations and camps had been established on the ice sheet in the ice-covered central part of Greenland (indicated as pale blue in the adjacent map): Eismitte, North Ice, North GRIP Camp and The Raven Skiway. There is a year-round station Summit Camp on the ice sheet, established in 1989. The radio station Jørgen Brønlund Fjord was, until 1950, the northernmost permanent outpost in the world.
The extreme north of Greenland, Peary Land, is not covered by an ice sheet, because the air there is too dry to produce snow, which is essential in the production and maintenance of an ice sheet.
In 2007, the existence of a new island was announced. Named "Uunartoq Qeqertaq" (English: Warming Island), this island has always been present off the coast of Greenland but was covered by a glacier. This glacier was discovered in 2002 to be shrinking rapidly, and by 2007 had completely melted away, leaving the exposed island. The island was named Place of the Year by the Oxford Atlas of the World in 2007. Ben Keene, the atlas's editor, commented:
In the last two or three decades, global warming has reduced the size of glaciers throughout the Arctic and earlier this year, news sources confirmed what climate scientists already knew: water, not rock, lay beneath this ice bridge on the east coast of Greenland. More islets are likely to appear as the sheet of frozen water covering the world's largest island continues to melt.
Some controversy surrounds the history of the island, specifically over whether the island might have been revealed during a brief warm period in Greenland during the mid-20th century.
Northernmost land
The northernmost point of land on Earth was long thought to be Cape Morris Jesup at the northern tip of mainland Greenland. However, in 1969 a Canadian team surveyed Kaffeklubben Island (latitude 83° 39′ 45″ N), which was first recorded in 1900 and first visited in 1921, and determined that its northernmost point is 750 m north of Cape Morris Jesup. It is thus the northernmost undisputed permanent land.
Other points have been claimed to be the northernmost point, with dispute over the title arising from ice sheets, water movement and inundation, and storm activity that may build, shift, or destroy banks of gravelly moraine material. In 1978 Uffe Petersen, a member of the Danish Geodetic Institute, discovered Oodaaq Island at 83° 40' 32.5" N. Its last confirmed sighting was in 1979. In 2003, a small protrusion of rocks and boulders, 35 m × 15 m (115 ft × 49 ft) in length and width, was discovered by Arctic explorer Dennis Schmitt and his team at latitude 83° 42' N and unofficially named 83-42. Whether this land is permanent is uncertain; a 2022 bathymetric survey determined that it was likely not connected to the seafloor, but rather rocky material on top of sea ice, and thus not land.
Climate change
Greenland ice sheet always loses some mass from ice calving at its coasts, but it used to balance this on average by the accumulation of snowfall. However, Greenland has been warming since around 1900, and starting in the 1980s, the losses became larger than the gains. After 1996, Greenland has not had a single year when it did not lose mass on average. In the 2010s, the Greenland ice sheet melted at its fastest rate during at least the past 12,000 years, and is on track to exceed that later in the century. In 2012, 2019 and 2021, so-called "massive melting events" occurred, when practically the entire surface of the ice sheet was melting and no accumulation took place. During the 2021 event, rain fell at Greenland's highest point for the first time in recorded history, an event so unexpected that the research station at the summit had no rain gauges for the occasion.
As with the ice loss elsewhere, the melting of Greenland contributes to sea level rise. Between 2012 and 2017, this melting added an average of 0.68 mm per year, equal to 37% of sea level rise from land ice sources (excluding thermal expansion of water from the continual increase in the ocean heat content). By the end of the century, the melting of Greenland alone will add between ~6 cm (2.4 in) if the temperature change is kept below 2 °C (3.6 °F), to around 13 cm (5.1 in) if the most intense climate change scenario with ever-increasing greenhouse gas emissions is followed. Under this scenario, the worst case for Greenland melting could reach 33 cm (13 in) of sea level rise equivalent. The large quantities of fresh meltwater also affect the Atlantic meridional overturning circulation (AMOC) by diluting key currents, slowing it down. Due to this meltwater input, the circulation may even collapse outright with widespread detrimental effects, although research suggests this is likely only if the highest possible warming is sustained for multiple centuries.
Greenland's ice sheet has a volume of ~2,900,000 cubic kilometres (696,000 cu mi). This means that if it were all to melt, global sea level would increase by ~7.4 m (24 ft) from that event alone. However, it also means that it will take at least 1,000 years for the ice sheet to disappear even with very high rates of global warming, and in around 10,000 years under lower rates of warming which still cross the threshold for the ice sheet's disappearance. This threshold likely lies for between 1.7 °C (3.1 °F) and 2.3 °C (4.1 °F). Reducing the warming back to 1.5 °C (2.7 °F) or lower above preindustrial levels (such as through large-scale carbon dioxide removal) would arrest the losses, but still cause greater ultimate sea level rise than if the threshold had never been exceeded. Further, 1.5 °C (2.7 °F) itself appears to commit the Greenland ice sheet to 1.4 m (4.6 ft) of sea level rise.
Geology
The island was part of the very ancient Precambrian continent of Laurentia, the eastern core of which forms the Greenland Shield, while the less exposed coastal strips became a plateau. On these ice-free coastal strips are sediments formed in the Precambrian, overprinted by metamorphism and now formed by glaciers, which continue into the Cenozoic and Mesozoic in parts of the island.
In the east and west of Greenland there are remnants of flood basalts and igneous intrusions, such as the Skaergaard intrusion. Notable rock provinces (metamorphic igneous rocks, ultramafics, and anorthosites) are found on the southwest coast at Qeqertarsuatsiaat. East of Nuuk, the banded iron ore region of Isukasia, over three billion years old, contains the world's oldest rocks, such as greenlandite (a rock composed predominantly of hornblende and hyperthene), formed 3.8 billion years ago, and nuummite. In southern Greenland, the Illimaussaq alkaline complex consists of pegmatites such as nepheline, syenites (especially kakortokite or naujaite) and sodalite (sodalite-foya). In Ivittuut, where cryolite was formerly mined, there are fluoride-bearing pegmatites. To the north of Igaliku, there are the Gardar alkaline pegmatitic intrusions of augite syenite, gabbro, etc.
To the west and southwest are Palaeozoic carbonatite complexes at Kangerlussuaq (Gardiner complex) and Safartoq, and basic and ultrabasic igneous rocks at Uiffaq on Disko Island, where there are masses of heavy native iron up to 25 t (28 short tons) in the basalts.
The paleontology of East Greenland is specially rich, with some of the early tetrapods such as the Acanthostega and Ichthyostega from the Devonian and unique Triassic animals such as the phytosaur Mystriosuchus alleroq and the dinosaurs Issi saaneq and tracks.
Biodiversity
Greenland is home to two ecoregions: Kalaallit Nunaat high arctic tundra and Kalaallit Nunaat low arctic tundra. There are approximately 700 known species of insects in Greenland, which is low compared with other countries (over one million species have been described worldwide). The sea is rich in fish and invertebrates, especially in the milder West Greenland Current; a large part of the Greenland fauna is associated with marine-based food chains, including large colonies of seabirds. The few native land mammals in Greenland include the polar bear, reindeer (introduced by Europeans), arctic fox, arctic hare, musk ox, collared lemming, ermine, and arctic wolf. The last four are found naturally only in East Greenland, having immigrated from Ellesmere Island. There are dozens of species of seals and whales along the coast. Land fauna consists predominantly of animals which have spread from North America or, in the case of many birds and insects, from Europe. There are no native or free-living reptiles or amphibians on the island.
Phytogeographically, Greenland belongs to the Arctic province of the Circumboreal Region within the Boreal Kingdom. The island is sparsely populated in vegetation; plant life consists mainly of grassland and small shrubs, which are regularly grazed by livestock. The most common tree native to Greenland is the European white birch (Betula pubescens) along with gray-leaf willow (Salix glauca), rowan (Sorbus aucuparia), common juniper (Juniperus communis) and other smaller trees, mainly willows.
Greenland's flora consists of about 500 species of "higher" plants, such as flowering plants, ferns, horsetails and lycopodiophyta. Of the other groups, the lichens are the most diverse, with about 950 species; there are 600–700 species of fungi; mosses and bryophytes are also found. Most of Greenland's higher plants have circumpolar or circumboreal distributions; only a dozen species of saxifrage and hawkweed are endemic. A few plant species were introduced by the Norsemen, such as cow vetch.
.jpg)
The terrestrial vertebrates of Greenland include the Greenland dog, which was introduced by the Inuit, as well as European-introduced species such as Greenlandic sheep, goats, cattle, reindeer, horse, chicken and sheepdog, all descendants of animals imported by Europeans. Marine mammals include the hooded seal (Cystophora cristata) as well as the grey seal (Halichoerus grypus). Whales frequently pass very close to Greenland's shores in the late summer and early autumn. Whale species include the beluga whale, blue whale, Greenland whale, fin whale, humpback whale, minke whale, narwhal, pilot whale, sperm whale.
As of 2009, 269 species of fish from over 80 different families are known from the waters surrounding Greenland. Almost all are marine species with only a few in freshwater, such as Atlantic salmon and charr. The fishing industry is the primary industry of Greenland's economy, accounting for the majority of territory's total exports.
Birds, particularly seabirds, are an important part of Greenland's animal life; they consist of both Palearctic and Nearctic species, breeding populations of auks, puffins, skuas, and kittiwakes are found on steep mountainsides. Greenland's ducks and geese include common eider, long-tailed duck, king eider, white-fronted goose, pink-footed goose and barnacle goose. Breeding migratory birds include the snow bunting, lapland bunting, ringed plover, red-throated loon and red-necked phalarope. Non-migratory land birds include the arctic redpoll, ptarmigan, short-eared owl, snowy owl, gyrfalcon and white-tailed eagle.
Politics
The Greenlandic government holds executive power in local government affairs. The head of the government is called Naalakkersuisut Siulittaasuat ("Premier") and serves as head of Greenlandic Government. Any other member of the cabinet is called a Naalakkersuisoq ("Minister"). The Greenlandic parliament is called Inatsisartut ("Legislators"). The parliament currently has 31 members.
In contemporary times, elections are held at municipal, national (Inatsisartut), and kingdom (Folketing) levels.
Greenland is a self-governing entity within the constitutional monarchy of the Kingdom of Denmark, in which King Frederik X is the head of state. The monarch officially retains executive power and presides over the Council of State (privy council). However, following the introduction of a parliamentary system of government, the duties of the monarch have since become strictly representative and ceremonial, such as the formal appointment and dismissal of the prime minister and other ministers in the executive government. The monarch is not answerable for his or her actions, and the monarch's person is sacrosanct.
Political system
The party system was dominated by the social-democratic Forward Party, and the democratic socialist Inuit Community Party, both of which broadly argue for greater independence from Denmark. While the 2009 election saw the unionist Democrat Party (two MPs) decline greatly, the 2013 election consolidated the power of the two main parties at the expense of the smaller groups, and saw the eco-socialist Inuit Party elected to the Parliament for the first time. The dominance of the Forward and Inuit Community parties began to wane after the snap 2014 and 2018 elections.
The non-binding 2008 referendum on self-governance favouring increased self-governance and autonomy was passed winning 76.22% of the vote.
In 1985, Greenland left the European Economic Community (EEC), unlike Denmark, which remains a member. The EEC later became the European Union (EU, renamed and expanded in scope in 1992). Greenland retains some ties through its associated relationship with the EU. However, EU law largely does not apply to Greenland except in the area of trade. Greenland is designated as a member of the Overseas Countries and Territories (OCT) and is thus officially not a part of the European Union, though Greenland can and does receive support from the European Development Fund, Multiannual Financial Framework, European Investment Bank and EU Programmes.
Government
Greenland's head of state is King Frederik X. The King's government in Denmark appoints a high commissioner (Rigsombudsmand) to represent it on the island.
The Greenland constituency elect two MP representatives to the Kingdom Parliament (Folketinget) in Denmark, out of a total of 179.
Greenland has national Parliament that consists of 31 representatives. The government is the Naalakkersuisut whose members are appointed by the premier. The head of government is the premier, usually the leader of the majority party in Parliament.
Military
Several American and Danish military bases are located in Greenland, including Pituffik Space Base (previously Thule Air Base), which is home to the United States Space Force's global network of sensors providing missile warning, space surveillance and space control to North American Aerospace Defense Command (NORAD). Elements of the sensor systems are commanded and controlled variously by Space Deltas 2, 4, and 6.
In 1995, a political scandal in Denmark occurred after a report revealed the government had given tacit permission for nuclear weapons to be located in Greenland, in contravention of Denmark's 1957 nuclear-free zone policy. The United States built a secret nuclear powered base, called Camp Century, in the Greenland ice sheet. On 21 January 1968, a B-52G, with four nuclear bombs aboard as part of Operation Chrome Dome, crashed on the ice of the North Star Bay while attempting an emergency landing at Thule Air Base. The resulting fire caused extensive radioactive contamination. One of the H-bombs remains lost.
Administrative divisions
Formerly consisting of three counties comprising a total of 18 municipalities, Greenland abolished these in 2009 and has since been divided into large territories known as "municipalities" (Greenlandic: kommuneqarfiit, Danish: kommuner): Sermersooq ("Much Ice") around the capital Nuuk and also including all East Coast communities; Kujalleq ("South") around Cape Farewell; Qeqqata ("Centre") north of the capital along the Davis Strait; Qeqertalik ("The one with islands") surrounding Disko Bay; and Avannaata ("Northern") in the northwest; the latter two having come into being as a result of the Qaasuitsup municipality, one of the original four, being partitioned in 2018. The northeast of the island composes the unincorporated Northeast Greenland National Park. Pituffik Space Base is also unincorporated, an enclave within Avannaata municipality. As a territorial concession granted to the United States in perpetuity, it is administered by the United States Space Force. During its construction, there were as many as 12,000 American residents but in recent years the number has been below 1,000.
Economy
The Greenlandic economy is highly dependent on fishing. Fishing accounts for more than 90% of Greenland's exports. The shrimp and fish industry is by far the largest income earner.
Greenland is abundant in minerals. Mining of ruby deposits began in 2007. Other mineral prospects are improving as prices are increasing. These include iron, uranium, aluminium, nickel, platinum, tungsten, titanium, and copper. The state company Nunamineral has been launched on the Copenhagen Stock Exchange to raise more capital to increase the production of gold, started in 2007. Another state company, Nunaoil, was created to help develop the hydrocarbon industry in Greenland. However, in July 2021, Greenland banned all new oil and gas exploration in its territory, with government officials stating that the environmental "price of oil extraction is too high".
Electricity has traditionally been generated by oil or diesel power plants, even if there is a large surplus of potential hydropower. There is a programme to build hydropower plants. The first, and still the largest, is Buksefjord hydroelectric power plant.
There are also plans to build a large aluminium smelter, using hydropower to create an exportable product. It is expected that much of the labour needed will be imported.
The European Union has urged Greenland to restrict development by the People's Republic of China of rare-earth mineral projects, as China accounts for 95% of the world's current supply. However, in early 2013 the government of Greenland said that it had no plans to impose such restrictions.
The public sector, including publicly owned enterprises and the municipalities, plays a dominant role in Greenland's economy. About half the government revenues come from grants from the Danish government, an important supplement to the gross domestic product (GDP). Gross domestic product per capita is equivalent to that of the average economies of Europe.
Greenland suffered an economic contraction in the early 1990s. Since 1993, the economy has improved. The Greenland Home Rule Government (GHRG) has pursued a tight fiscal policy since the late 1980s, which has helped create surpluses in the public budget and low inflation. Since 1990, Greenland has registered a foreign-trade deficit following the closure of the last remaining lead and zinc mine that year. In 2017, new sources of ruby in Greenland have been discovered, promising to enhance the gemstone industry in Greenland and add a new export.
Transport
Air transport connects Greenland internally and with other nations. There is also scheduled boat traffic, but the long distances lead to long travel times and low frequency. There are virtually no roads between cities because the coast has many fjords that would require ferry service to connect a road network. The only exception is a gravel road of 4.8 km (3 mi) length between Kangilinnguit and the now abandoned former cryolite mining town of Ivittuut. In addition, the lack of agriculture, forestry and similar countryside activities has meant that very few country roads have been built. Greenland has no passenger railways.
A 1-lane dirt road designed primarily for all-terrain vehicles (secondarily for bicycles and hiking), is under construction between Kangerlussuaq and the town of Sisimiut. As of June 2023, the road was scheduled for completion in 2024. A news report in Sermitsiaq declared the road itself to be completed already in September 2021, but maintenance work and mud problems have caused delays. There are plans to extend the road to a 2-lane gravel road, but a date for its construction start has not been announced.
Nuuk Airport is the hub and international gateway for international and domestic airline passenger transport. Air Greenland is the flag carrier of Greenland. Additionally, Icelandair provides year-round services to Greenlandic airports. Seasonal and charter flights are also offered by other airlines. Kangerlussuaq Airport (SFJ) was until 2024 the main international gateway to Greenland, but is far from the vicinity of the larger metropolitan capital areas. Ilulissat Airport (JAV) is a domestic airport that also serves international flights to Iceland and is under reconstruction and expansion to enable larger aircraft to serve the airport by 2026.
There are a total of 13 registered civil airports and 47 helipads in Greenland; most of them are unpaved and located in rural areas. The fourth-longest runway is at Narsarsuaq Airport, a domestic airport with limited international service in south Greenland. All civil aviation matters are handled by the Danish Transport Authority. Most airports have short runways and can only be served by special fairly small aircraft on fairly short flights. Intercontinental flights connect mainly to Copenhagen. Travel between international destinations (except Iceland) and most cities, requires a plane change in Nuuk.
Sea passenger transport is served by several coastal ferries. Arctic Umiaq Line makes a single round trip per week, taking 80 hours each direction.
Cargo freight by sea is handled by the shipping company Royal Arctic Line from, to and across Greenland. It provides trade and transport opportunities between Greenland, Europe, and North America.
Population
Demographics
.jpg)
In 2021, Greenland had a population of 56,421. That year, 18,800 people resided in the capital city Nuuk. Nearly all Greenlanders live along the fjords in the south-west of the main island, which has a relatively mild climate, especially considering the high latitude upon which it lies. Whereas the majority of the population lives north of 64°N in colder coastal climates, Greenland's warmest climates such as the vegetated area around Narsarsuaq are sparsely populated.
The majority of the population is Lutheran. The historically important Moravian Brothers (Herrnhuters) were a congregation of faith, in a Danish context based in Christiansfeld in South Jutland, and partially of German origin, but their name does not signify they were ethnic Moravians (Czechs).
In terms of country of birth, the population is estimated to be of 89.7% Greenlandic multiethnic European-Inuit origin, 7.8% Danish, 1.1% other Nordic and 1.4% other. The multi-ethnic population of European-Inuit represent people of Danish, Norwegian and to a lesser degree of Faroese, Icelandic, Dutch (whalers), German and American descent.
A 2015 wide genetic study of Greenlanders found modern-day Inuit in Greenland are direct descendants of the first Inuit pioneers of the Thule culture who arrived in the 13th century, with approximately 25% admixture of the European colonizers from the 16th century. Despite previous speculations, no evidence of Viking settlers predecessors has been found.
|
Largest cities or towns in Greenland
2020 estimate |
||
|---|---|---|
| Rank | Pop. | |
| 1 | Nuuk | 18,326 |
| 2 | Sisimiut | 5,582 |
| 3 | Ilulissat | 4,670 |
| 4 | Aasiaat | 3,069 |
| 5 | Qaqortoq | 3,050 |
| 6 | Maniitsoq | 2,534 |
| 7 | Tasiilaq | 2,063 |
| 8 | Uummannaq | 1,407 |
| 9 | Narsaq | 1,346 |
| 10 | Paamiut | 1,308 |
Languages
Greenlandic (effectively West Greenlandic), spoken by nearly 50,000 people, became the official sole language in 2009. The majority of the population speak both Danish and West Greenlandic Kalaallisut (the most populous Eskaleut language). They have been used in public affairs since the establishment of home rule in 1979. In practice, Danish is still widely used in administration, academics, and skilled trades and other professions. The orthography of Greenlandic, established in 1851, was revised in 1973. The literacy rate is 100%.
About 12% of the population speak Danish as a first or sole language. These primarily are Danish immigrants, many of whom remain the first and only language for those in Nuuk and other larger towns. Debate about the roles of Greenlandic and Danish in the country's future is evolving. While Greenlandic was dominant in all smaller settlements, most of the multi ethnic Inuit ancestors spoke Danish as a second language. In larger towns, especially Nuuk, this Danish group was more important for social matters. English is another important language for Greenland now taught from the first school year.
West Greenland has long been the most populous area of the island and home to its de facto status as the official Greenlandic language. Although around 3,000 people speak East Greenlandic (Tunumiisut) and nearly 1,000 around northern Qaanaaq speak Inuktun. North Greenlandic is closer to the Inuit languages of Canada than it is to other Greenlandic. Each of these varieties is nearly unintelligible to the speakers of the others and some linguists consider Tunumiisut to be a separate language all together. A UNESCO report labelled the other varieties as endangered, and measures are now considered to protect the East Greenlandic dialect.
Education
Education is organized in a similar way to Denmark. There is ten year mandatory primary school. There is also a secondary school, with either work education or preparatory for university education. There is one university, the University of Greenland (Greenlandic: Ilisimatusarfik) in Nuuk. Many Greenlanders attend universities in Denmark or elsewhere.
The public school system in Greenland is, as in Denmark, under the jurisdiction of the municipalities: they are therefore municipal schools. The legislature specifies the standards allowed for the content in schools, but the municipal governments decide how the schools under their responsibility are run. Education is free and compulsory for children aged seven to 16. The financial effort devoted to education is now very important (11.3% of GDP). Section 1 of the Government Ordinance on Public Schools (as amended on 6 June 1997) requires Greenlandic as the language of instruction.
Education is governed by Regulation No. 10 of 25 October 1990 on primary and lower secondary education. This regulation was amended by Regulation No. 8 of 13 May 1993 and Regulation No. 1 of 1 March 1994. Under Regulation No. 10 of 25 October 1990, linguistic integration in primary and lower secondary schools became compulsory for all students. The aim is to place Greenlandic-speaking and Danish-speaking pupils in the same classes, whereas previously they were placed in separate classes according to their mother tongue. At the same time, the government guarantees that Danish speakers can learn Greenlandic. In this way, the Greenlandic government wants to give the same linguistic, cultural and social education to all students, both those of Greenlandic and Danish origin. A study, which was carried out during a three-year trial period, concluded that this policy had achieved positive results. This bilingualism policy has been in force since 1994.
About 100 schools have been established. Greenlandic and Danish are taught there. Normally, Greenlandic is taught from kindergarten to the end of secondary school, but Danish is compulsory from the first cycle of primary school as a second language. As in Denmark with Danish, the school system provides for "Greenlandic 1" and "Greenlandic 2" courses. Language tests allow students to move from one level to the other. Based on the teachers' evaluation of their students, a third level of courses has been added: "Greenlandic 3". Secondary education in Greenland is generally vocational and technical. The system is governed by Regulation No. 16 of 28 October 1993 on Vocational and Technical Education, Scholarships and Career Guidance. Danish remains the main language of instruction. The capital, Nuuk, has a (bilingual) teacher training college and a (bilingual) university. At the end of their studies, all students must pass a test in the Greenlandic language.
Higher education is offered in Greenland: "university education" (regulation no. 3 of 9 May 1989); training of journalists, training of primary and lower secondary school teachers, training of social workers, training of social educators (regulation no. 1 of 16 May 1989); and training of nurses and nursing assistants (regulation no. 9 of 13 May 1990). Greenlandic students can continue their education in Denmark, if they wish and have the financial means to do so. For admission to Danish educational institutions, Greenlandic applicants are placed on an equal footing with Danish applicants. Scholarships are granted to Greenlandic students who are admitted to Danish educational institutions. To be eligible for these scholarships, the applicant must be a Danish citizen and have had permanent residence in Greenland for at least five years. The total period of residence outside Greenland may not exceed three years.
Religion
Religion in Greenland (2010): Protestantism (95.5%) Roman Catholicism (0.2%) Other Christian (0.4%) Inuit spiritual beliefs (0.8%) Agnostic (2.3%) Atheist (0.2%) Other religion (0.6%)
The nomadic Inuit were traditionally shamanistic, with a well-developed religion primarily concerned with appeasing a vengeful and fingerless sea goddess called Sedna who controlled the success of the seal and whale hunts.
The first Norse colonists worshipped the Norse gods, but Erik the Red's son Leif was converted to Christianity by King Olaf Trygvesson on a trip to Norway in 999 and sent missionaries back to Greenland. These swiftly established sixteen parishes, some monasteries, and a bishopric at Garðar.
Rediscovering these colonists and spreading ideas of the Protestant Reformation among them was one of the primary reasons for the Danish recolonization in the 18th century. Under the patronage of the Royal Mission College in Copenhagen, Norwegian and Danish Lutherans and German Moravian missionaries searched for the missing Norse settlements, but no Norse were found, and instead they began preaching to the Inuit. The principal figures in the Christianization of Greenland were Hans and Poul Egede and Matthias Stach. The New Testament was translated piecemeal from the time of the first settlement on Kangeq Island, but the first translation of the whole Bible was not completed until 1900. An improved translation using the modern orthography was completed in 2000.
The major religion is Protestant Christianity, represented mainly by the Church of Denmark, which is Lutheran in orientation. There are no official census data on religion in Greenland, but the Bishop of Greenland Sofie Petersen estimates that 85% of the Greenlandic population are members of her congregation. The Church of Denmark is the established church through the Constitution of Denmark.
The Roman Catholic minority is pastorally served by the Roman Catholic Diocese of Copenhagen. There are still Christian missionaries on the island, but mainly from charismatic movements proselytizing fellow Christians.
Culture
.JPG)
Greenlandic culture is a blending of traditional Inuit (Kalaallit, Tunumiit, Inughuit) and Scandinavian culture. Inuit, or Kalaallit, culture has a strong artistic tradition, dating back thousands of years. The Kalaallit are known for an art form of figures called tupilak or a "spirit object". Traditional art-making practices thrive in the Ammassalik. Sperm whale ivory remains a valued medium for carving.
Music
Greenland has a successful, albeit small, music culture. Some popular Greenlandic bands and artists include Sumé (classic rock), Chilly Friday (rock), Nanook (rock), Siissisoq (rock), Nuuk Posse (hip hop) and Rasmus Lyberth (folk), who performed in the Danish national final for the 1979 Eurovision Song Contest, performing in Greenlandic. The singer-songwriter Simon Lynge is the first musical artist from Greenland to have an album released across the United Kingdom, and to perform at the UK's Glastonbury Festival. The music culture of Greenland also includes traditional Inuit music, largely revolving around singing and drums.
The drum is the traditional Greenlandic instrument. It was used to perform traditional drum dances. For this purpose, a round drum (qilaat) in the form of a frame made of driftwood or walrus ribs covered with a polar bear bladder, polar bear stomach or walrus stomach was used. The drumming was not done on the membrane, but with a stick from underneath the frame. Simple melodies were sung for this purpose.
The drum dance used to serve two functions. One was to drive away fear on long, dark winter nights by making faces and trying to make others laugh. Disputes were also settled with the drum. If someone had misbehaved, he was challenged with the drum. People would gather at certain powerful places and take turns beating the drum and singing to it. They tried to ridicule the other person as much as possible. The spectators expressed with their laughter who was the winner and who was therefore the guilty one.
The drum could also be used by shamans for ritual conjurations of spirits.
After the arrival of missionaries in the 18th century, the drum dance (still popular among Canadian Inuit) was banned as pagan and shamanistic and replaced by polyphonic singing of secular and church songs. This choral singing is known for its special sound. Church hymns are partly of German origin due to the influence of the Herrnhuter Brüdergemeinde. Scandinavian, German and Scottish whalers brought the fiddle, accordion and polka (kalattuut) to Greenland, where they are now played in intricate dance steps.
Sport
Sport is an important part of Greenlandic culture, as the population is generally quite active. Popular sports include association football, track and field, handball and skiing. Handball is often referred to as the national sport, and the men's national team was ranked among the top 20 in the world in 2001.
Greenland has excellent conditions for skiing, fishing, snowboarding, ice climbing and rock climbing, although mountain climbing and hiking are preferred by the general public. Although the environment is generally ill-suited for golf, there is a golf course in Nuuk.
Cuisine
.png)
The national dish of Greenland is suaasat, a soup made from seal meat. Meat from marine mammals, game, birds, and fish have a large role in the Greenlandic diet. Due to the glacial landscape, most ingredients come from the ocean. Spices are seldom used besides salt and pepper. Greenlandic coffee is a "flaming" dessert coffee (set alight before serving) made with coffee, whiskey, Kahlúa, Grand Marnier, and whipped cream. It is stronger than the familiar Irish dessert coffee.
Media
Kalaallit Nunaata Radioa (KNR) is the public broadcasting company of Greenland. It is an associate member of Eurovision and an associate member of the Nordvision network. Nearly one hundred people are directly employed by this company, which is one of the largest in the territory. The city of Nuuk also has its own radio and television station. The city of Nuuk also has a local television channel, Nanoq Media, which was created on 1 August 2002. It is the largest local television station in Greenland, reaching more than 4,000 households as receiving members, which corresponds to about 75% of all households in the capital.
Only two newspapers are published in Greenland, both of which are distributed nationally. The Greenlandic weekly Sermitsiaq is published every Friday, while the online version is updated several times a day. It was distributed only in Nuuk until the 1980s. It is named after the mountain Sermitsiaq, located about 15 km (9.5 mi) northeast of Nuuk. The bi-weekly Atuagagdliutit/Grønlandsposten (AG) is the other newspaper in Greenland, published every Tuesday and Thursday in Greenlandic as Atuagagdliutit and in Danish as Grønlandsposten. The articles are all published in both languages.
Fine arts
The Inuit have their own arts and crafts tradition; for example, they carve tupilaks, sculptures of figures of avenging monsters practiced within shaman traditions. This Kalaallisut word means soul or spirit of a deceased person and describes an artistic figure, usually no more than 20 centimetres (8 in) tall, carved mainly from walrus ivory, with a variety of unusual shapes. This sculpture actually represents a mythical or spiritual being; usually, however, it has become a mere collector's item because of its grotesque appearance for Western visual habits. Modern artisans still use indigenous materials such as musk ox and sheep wool, seal fur, shells, soapstone, reindeer antlers or gemstones.
The history of Greenlandic painting began with Aron von Kangeq, who depicted the old Greenlandic sagas and myths in his drawings and watercolours in the mid-19th century. In the 20th century, landscape and animal painting developed, as well as printmaking and book illustrations with sometimes expressive colouring. It was mainly through their landscape paintings that Kiistat Lund and Buuti Pedersen became known abroad. Anne-Birthe Hove chose themes from Greenlandic social life. There is a museum of fine arts in Nuuk, the Nuuk Art Museum.
See also
In Spanish: Groenlandia para niños
