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| established_date = {{start date|1928|01|23|df=y}}
| established_date = {{start date|1928|01|23|df=y}}
| established_title2 = Dependency status
| established_title2 = Dependency status
| established_date2 = 27 February 1930<ref name="LOV19300227" />
| established_date2 = 27 February 1930<ref name="LOV19300227"/>
| established_title3 = Nature reserve declared
| established_title3 = Nature reserve declared
| established_date3 = 17 December 1971<ref name="FOR19711217" />
| established_date3 = 17 December 1971<ref name="FOR19711217"/>
| government_type = [[Dependent territory|Dependency]] under a [[constitutional monarchy]]
| government_type = [[Dependent territory|Dependency]] under a [[constitutional monarchy]]
| leader_title1 = [[Monarchy of Norway|Monarch]]
| leader_title1 = [[Monarchy of Norway|Monarch]]
Line 25: Line 25:
| leader_title2 = Administered by
| leader_title2 = Administered by
| leader_name2 = [[Ministry of Justice and Public Security]]
| leader_name2 = [[Ministry of Justice and Public Security]]
| leader_title3 = Baron (de jure)
| leader_name3 = [[Nils Olav III]]
| area_km2 = 49
| area_km2 = 49
| area_label2 = [[Glacier|Glaciated]]
| area_label2 = [[Glacier|Glaciated]]
Line 39: Line 41:
|official_languages=[[Norwegian language|Norwegian]]
|official_languages=[[Norwegian language|Norwegian]]
}}
}}
'''Bouvet Island''' ({{IPAc-en|ˈ|b|uː|v|eɪ}} {{respell|BOO|vay}}; {{Lang-no|Bouvetøya}}<ref name="polar-stadnamn-Bouvetøya" /> {{IPA-no|bʉˈvèːœʏɑ|}})<ref name="Berulfsen-1969" /> is an island and dependency of [[Norway]], and declared an uninhabited protected nature reserve. It is a [[subantarctic]] volcanic island, situated in the South [[Atlantic Ocean]] at the southern end of the [[Mid-Atlantic Ridge]], and is the world's most [[extreme points of Earth#Remoteness|remote]] island. It is not part of the southern region covered by the [[Antarctic Treaty System]].
'''Bouvet Island''' ({{IPAc-en|ˈ|b|uː|v|eɪ}} {{respell|BOO|vay}}; {{Langx|no|Bouvetøya}}<ref name="polar-stadnamn-Bouvetøya"/> {{IPA-no|bʉˈvèːœʏɑ|}})<ref name="Berulfsen-1969"/> is an uninhabited [[subantarctic]] volcanic island and dependency of [[Norway]]. It is a protected nature reserve, and situated in the South [[Atlantic Ocean]] at the southern end of the [[Mid-Atlantic Ridge]], it is the world's most [[extreme points of Earth#Remoteness|remote]] island. Located north of the [[Antarctic Circle]], Bouvet Island is not part of the southern region covered by the [[Antarctic Treaty System]].


The island lies {{cvt|1700|km}} north of the [[Princess Astrid Coast]] of [[Queen Maud Land]], [[Antarctica]], {{cvt|1900|km}} east of the [[South Sandwich Islands]], {{cvt|1845|km}} south of [[Gough Island]], and {{cvt|2600|km}} south-southwest of the coast of South Africa. It has an area of {{cvt|49|km2}}, 93&nbsp;percent of which is covered by a [[glacier]]. The centre of the island is the ice-filled crater of an inactive [[volcano]]. Some [[Skerry|skerries]] and one smaller island, [[Larsøya]], lie along its coast. Nyrøysa, created by a rock slide in the late 1950s, is the only easy place to land and is the location of a [[weather station]].
The island lies {{cvt|1700|km}} north of the [[Princess Astrid Coast]] of [[Queen Maud Land]], [[Antarctica]], {{cvt|1870|km}} east of the [[South Sandwich Islands]], {{cvt|1845|km}} south of [[Gough Island]], and {{cvt|2520|km}} south-southwest of the coast of South Africa. It has an area of {{cvt|49|km2}}, 93&nbsp;percent of which is covered by a [[glacier]]. The centre of the island is the ice-filled crater of an inactive [[volcano]]. Some [[Skerry|skerries]] and one smaller island, [[Larsøya]], lie along its coast. Nyrøysa, created by a rock slide in the late 1950s, is the only easy place to land and is the location of a [[weather station]].


The island was first spotted on 1&nbsp;January 1739 by the Frenchman [[Jean-Baptiste Charles Bouvet de Lozier]], during a French exploration mission in the [[South Atlantic]] with the ships ''Aigle'' and ''Marie''. They did not make landfall. He mislabeled the coordinates for the island, and it was not sighted again until 1808, when the British [[whaler]] James Lindsay encountered it and named it '''Lindsay Island'''.<ref name="Mills-2003-1-96" /> The first claim to have landed on the island was made by the American sailor [[Benjamin Morrell]], although this claim is disputed. In 1825, the island was claimed for the [[British Crown]] by George Norris, who named it '''Liverpool Island'''. He also reported having sighted another island nearby, which he named [[Thompson Island (South Atlantic)|Thompson Island]], but this was later shown to be a [[phantom island]].
The island was first spotted on 1&nbsp;January 1739 by the Frenchman [[Jean-Baptiste Charles Bouvet de Lozier]], during a French exploration mission in the [[South Atlantic]] with the ships ''Aigle'' and ''Marie''. They did not make landfall. He mislabeled the coordinates for the island, and it was not sighted again until 1808, when the British [[whaler]] James Lindsay encountered it and named it '''Lindsay Island'''.<ref name="Mills-2003-1-96"/> The first claim to have landed on the island was made by the American sailor [[Benjamin Morrell]], although this claim is disputed. In 1825, the island was claimed for the [[British Crown]] by George Norris, who named it '''Liverpool Island'''. He also reported having sighted another island nearby, which he named [[Thompson Island (South Atlantic)|Thompson Island]], but this was later shown to be a [[phantom island]].


In 1927, the [[Hjalmar Riiser-Larsen#The Norvegia expeditions|first ''Norvegia'' expedition]] landed on the island, and claimed it for Norway. At that point, the island was given its current name of ''Bouvet Island'' ("Bouvetøya" in Norwegian).<ref name="wordpress-abandoned-lifeboat" /> In 1930, following resolution of a dispute with the United Kingdom over claiming rights, it was declared a Norwegian dependency. In 1971, it was designated a [[nature reserve]].
In 1927, the [[Hjalmar Riiser-Larsen#The Norvegia expeditions|first ''Norvegia'' expedition]] landed on the island, and claimed it for Norway. At that point, the island was given its current name of ''Bouvet Island'' ("Bouvetøya" in Norwegian).<ref name="wordpress-abandoned-lifeboat"/> In 1930, following resolution of a dispute with the United Kingdom over claiming rights, it was declared a Norwegian dependency. In 1971, it was designated a [[nature reserve]].


== History ==
== History ==
=== Discovery and early sightings ===
=== Discovery and early sightings ===
[[File:Bouvet island 0.jpg|thumb|upright=1.3|Hand-coloured photograph of the southeast coast of Bouvet Island in 1898]]
[[File:Bouvet island 0.jpg|thumb|upright=1.3|Hand-coloured photograph of the southeast coast of Bouvet Island in 1898]]
The island was discovered on 1 January 1739 by [[Jean-Baptiste Charles Bouvet de Lozier]], commander of the French ships ''Aigle'' and ''Marie''.<ref name="Mills-2003-1-96" /> Bouvet, who was searching for a presumed large southern continent, spotted the island through the fog and named the cape he saw [[Cap de la Circoncision]]. He was not able to land and did not [[circumnavigate]] his discovery, thus not clarifying if it was an island or part of [[Terra Australis|a continent]].<ref name="Barr-1987" />{{rp|page=62}} His plotting of its position was inaccurate,<ref name="Mill-1905" />{{rp|page=47}} leading several expeditions to fail to find the island.<ref name="Barr-1987" />{{rp|page=58}} [[James Cook]]'s [[second voyage of James Cook|second voyage]] set off from [[Cape Verde]] on 22 November 1772 and attempted to find the island, but also failed.<ref name="Hough-1994" />
The island was discovered on 1 January 1739 by [[Jean-Baptiste Charles Bouvet de Lozier]], commander of the French ships ''Aigle'' and ''Marie''.<ref name="Mills-2003-1-96"/> Bouvet, who was searching for a presumed large southern continent, spotted the island through the fog and named the cape he saw [[Cap de la Circoncision]]. He was not able to land and did not [[circumnavigate]] his discovery, thus not clarifying if it was an island or part of [[Terra Australis|a continent]].<ref name="Barr-1987"/>{{rp|page=62}} His plotting of its position was inaccurate,<ref name="Mill-1905"/>{{rp|page=47}} leading several expeditions to fail to find the island.<ref name="Barr-1987"/>{{rp|page=58}} [[James Cook]]'s [[second voyage of James Cook|second voyage]] set off from [[Cape Verde]] on 22 November 1772 and attempted to find the island, but also failed.<ref name="Hough-1994"/>


The next expedition to spot the island was in 1808 by James Lindsay, captain of the [[Samuel Enderby & Sons]]' (SE&S) [[Snow (ship)|snow]] [[whaler]] ''Swan''.<ref name="Burney-1817" /> ''Swan'' and another Enderby whaler, {{ship||Otter|1807 ship|2}} were in company when they reached the island and recorded its position, though they were unable to land.<ref name="McGonigal-2003" /><ref name="Mills-2003" />{{rp|pages=434–435}} Lindsay could confirm that the "cape" was indeed an island.<ref name="Barr-1987" />{{rp|page=62}} The next expedition to arrive at the island was American [[Benjamin Morrell]] and his [[seal hunting]] ship ''Wasp''. Morrell, by his own account, found the island without difficulty (with "improbable ease", in the words of historian William Mills)<ref name="Mills-2003" />{{rp|pages=434–435}} before landing and hunting 196&nbsp;seals.<ref name="Barr-1987" />{{rp|page=62}} In his subsequent lengthy description, Morrell does not mention the island's most obvious physical feature: Its permanent ice cover.<ref name="Mill-1905" />{{rp|pages=106–107}} This has caused some commentators to doubt whether he actually visited the island.<ref name="Mills-2003" />{{rp|pages=434–435}}<ref name="Simpson-Housley-1992" />
The next expedition to spot the island was in 1808 by James Lindsay, captain of the [[Samuel Enderby & Sons]]' (SE&S) [[Snow (ship)|snow]] [[whaler]] ''Swan''.<ref name="Burney-1817"/> ''Swan'' and another Enderby whaler, {{ship||Otter|1807 ship|2}} were in company when they reached the island and recorded its position, though they were unable to land.<ref name="McGonigal-2003"/><ref name="Mills-2003"/>{{rp|pages=434–435}} Lindsay could confirm that the "cape" was indeed an island.<ref name="Barr-1987"/>{{rp|page=62}} The next expedition to arrive at the island was American [[Benjamin Morrell]] and his [[seal hunting]] ship ''Wasp''. Morrell, by his own account, found the island without difficulty (with "improbable ease", in the words of historian William Mills)<ref name="Mills-2003"/>{{rp|pages=434–435}} before landing and hunting 196&nbsp;seals.<ref name="Barr-1987"/>{{rp|page=62}} In his subsequent lengthy description, Morrell does not mention the island's most obvious physical feature: Its permanent ice cover.<ref name="Mill-1905"/>{{rp|pages=106–107}} This has caused some commentators to doubt whether he actually visited the island.<ref name="Mills-2003"/>{{rp|pages=434–435}}<ref name="Simpson-Housley-1992"/>


On 10&nbsp;December 1825, SE&S's George Norris, master of the ''Sprightly'', landed on the island,<ref name="Barr-1987" />{{rp|page=62}} named it Liverpool Island and claimed it for the [[British Crown]] and [[George IV]] on 16&nbsp;December.<ref name="Barr-1987" />{{rp|page=63}} The next expedition to spot the island was Joseph Fuller and his ship ''Francis Allyn'' in 1893, but he was not able to land on the island. German [[Carl Chun]]'s [[Valdivia Expedition]] arrived at the island in 1898. They were not able to land, but dredged the seabed for geological samples.<ref name="Baker-1967" /> They were also the first to accurately fix the island's position.<ref name="Barr-1987" />{{rp|page=63}} At least three sealing vessels visited the island between 1822 and 1895. A voyage of exploration in 1927–1928 also took seal pelts.<ref name="Headland-2018" />
On 10&nbsp;December 1825, SE&S's George Norris, master of the ''Sprightly'', landed on the island,<ref name="Barr-1987"/>{{rp|page=62}} named it Liverpool Island and claimed it for the [[British Crown]] and [[George IV]] on 16&nbsp;December.<ref name="Barr-1987"/>{{rp|page=63}} The next expedition to spot the island was Joseph Fuller and his ship ''Francis Allyn'' in 1893, but he was not able to land on the island. German [[Carl Chun]]'s [[Valdivia Expedition]] arrived at the island in 1898. They were not able to land, but dredged the seabed for geological samples.<ref name="Baker-1967"/> They were also the first to accurately fix the island's position.<ref name="Barr-1987"/>{{rp|page=63}} At least three sealing vessels visited the island between 1822 and 1895. A voyage of exploration in 1927–1928 also took seal pelts.<ref name="Headland-2018"/>


Norris also spotted a second island in 1825, which he named [[Thompson Island (South Atlantic)|Thompson Island]], which he placed {{cvt|72|km}} north-northeast of Liverpool Island. Thompson Island was also reported in 1893 by Fuller, but in 1898 Chun did not report seeing such an island, nor has anyone since.<ref name="Baker-1967" /> However, Thompson Island continued to appear on maps as late as 1943.<ref name="ARH-NAM-1943" /> A 1967 paper suggested that the island might have disappeared in an undetected volcanic eruption, but in 1997 it was discovered that the ocean is more than {{cvt|2400|m}} deep in the area.<ref>{{cite web |url=http://www.volcano.si.edu/world/volcano.cfm?vnum=1806-03- |title=Thompson Island |publisher=[[Smithsonian Institution]] |department=[[Global Volcanism Program]] |access-date=8 May 2012 |archive-date=23 September 2012 |archive-url=https://web.archive.org/web/20120923041437/http://www.volcano.si.edu/world/volcano.cfm?vnum=1806-03- |url-status=live |df=dmy}}</ref>
Norris also spotted a second island in 1825, which he named [[Thompson Island (South Atlantic)|Thompson Island]], which he placed {{cvt|72|km}} north-northeast of Liverpool Island. Thompson Island was also reported in 1893 by Fuller, but in 1898 Chun did not report seeing such an island, nor has anyone since.<ref name="Baker-1967"/> However, Thompson Island continued to appear on maps as late as 1943.<ref name="ARH-NAM-1943"/> A 1967 paper suggested that the island might have disappeared in an undetected volcanic eruption, but in 1997 it was discovered that the ocean is more than {{cvt|2400|m}} deep in the area.<ref>{{cite web|url=http://www.volcano.si.edu/world/volcano.cfm?vnum=1806-03-|title=Thompson Island|publisher=[[Smithsonian Institution]]|department=[[Global Volcanism Program]]|access-date=8 May 2012|archive-date=23 September 2012|archive-url=https://web.archive.org/web/20120923041437/http://www.volcano.si.edu/world/volcano.cfm?vnum=1806-03-|url-status=live}}</ref>


=== Norwegian annexation ===
=== Norwegian annexation ===
[[File:Bouvet Island 1927.jpg|thumb|upright=1.3|The claiming of the island on 1&nbsp;December 1927]]
[[File:Bouvet Island 1927.jpg|thumb|upright=1.3|The claiming of the island on 1&nbsp;December 1927]]
[[File:Cape Circoncision - Bouvet Island.jpg|thumb|upright=1.3|The first hut, built on [[Cape Circoncision]], in 1929]]
[[File:Cape Circoncision - Bouvet Island.jpg|thumb|upright=1.3|The first hut, built on [[Cape Circoncision]], in 1929]]
In 1927, the First ''Norvegia'' Expedition, led by Harald Horntvedt and financed by the shipowner and philanthropist [[Lars Christensen]], was the first to make an extended stay on the island. Observations and surveying were conducted on the island and [[oceanographic]] measurements performed in the sea around it. At Ny Sandefjord, a small hut was erected and, on 1&nbsp;December, the [[Flag of Norway|Norwegian flag]] was hoisted and the island claimed for Norway. The annexation was established by a royal decree on 23&nbsp;January 1928.<ref name="Barr-1987" />{{rp|page=63}}
In 1927, the First ''Norvegia'' Expedition, led by Harald Horntvedt and financed by the shipowner and philanthropist [[Lars Christensen]], was the first to make an extended stay on the island. Observations and surveying were conducted on the island and [[oceanographic]] measurements performed in the sea around it. At Ny Sandefjord, a small hut was erected and, on 1&nbsp;December, the [[Flag of Norway|Norwegian flag]] was hoisted and the island claimed for Norway. The annexation was established by a royal decree on 23&nbsp;January 1928.<ref name="Barr-1987"/>{{rp|page=63}}


The claim was initially protested by the United Kingdom, on the basis of Norris's landing and annexation. However, the British position was weakened by Norris's sighting of two islands and the uncertainty as to whether he had been on Thompson or Liverpool (i.e. Bouvet) Island. Norris's positioning deviating from the correct location combined with the island's small size and lack of a [[natural harbour]] made the UK accept the Norwegian claim.<ref name="Kyvik-2008" />{{rp|page=52}} This resulted in diplomatic negotiations between the two countries, and in November 1929, Britain renounced its claim to the island.<ref name="Barr-1987" />{{rp|page=63}}
The claim was initially protested by the United Kingdom, on the basis of Norris's landing and annexation. However, the British position was weakened by Norris's sighting of two islands and the uncertainty as to whether he had been on Thompson or Liverpool (i.e. Bouvet) Island. Norris's positioning deviating from the correct location combined with the island's small size and lack of a [[natural harbour]] made the UK accept the Norwegian claim.<ref name="Kyvik-2008"/>{{rp|page=52}} This resulted in diplomatic negotiations between the two countries, and in November 1929, Britain renounced its claim to the island.<ref name="Barr-1987"/>{{rp|page=63}}


The [[Hjalmar Riiser-Larsen#The Norvegia expeditions|Second ''Norvegia'' Expedition]] arrived in 1928 with the intent of establishing a staffed meteorological radio station, but a suitable location could not be found.<ref name="Barr-1987" />{{rp|page=63}} By then both the flagpole and hut from the previous year had been washed away. The [[Hjalmar Riiser-Larsen#The Norvegia expeditions|Third ''Norvegia'' Expedition]], led by [[Hjalmar Riiser-Larsen]], arrived the following year and built a new hut at [[Cape Circoncision]] and on Larsøya. The expedition carried out [[aerial photography]] of the island and was the first Antarctic expedition to use aircraft.<ref name="Barr-1987" />{{rp|page=64}} The ''Dependency Act'', passed by the [[Parliament of Norway]] on 27&nbsp;February 1930, established Bouvet Island as a Norwegian dependency, along with [[Peter I Island]] and [[Queen Maud Land]].<ref name="LOV19300227">{{Cite web |title=Lov om Bouvet-øya, Peter&nbsp;I's øy og Dronning Maud Land m.m. (bilandsloven) |url=http://www.lovdata.no/all/tl-19300227-003-0.html#1 |language=no |publisher=Lovdata |access-date=29 August 2011 |archive-date=2 December 2013 |archive-url=https://web.archive.org/web/20131202231248/http://www.lovdata.no/all/tl-19300227-003-0.html |url-status=live}}</ref> The [[eared seal]] was protected on and around the island in 1929, and in 1935 all seals around the island were protected.<ref name="placenames-npolar-Bouvetøya" />
The [[Hjalmar Riiser-Larsen#The Norvegia expeditions|Second ''Norvegia'' Expedition]] arrived in 1928 with the intent of establishing a staffed meteorological radio station, but a suitable location could not be found.<ref name="Barr-1987"/>{{rp|page=63}} By then both the flagpole and hut from the previous year had been washed away. The [[Hjalmar Riiser-Larsen#The Norvegia expeditions|Third ''Norvegia'' Expedition]], led by [[Hjalmar Riiser-Larsen]], arrived the following year and built a new hut at [[Cape Circoncision]] and on Larsøya. The expedition carried out [[aerial photography]] of the island and was the first Antarctic expedition to use aircraft.<ref name="Barr-1987"/>{{rp|page=64}} The ''Dependency Act'', passed by the [[Parliament of Norway]] on 27&nbsp;February 1930, established Bouvet Island as a Norwegian dependency, along with [[Peter I Island]] and [[Queen Maud Land]].<ref name="LOV19300227"/> The [[eared seal]] was protected on and around the island in 1929, and in 1935 all seals around the island were protected.<ref name="placenames-npolar-Bouvetøya"/>


=== Recent history ===
=== Recent history ===
In 1955, the South African frigate {{ship|SAS|Transvaal}} visited the island.<ref>{{cite journal |title=South African expedition to Bouvetøya, 1955 |journal=[[Polar Record]] |volume=8 |issue=54 |date=September 1956 |pages=256–258 |doi=10.1017/S003224740004907X |bibcode=1956PoRec...8..256. |s2cid=251062020}}</ref> Nyrøysa, a rock-strewn ice-free area, the largest such on Bouvet, was created sometime between 1955 and 1958, probably by a landslide.<ref>{{Cite web |url=http://www.birdlife.org/datazone/userfiles/file/IBAs/AfricaCntryPDFs/Bouvet.pdf |title=Bouvet |access-date=11 May 2012 |archive-url=https://web.archive.org/web/20130313172001/http://www.birdlife.org/datazone/userfiles/file/IBAs/AfricaCntryPDFs/Bouvet.pdf |archive-date=13 March 2013 |url-status=live |df=dmy-all}}</ref>
In 1955, the South African frigate {{ship|SAS|Transvaal}} visited the island.<ref>{{cite journal|title=South African expedition to Bouvetøya, 1955|journal=[[Polar Record]]|volume=8|issue=54|date=September 1956|pages=256–258|doi=10.1017/S003224740004907X|bibcode=1956PoRec...8..256.|s2cid=251062020}}</ref> Nyrøysa, a rock-strewn ice-free area, the largest such on Bouvet, was created sometime between 1955 and 1958, probably by a landslide.<ref>{{Cite web|url=http://www.birdlife.org/datazone/userfiles/file/IBAs/AfricaCntryPDFs/Bouvet.pdf|title=Bouvet|access-date=11 May 2012|archive-url=https://web.archive.org/web/20130313172001/http://www.birdlife.org/datazone/userfiles/file/IBAs/AfricaCntryPDFs/Bouvet.pdf|archive-date=13 March 2013|url-status=live}}</ref>


In 1964, the island was visited by the British naval ship {{HMS|Protector|A146|6}}. One of ''Protector''{{'}}s two [[Westland Whirlwind (helicopter)|Westland Whirlwind]] helicopters landed a small survey team on the island led by [[Lieutenant Commander]] Alan Crawford at Nyrøysa for a brief visit. Shortly after landing, the survey team discovered an abandoned [[Lifeboat (shipboard)|lifeboat]] in a small lagoon. With very little time, a brief search was made but no other signs of human activity were found, and the identity of the lifeboat remained a mystery for many years.<ref>{{Cite book |last=Crawford |first=Allan |title=Tristan da Cunha and the Roaring Forties |publisher=Charles Skilton Ltd |year=1982 |isbn=978-0-284-98589-7 |location=Edinburgh |oclc=868642138}}</ref>{{rp|177–85}}
In 1964, the island was visited by the British naval ship {{HMS|Protector|A146|6}}. One of ''Protector''{{'}}s two [[Westland Whirlwind (helicopter)|Westland Whirlwind]] helicopters landed a small survey team on the island led by [[Lieutenant Commander]] Alan Crawford at Nyrøysa for a brief visit. Shortly after landing, the survey team discovered an abandoned [[Lifeboat (shipboard)|lifeboat]] in a small lagoon. With very little time, a brief search was made but no other signs of human activity were found, and the identity of the lifeboat remained a mystery for many years.<ref>{{Cite book|last=Crawford|first=Allan|title=Tristan da Cunha and the Roaring Forties|publisher=Charles Skilton Ltd|year=1982|isbn=978-0-284-98589-7|location=Edinburgh|oclc=868642138}}</ref>{{rp|177–85}}


On 17&nbsp;December 1971, the entire island and its territorial waters were protected as a [[nature reserve]].<ref name="FOR19711217">{{cite web |title=Forskrift om fredning av Bouvetøya med tilliggende territorialfarvann som naturreservat |url=http://lovdata.no/for/sf/md/xd-19711217-0009.html |language=no |publisher=Lovdata |access-date=9 May 2012 |archive-date=6 June 2014 |archive-url=https://web.archive.org/web/20140606224540/http://lovdata.no/for/sf/md/xd-19711217-0009.html |url-status=live |df=dmy}}</ref> A scientific landing was made in 1978, during which the underground temperature was measured to be {{cvt|25|C}}.<ref name="Rubin-2005" /> In addition to scientific surveys,<ref name="Baker-1967" /> the lifeboat found by the ''Protector'' team was recovered from Nyrøysa, although no other signs of people were found.<ref name="Rubin-2005" /> The lifeboat was believed to belong to a Soviet scientific reconnaissance vessel.{{efn|The scientific reconnaissance vessel 'Slava-9' began its regular 13th cruise with the 'Slava' Antarctic whaling fleet on 22&nbsp;October 1958 ... On 27&nbsp;November she got to Bouvet Island. A group of sailors landed, but were unable to leave the island in time because of worsened weather and stayed on it for about 3&nbsp;days. The people were withdrawn by helicopter on 29&nbsp;November 1958.<ref>{{Cite book |title=Transactions of the Oceanographical Institute |pages=129}}</ref>}}
On 17&nbsp;December 1971, the entire island and its territorial waters were protected as a [[nature reserve]].<ref name="FOR19711217"/> A scientific landing was made in 1978, during which the underground temperature was measured to be {{cvt|25|C}}.<ref name="Rubin-2005"/> In addition to scientific surveys,<ref name="Baker-1967"/> the lifeboat found by the ''Protector'' team was recovered from Nyrøysa, although no other signs of people were found.<ref name="Rubin-2005"/> The lifeboat was believed to belong to a Soviet scientific reconnaissance vessel.{{efn|The scientific reconnaissance vessel 'Slava-9' began its regular 13th cruise with the 'Slava' Antarctic whaling fleet on 22&nbsp;October 1958 ... On 27&nbsp;November she got to Bouvet Island. A group of sailors landed, but were unable to leave the island in time because of worsened weather and stayed on it for about 3&nbsp;days. The people were withdrawn by helicopter on 29&nbsp;November 1958.<ref>{{Cite book|title=Transactions of the Oceanographical Institute|pages=129}}</ref>}}


The [[Vela incident]] took place on 22&nbsp;September 1979, on or above the sea between Bouvetøya and [[Prince Edward Islands]], when the American [[Vela (satellite)|Vela Hotel]] satellite&nbsp;6911 registered an unexplained [[effects of nuclear explosions|double flash]]. This observation has been variously interpreted as a meteor, or an instrumentation glitch, but most independent assessments conclude it was an [[South Africa and weapons of mass destruction#Nuclear weapons|undeclared joint nuclear test]] carried out by South Africa and Israel.<ref name="Rubin-2005" /><ref name="Hersh-1991" /><ref name="Rhodes-2011" /><ref name="Weiss-2011" />
The [[Vela incident]] took place on 22&nbsp;September 1979, on or above the sea between Bouvetøya and [[Prince Edward Islands]], when the American [[Vela (satellite)|Vela Hotel]] satellite&nbsp;6911 registered an unexplained [[effects of nuclear explosions|double flash]]. This observation has been variously interpreted as a meteor, or an instrumentation glitch, but most independent assessments conclude it was an [[Vela incident|undeclared joint nuclear test]] carried out by South Africa and Israel.<ref name="Rubin-2005"/><ref name="Hersh-1991"/><ref name="Rhodes-2011"/><ref name="Weiss-2011"/>


In the mid-1980s<!--1984–1987-->, Bouvetøya, [[Jan Mayen]], and [[Svalbard]] were considered as locations for the new [[Norwegian International Ship Register]], but the [[flag of convenience]] registry was ultimately established in [[Bergen]], Norway, in 1987.<ref name="Kyvik-2008" />{{rp|page=189}}
In the mid-1980s<!--1984–1987-->, Bouvetøya, [[Jan Mayen]], and [[Svalbard]] were considered as locations for the new [[Norwegian International Ship Register]], but the [[flag of convenience]] registry was ultimately established in [[Bergen]], Norway, in 1987.<ref name="Kyvik-2008"/>{{rp|page=189}}
In 2007, the island was added to Norway's tentative list of nominations as a [[World Heritage Site]] as part of the transnational nomination of the Mid-Atlantic Ridge.<ref>{{cite web |url=https://whc.unesco.org/en/tentativelists/5162/ |title=Islands of Jan Mayen and Bouvet as parts of a serial transnational nomination of the Mid-Atlantic Ridge system |publisher=[[UNESCO]] |access-date=9 May 2012 |archive-date=8 August 2012 |archive-url=https://web.archive.org/web/20120808163044/https://whc.unesco.org/en/tentativelists/5162/ |url-status=live |df=dmy}}</ref>
In 2007, the island was added to Norway's tentative list of nominations as a [[World Heritage Site]] as part of the transnational nomination of the Mid-Atlantic Ridge.<ref>{{cite web|url=https://whc.unesco.org/en/tentativelists/5162/|title=Islands of Jan Mayen and Bouvet as parts of a serial transnational nomination of the Mid-Atlantic Ridge system|publisher=[[UNESCO]]|access-date=9 May 2012|archive-date=8 August 2012|archive-url=https://web.archive.org/web/20120808163044/https://whc.unesco.org/en/tentativelists/5162/|url-status=live}}</ref>


[[Krill fishery|Krill fishing]] in the Southern Ocean is subject to the [[Convention for the Conservation of Antarctic Marine Living Resources]], which defines maximum catch quotas for a [[sustainable fisheries|sustainable exploitation]] of [[Antarctic krill]].<ref name="Schiermeier-2010" /> Surveys conducted in 2000 showed high concentration of krill around Bouvetøya. In 2004, [[Aker BioMarine]] was awarded a concession to fish krill, and additional quotas were awarded from 2008 for a total catch of {{cvt|620000|t}}.<ref>{{cite news |url=http://nrk.no/okonomi/krill---eit-nytt-oljeeventyr_-1.4984136 |title=Satsar på krill – eit nytt oljeeventyr |last=Molde |first=Eivind |work=[[Norwegian Broadcasting Corporation]] |date=2 March 2008 |language=no |access-date=9 May 2012 |archive-date=2 April 2015 |archive-url=https://web.archive.org/web/20150402103624/http://www.nrk.no/okonomi/krill---eit-nytt-oljeeventyr_-1.4984136 |url-status=live |df=dmy}}</ref> There is a controversy as to whether the fisheries are sustainable, particularly in relation to krill being important food for whales.<ref>{{cite news |url=http://www.nrk.no/nyheter/norge/1.3952784 |title=Norge tek maten frå kvalen |last=Haram |first=Øyvind Andre |work=[[Norwegian Broadcasting Corporation]] |date=5 November 2007 |language=no |access-date=9 May 2012 |archive-date=6 September 2012 |archive-url=https://archive.today/20120906094448/http://www.nrk.no/nyheter/norge/1.3952784 |url-status=live |df=dmy}}</ref> In 2009, Norway filed with the [[UN Commission on the Limits of the Continental Shelf]] to extend the outer limit of the continental shelf past {{cvt|200|NM|mi km|sp=us}} surrounding the island.<ref>{{cite web |url=http://folk.uio.no/giudittm/IACL_10_IIID%20Norway.pdf |title=The Law applicable to the Continental Shelf and in the Exclusive Economic Zone |last=Cordero-Moss |first=Giuditta |publisher=[[University of Oslo]] |access-date=9 May 2012 |archive-date=4 July 2013 |archive-url=https://web.archive.org/web/20130704103645/http://folk.uio.no/giudittm/IACL_10_IIID%20Norway.pdf |url-status=live |df=dmy}}</ref>
[[Krill fishery|Krill fishing]] in the Southern Ocean is subject to the [[Convention for the Conservation of Antarctic Marine Living Resources]], which defines maximum catch quotas for a [[sustainable fisheries|sustainable exploitation]] of [[Antarctic krill]].<ref name="Schiermeier-2010"/> Surveys conducted in 2000 showed high concentration of krill around Bouvetøya. In 2004, [[Aker BioMarine]] was awarded a concession to fish krill, and additional quotas were awarded from 2008 for a total catch of {{cvt|620000|t}}.<ref>{{cite news|url=http://nrk.no/okonomi/krill---eit-nytt-oljeeventyr_-1.4984136|title=Satsar på krill – eit nytt oljeeventyr|last=Molde|first=Eivind|work=[[Norwegian Broadcasting Corporation]]|date=2 March 2008|language=no|access-date=9 May 2012|archive-date=2 April 2015|archive-url=https://web.archive.org/web/20150402103624/http://www.nrk.no/okonomi/krill---eit-nytt-oljeeventyr_-1.4984136|url-status=live}}</ref> There is a controversy as to whether the fisheries are sustainable, particularly in relation to krill being important food for whales.<ref>{{cite news|url=http://www.nrk.no/nyheter/norge/1.3952784|title=Norge tek maten frå kvalen|last=Haram|first=Øyvind Andre|work=[[Norwegian Broadcasting Corporation]]|date=5 November 2007|language=no|access-date=9 May 2012|archive-date=6 September 2012|archive-url=https://archive.today/20120906094448/http://www.nrk.no/nyheter/norge/1.3952784|url-status=live}}</ref> In 2009, Norway filed with the [[UN Commission on the Limits of the Continental Shelf]] to extend the outer limit of the continental shelf past {{cvt|200|NM|mi km|sp=us}} surrounding the island.<ref>{{cite web|url=http://folk.uio.no/giudittm/IACL_10_IIID%20Norway.pdf|title=The Law applicable to the Continental Shelf and in the Exclusive Economic Zone|last=Cordero-Moss|first=Giuditta|publisher=[[University of Oslo]]|access-date=9 May 2012|archive-date=4 July 2013|archive-url=https://web.archive.org/web/20130704103645/http://folk.uio.no/giudittm/IACL_10_IIID%20Norway.pdf|url-status=live}}</ref>


The expedition ship ''Hanse Explorer'' visited Bouvet Island on 20 and 21&nbsp;February 2012 as part of "Expédition pour le Futur".<ref name="Expedition-Futur-2012-03-12" /> The expedition's goal was to land and climb the highest point on the island.{{efn|The first four climbers (Aaron Halstead, Will Allen, Bruno Rodi and Jason Rodi) were the first humans to climb the highest peak. A [[time capsule]] containing the top visions of the future for 2062 was left behind. The next morning, Aaron Halstead led five other climbers (Sarto Blouin, Seth Sherman, Chakib Bouayed, [[Cindy Sampson]], and Akos Hivekovics) to the top.<ref name="Expedition-Futur-2012-03-12" />}}
The expedition ship ''Hanse Explorer'' visited Bouvet Island on 20 and 21&nbsp;February 2012 as part of "Expédition pour le Futur".<ref name="Expedition-Futur-2012-03-12"/> The expedition's goal was to land and climb the highest point on the island.{{efn|The first four climbers (Aaron Halstead, Will Allen, Bruno Rodi and Jason Rodi) were the first humans to climb the highest peak. A [[time capsule]] containing the top visions of the future for 2062 was left behind. The next morning, Aaron Halstead led five other climbers (Sarto Blouin, Seth Sherman, Chakib Bouayed, [[Cindy Sampson]], and Akos Hivekovics) to the top.<ref name="Expedition-Futur-2012-03-12"/>}}


Bouvet Island is assigned the amateur radio callsign prefix 3Y0,<ref>{{cite web |title=International Call Sign Series |url=http://www.arrl.org/international-call-sign-series |website=ARRL – The National Association for Amateur Radio |publisher=The National Association for Amateur Radio |access-date=2021-10-01}}</ref> and several amateur radio [[DX-pedition]]s have been conducted to the island.<ref name="DX-Bouvet-1989-1990" /><ref name="DX-Bouvet-3Y5X" /><ref name="DX-Bouvet-3Y0E" /><ref name="radcom199008_3y5x">{{ cite magazine | url=https://archive.org/details/RadCom_Magazine_1990-08/page/n11/mode/2up | title=The Club Bouvet 3Y5X Story | magazine=Radio Communication | last1=Enderud | first1=Einar | last2=Pedersen | first2=Kåre | date=August 1990 | access-date=24 February 2024 | pages=12–13, 61 }}</ref> The [[3Y0J Bouvet Island DXpedition|3Y0J DX-pedition to Bouvet Island]] took place between January and February 2023, but had to be reduced in scope and eventually cut short due to bad and worsening weather conditions.<ref>{{cite web |title=Bouvet Island DXpedition is On the Air! |url=https://www.arrl.org/news/bouvet-island-dxpedition-is-on-the-air |website=ARRL |publisher=The National Association for Amateur Radio |access-date=2023-02-15}}</ref><ref>{{cite web |title=[QRT] 3Y0J – Bouvet Island |url=https://www.dx-world.net/3y0j-bouvet-island/ |website=DX World |publisher=DX-World.net |access-date=2023-02-15}}</ref>
Bouvet Island is assigned the amateur radio callsign prefix 3Y0,<ref>{{cite web|title=International Call Sign Series|url=http://www.arrl.org/international-call-sign-series|website=ARRL – The National Association for Amateur Radio|publisher=The National Association for Amateur Radio|access-date=2021-10-01}}</ref> and several amateur radio [[DX-pedition]]s have been conducted to the island.<ref name="DX-Bouvet-1989-1990"/><ref name="DX-Bouvet-3Y5X"/><ref name="DX-Bouvet-3Y0E"/><ref name="radcom199008_3y5x"/> The [[3Y0J Bouvet Island DXpedition|3Y0J DX-pedition to Bouvet Island]] took place between January and February 2023, but had to be reduced in scope and eventually cut short due to bad and worsening weather conditions.<ref>{{cite web|title=Bouvet Island DXpedition is On the Air!|url=https://www.arrl.org/news/bouvet-island-dxpedition-is-on-the-air|website=ARRL|publisher=The National Association for Amateur Radio|access-date=2023-02-15}}</ref><ref>{{cite web|title=[QRT] 3Y0J – Bouvet Island|url=https://www.dx-world.net/3y0j-bouvet-island/|website=DX World|publisher=DX-World.net|access-date=2023-02-15}}</ref>


==Norvegia Station==
==Norvegia Station==
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|website = {{URL|https://www.npolar.no/en/norvegia/|npolar.no}}
|website = {{URL|https://www.npolar.no/en/norvegia/|npolar.no}}
}}
}}
Since the 1970s, the island has been visited frequently by Norwegian Antarctic expeditions. In 1977 a temporary five-man station and an [[automated weather station]] were constructed and staffed for two months in 1978 and 1979.<ref name="Barr-1987" />{{rp|page=64}}
Since the 1970s, the island has been visited frequently by Norwegian Antarctic expeditions. In 1977 a temporary five-man station and an [[automated weather station]] were constructed and staffed for two months in 1978 and 1979.<ref name="Barr-1987"/>{{rp|page=64}}


In March&nbsp;1985, a Norwegian expedition experienced sufficiently clear weather to allow the entire island to be photographed from the air, resulting in the first accurate map of the whole island, 247 years after its discovery.<ref name="Barr-1987" />{{rp|page=59}}
In March&nbsp;1985, a Norwegian expedition experienced sufficiently clear weather to allow the entire island to be photographed from the air, resulting in the first accurate map of the whole island, 247 years after its discovery.<ref name="Barr-1987"/>{{rp|page=59}}


The [[Norwegian Polar Institute]] established a {{cvt|36|m2|sqft|adj=on}} research station, made of [[shipping container]]s, at Nyrøysa in 1996. On 23&nbsp;February 2006, the island experienced a magnitude&nbsp;6.2 earthquake whose epicentre was about {{cvt|100|km|mi|sp=us}} away,<ref>{{cite web |title=M&nbsp;6.2 – Bouvet Island region |url=https://earthquake.usgs.gov/earthquakes/eventpage/usp000eang#general_summary |publisher=[[United States Geological Survey]] |access-date=28 August 2017 |archive-url=https://web.archive.org/web/20171107114536/https://earthquake.usgs.gov/earthquakes/eventpage/usp000eang#general_summary |archive-date=7 November 2017 |url-status=live |df=dmy-all}}</ref> weakening the station's foundation and causing it to be blown to sea during a winter storm.<ref>{{cite web |url=http://www.npolar.no/no/nyheter/2007/2007-10-19-norsk-feltstasjon-tatt-av-naturkrefter.html |title=Norsk feltstasjon tatt av naturkreftene ved Antarktis |publisher=[[Norwegian Polar Institute]] |date=20 July 2010 |last=Jaklin |first=Patrick |access-date=9 May 2012 |archive-date=14 March 2013 |archive-url=https://web.archive.org/web/20130314122923/http://www.npolar.no/no/nyheter/2007/2007-10-19-norsk-feltstasjon-tatt-av-naturkrefter.html |url-status=dead |df=dmy}}</ref><ref>{{cite book |last1=Government Publications Office |title=The World Factbook 2016-17 |date=18 August 2016 |publisher=Government Printing Office |isbn=978-0-16-093327-1 |page=104 |url=https://books.google.com/books?id=HfywxU2EnFwC |language=en}}</ref>
The [[Norwegian Polar Institute]] established a {{cvt|36|m2|sqft|adj=on}} research station, made of [[shipping container]]s, at Nyrøysa in 1996. On 23&nbsp;February 2006, the island experienced a magnitude&nbsp;6.2 earthquake whose epicentre was about {{cvt|100|km|mi|sp=us}} away,<ref>{{cite web|title=M&nbsp;6.2 – Bouvet Island region|url=https://earthquake.usgs.gov/earthquakes/eventpage/usp000eang#general_summary|publisher=United States Geological Survey|access-date=28 August 2017|archive-url=https://web.archive.org/web/20171107114536/https://earthquake.usgs.gov/earthquakes/eventpage/usp000eang#general_summary|archive-date=7 November 2017|url-status=live}}</ref> weakening the station's foundation and causing it to be blown to sea during a winter storm.<ref>{{cite web|url=http://www.npolar.no/no/nyheter/2007/2007-10-19-norsk-feltstasjon-tatt-av-naturkrefter.html|title=Norsk feltstasjon tatt av naturkreftene ved Antarktis|publisher=[[Norwegian Polar Institute]]|date=20 July 2010|last=Jaklin|first=Patrick|access-date=9 May 2012|archive-date=14 March 2013|archive-url=https://web.archive.org/web/20130314122923/http://www.npolar.no/no/nyheter/2007/2007-10-19-norsk-feltstasjon-tatt-av-naturkrefter.html|url-status=dead}}</ref><ref>{{cite book|last1=Government Publications Office|title=The World Factbook 2016-17|date=18 August 2016|publisher=Government Printing Office|isbn=978-0-16-093327-1|page=104|url=https://books.google.com/books?id=HfywxU2EnFwC}}</ref>


In December 2012, a new research station was sent by ship from [[Tromsø]] in Norway, via [[Cape Town]], to Bouvet.<ref>{{cite news |last=Molde |first=Eivind |date=7 February 2014 |title=Ny "ekstremstasjon" på Bouvetøya |url=http://www.nrk.no/norge/ny-_ekstremstasjon_-pa-bouvetoya-1.11525409 |newspaper=[[NRK]] |access-date=11 February 2014 |language=no |archive-url=https://web.archive.org/web/20140211023811/http://www.nrk.no/norge/ny-_ekstremstasjon_-pa-bouvetoya-1.11525409 |archive-date=11 February 2014 |url-status=live |df=dmy-all}}</ref>
In December 2012, a new research station was sent by ship from [[Tromsø]] in Norway, via [[Cape Town]], to Bouvet.<ref>{{cite news|last=Molde|first=Eivind|date=7 February 2014|title=Ny "ekstremstasjon" på Bouvetøya|url=http://www.nrk.no/norge/ny-_ekstremstasjon_-pa-bouvetoya-1.11525409|newspaper=[[NRK]]|access-date=11 February 2014|language=no|archive-url=https://web.archive.org/web/20140211023811/http://www.nrk.no/norge/ny-_ekstremstasjon_-pa-bouvetoya-1.11525409|archive-date=11 February 2014|url-status=live}}</ref>


The robust and technically advanced station was assembled in Nyrøysa, on the north-western part of the island, the only place wide enough to land by helicopter. The elevated station is formed by three modules placed on a steel platform fixed into a concrete base. It can accommodate six people for periods of 2–4 months, and it is designed and equipped to resist rough weather conditions. The energy is supplied by wind power, which makes it easier to operate the equipment during the long periods when the station is uninhabited. The base is equipped with an automatic meteorological station that sends data via satellite throughout the year.<ref>{{cite web | url = https://www.nrk.no/norge/ny-_ekstremstasjon_-pa-bouvetoya-1.11525409 | title = Bouvetøya | website = NRK | date = 7 February 2014 | access-date = 3 April 2023}}</ref>
The robust and technically advanced station was assembled in Nyrøysa, on the north-western part of the island, the only place wide enough to land by helicopter. The elevated station is formed by three modules placed on a steel platform fixed into a concrete base. It can accommodate six people for periods of 2–4 months, and it is designed and equipped to resist rough weather conditions. The energy is supplied by wind power, which makes it easier to operate the equipment during the long periods when the station is uninhabited. The base is equipped with an automatic meteorological station that sends data via satellite throughout the year.<ref>{{cite web|url=https://www.nrk.no/norge/ny-_ekstremstasjon_-pa-bouvetoya-1.11525409|title=Bouvetøya|website=NRK|date=7 February 2014|access-date=3 April 2023}}</ref>


== Geography and geology ==
== Geography and geology ==
[[File:Bouvet Island topographic map-en.svg|thumb|upright=1.5|Bouvet Island]]
[[File:Bouvet Island topographic map-en.svg|thumb|upright=1.5|Map of Bouvet Island]]
[[File:Bouvet Island west coast glacier.jpg|thumb|upright=1.5|Glacier on Bouvet Island's west coast]]
[[File:Bouvet Island west coast glacier.jpg|thumb|upright=1.5|Glacier on Bouvet Island's west coast]]
Bouvetøya is a volcanic island constituting the top of a [[shield volcano]] just off the [[Southwest Indian Ridge]] in the South Atlantic Ocean.<ref>{{cite gvp |vn=386020 |vtab= |name=Bouvet|access-date=2021-02-05}}</ref> The island measures {{cvt|9.5|by|7|km}} and covers an area of {{cvt|49|km2}},<ref name="placenames-npolar-Bouvetøya" /> including a number of small rocks and skerries and one sizable island, [[Larsøya]].<ref name=larsoya>{{cite web |title=Larsøya |url=http://stadnamn.npolar.no/stadnamn/Lars%C3%B8ya?ident=903010&lang=en |publisher=[[Norwegian Polar Institute]] |access-date=8 May 2012 |archive-date=14 March 2013 |archive-url=https://web.archive.org/web/20130314123005/http://stadnamn.npolar.no/stadnamn/Lars%C3%B8ya?ident=903010&lang=en |url-status=live |df=dmy-all}}</ref>
Bouvetøya is a volcanic island constituting the top of a [[shield volcano]] just off the [[Southwest Indian Ridge]] in the South Atlantic Ocean.<ref>{{cite gvp|vn=386020|vtab=|name=Bouvet|access-date=2021-02-05}}</ref> The island measures {{cvt|9.5|by|7|km}} and covers an area of {{cvt|49|km2}},<ref name="placenames-npolar-Bouvetøya"/> including a number of small rocks and skerries and one sizable island, [[Larsøya]].<ref name="larsoya"/>


It is located in the Subantarctic, south of the [[Antarctic Convergence]],<ref>{{cite web |url=http://geonames.usgs.gov/pls/gnispublic/f?p=gnispq:5:::NO::P5_ANTAR_ID:488 |title=Antarctic Convergence |publisher=[[Geographic Names Information System]] |access-date=10 May 2012 |archive-date=25 May 2024 |archive-url=https://archive.today/20240525234240/https://www.webcitation.org/67YMrdClM?url=http://geonames.usgs.gov/pls/gnispublic/f%3Fp=gnispq:5:3640568296138586::NO::P5_ANTAR_ID:488 |url-status=live |df=dmy-all}}</ref> which, by some definitions, would place the island in the [[Southern Ocean]].<ref>{{cite web |url=http://www.grida.no/graphicslib/detail/the-antarctic-convergence_26e0 |title=The Antarctic convergence |publisher=[[United Nations Environment Programme]]/GRID-Arendal |date=25 February 2012 |access-date=10 May 2012 |archive-date=2 June 2012 |archive-url=https://web.archive.org/web/20120602004941/http://grida.no/graphicslib/detail/the-antarctic-convergence_26e0 |url-status=live}}</ref>
It is located in the Subantarctic, south of the [[Antarctic Convergence]],<ref>{{cite web|url=http://geonames.usgs.gov/pls/gnispublic/f?p=gnispq:5:::NO::P5_ANTAR_ID:488|title=Antarctic Convergence|publisher=[[Geographic Names Information System]]|access-date=10 May 2012|archive-date=25 May 2024|archive-url=https://archive.today/20240525234240/https://www.webcitation.org/67YMrdClM?url=http://geonames.usgs.gov/pls/gnispublic/f%3Fp=gnispq:5:3640568296138586::NO::P5_ANTAR_ID:488|url-status=live}}</ref> which, by some definitions, would place the island in the [[Southern Ocean]].<ref>{{cite web|url=http://www.grida.no/graphicslib/detail/the-antarctic-convergence_26e0|title=The Antarctic convergence|publisher=[[United Nations Environment Programme]]/GRID-Arendal|date=25 February 2012|access-date=10 May 2012|archive-date=2 June 2012|archive-url=https://web.archive.org/web/20120602004941/http://grida.no/graphicslib/detail/the-antarctic-convergence_26e0|url-status=live}}</ref>


Bouvet Island is one of the [[extreme points of Earth|most remote islands]] in the world.<ref>{{cite web |url=http://www.volcano.si.edu/world/region.cfm?rnum=18&rpage=highlights |title=Volcanology Highlights |publisher=[[Global Volcanism Program]] |access-date=11 May 2012 |url-status=dead |df=dmy-all|archive-url=https://web.archive.org/web/20120528054941/https://volcano.si.edu/world/region.cfm?rnum=18&rpage=highlights|archive-date=28 May 2012}}</ref>
Bouvet Island is one of the [[extreme points of Earth|most remote islands]] in the world.<ref>{{cite web|url=http://www.volcano.si.edu/world/region.cfm?rnum=18&rpage=highlights|title=Volcanology Highlights|publisher=[[Global Volcanism Program]]|access-date=11 May 2012|url-status=dead|archive-url=https://web.archive.org/web/20120528054941/https://volcano.si.edu/world/region.cfm?rnum=18&rpage=highlights|archive-date=28 May 2012}}</ref>
The closest land is [[Queen Maud Land]] of Antarctica, which is {{cvt|1700|km}} to the south,<ref name="Barr-1987" />{{rp|page=58}} and [[Gough Island]], {{cvt|1845|km}} to the north.<ref name=npolar>{{cite web |url=http://www.npolar.no/no/antarktis/bouvetoya.html |title=Bouvetøya |publisher=[[Norwegian Polar Institute]] |access-date=10 May 2012 |archive-date=15 April 2012 |archive-url=https://web.archive.org/web/20120415125957/http://www.npolar.no/no/antarktis/bouvetoya.html |url-status=dead |df=dmy}}</ref> The closest inhabited location is [[Tristan da Cunha]] island, {{cvt|2250|km}} to the northwest.<ref name="placenames-npolar-Bouvetøya" /> To its west, the [[South Sandwich Islands]] lie about {{cvt|1900|km|mi}} away, and to its east are the [[Prince Edward Islands]], about {{cvt|2500|km|mi}} away.{{Citation needed|date=October 2023}}
The closest land is [[Queen Maud Land]] of Antarctica, which is {{cvt|1700|km}} to the south,<ref name="Barr-1987"/>{{rp|page=58}} and [[Gough Island]], {{cvt|1845|km}} to the north.<ref name="npolar"/> The closest inhabited location is [[Tristan da Cunha]] island, {{cvt|2250|km}} to the northwest.<ref name="placenames-npolar-Bouvetøya"/> To its west, the [[South Sandwich Islands]] lie about {{cvt|1900|km|mi}} away, and to its east are the [[Prince Edward Islands]], about {{cvt|2500|km|mi}} away.{{Citation needed|date=October 2023}}


Nyrøysa is a {{cvt|2|by|0.5|km|adj=on|1}} terrace located on the north-west coast of the island. Created by a [[rock slide]] sometime between 1955 and 1957, it is the island's easiest access point.<ref name="Barr-1987" />{{rp|page=59}} It is the site of the automatic weather station.<ref name="Hyser-Bouvetøya-birdlife" /> The north-west corner is the peninsula of [[Cape Circoncision]].<ref>{{cite web |title=Kapp Circoncision |url=http://stadnamn.npolar.no/stadnamn/Bennskjera?ident=902575&lang=en |publisher=[[Norwegian Polar Institute]] |access-date=11 May 2012 |archive-date=3 June 2016 |archive-url=https://web.archive.org/web/20160603154137/http://stadnamn.npolar.no/stadnamn/Kapp+Circoncision?ident=901077&lang=en |url-status=live |df=dmy-all}}</ref> From there, east to [[Cape Valdivia]], the coast is known as Morgenstiernekysten.<ref>{{cite web |title=Kapp Valdivia |url=http://stadnamn.npolar.no/stadnamn/Kapp+Valdivia?ident=901087&lang=en |publisher=[[Norwegian Polar Institute]] |access-date=11 May 2012 |archive-date=14 March 2013 |archive-url=https://web.archive.org/web/20130314122940/http://stadnamn.npolar.no/stadnamn/Kapp+Valdivia?ident=901087&lang=en |url-status=live |df=dmy-all}}</ref>
Nyrøysa is a {{cvt|2|by|0.5|km|adj=on|1}} terrace located on the north-west coast of the island. Created by a [[rock slide]] sometime between 1955 and 1957, it is the island's easiest access point.<ref name="Barr-1987"/>{{rp|page=59}} It is the site of the automatic weather station.<ref name="Hyser-Bouvetøya-birdlife"/> The north-west corner is the peninsula of [[Cape Circoncision]].<ref>{{cite web|title=Kapp Circoncision|url=http://stadnamn.npolar.no/stadnamn/Bennskjera?ident=902575&lang=en|publisher=[[Norwegian Polar Institute]]|access-date=11 May 2012|archive-date=3 June 2016|archive-url=https://web.archive.org/web/20160603154137/http://stadnamn.npolar.no/stadnamn/Kapp+Circoncision?ident=901077&lang=en|url-status=live}}</ref> From there, east to [[Cape Valdivia]], the coast is known as Morgenstiernekysten.<ref>{{cite web|title=Kapp Valdivia|url=http://stadnamn.npolar.no/stadnamn/Kapp+Valdivia?ident=901087&lang=en|publisher=[[Norwegian Polar Institute]]|access-date=11 May 2012|archive-date=14 March 2013|archive-url=https://web.archive.org/web/20130314122940/http://stadnamn.npolar.no/stadnamn/Kapp+Valdivia?ident=901087&lang=en|url-status=live}}</ref>


[[Store Kari Rock|Store Kari]] is an islet located {{cvt|1.2|km}} east of the cape.<ref>{{cite web |title=Store-Kari |url=http://stadeumn.npolar.no/stadnamn/Store-Kari?ident=902130&lang=en |publisher=[[Norwegian Polar Institute]] |access-date=11 May 2012 |archive-date=16 July 2012 |archive-url=https://archive.today/20120716222224/http://stadnamn.npolar.no/stadnamn/Store-Kari?ident=902130&lang=en |url-status=dead |df=dmy-all}}</ref> From Kapp Valdivia, southeast to [[Kapp Lollo]], on the east side of the island, the coast is known as Victoria Terrasse.<ref>{{cite web |title=Kapp Lollo |url=http://stadnamn.npolar.no/stadnamn/Kapp+Lollo?ident=901082&lang=en |publisher=[[Norwegian Polar Institute]] |access-date=11 May 2012 |archive-date=14 March 2013 |archive-url=https://web.archive.org/web/20130314122933/http://stadnamn.npolar.no/stadnamn/Kapp+Lollo?ident=901082&lang=en |url-status=live |df=dmy-all}}</ref> From there to [[Kapp Fie]] at the southeastern corner, the coast is known as [[Mowinckelkysten]]. Svartstranda is a section of [[black sand]] which runs {{cvt|1.8|km}} along the section from [[Cape Meteor|Kapp Meteor]], south to Kapp Fie.<ref>{{cite web |title=Svartstranda |url=http://stadnamn.npolar.no/stadnamn/Svartstranda?ident=902185&lang=en |publisher=[[Norwegian Polar Institute]] |access-date=11 May 2012 |archive-date=14 March 2013 |archive-url=https://web.archive.org/web/20130314122933/http://stadnamn.npolar.no/stadnamn/Kapp+Lollo?ident=901082&lang=en |url-status=live |df=dmy-all}}</ref>
[[Store Kari Rock|Store Kari]] is an islet located {{cvt|1.2|km}} east of the cape.<ref>{{cite web|title=Store-Kari|url=http://stadeumn.npolar.no/stadnamn/Store-Kari?ident=902130&lang=en|publisher=[[Norwegian Polar Institute]]|access-date=11 May 2012|archive-date=16 July 2012|archive-url=https://archive.today/20120716222224/http://stadnamn.npolar.no/stadnamn/Store-Kari?ident=902130&lang=en|url-status=dead}}</ref> From Cape Valdivia, southeast to [[Cape Lollo]], on the east side of the island, the coast is known as Victoria Terrasse.<ref>{{cite web|title=Kapp Lollo|url=http://stadnamn.npolar.no/stadnamn/Kapp+Lollo?ident=901082&lang=en|publisher=[[Norwegian Polar Institute]]|access-date=11 May 2012|archive-date=14 March 2013|archive-url=https://web.archive.org/web/20130314122933/http://stadnamn.npolar.no/stadnamn/Kapp+Lollo?ident=901082&lang=en|url-status=live}}</ref> From there to [[Cape Fie]] at the southeastern corner, the coast is known as [[Mowinckelkysten]]. Svartstranda is a section of [[black sand]] which runs {{cvt|1.8|km}} along the section from [[Cape Meteor]], south to Cape Fie.<ref>{{cite web|title=Svartstranda|url=http://stadnamn.npolar.no/stadnamn/Svartstranda?ident=902185&lang=en|publisher=[[Norwegian Polar Institute]]|access-date=11 May 2012|archive-date=14 March 2013|archive-url=https://web.archive.org/web/20130314122933/http://stadnamn.npolar.no/stadnamn/Kapp+Lollo?ident=901082&lang=en|url-status=live}}</ref>


After rounding Kapp Fie, the coast along the south side is known as Vogtkysten.<ref>{{cite web |title=Vogtkysten |url=http://stadnamn.npolar.no/stadnamn/Svartstranda?ident=902185&lang=en |publisher=[[Norwegian Polar Institute]] |access-date=11 May 2012 |archive-date=14 March 2013 |archive-url=https://web.archive.org/web/20130314122945/http://stadnamn.npolar.no/stadnamn/Vogtkysten?ident=902470&lang=en |url-status=live |df=dmy-all}}</ref> The westernmost part of it is the {{cvt|300|m}} long shore of Sjøelefantstranda.<ref>{{cite web |title=Sjøelefantstranda |url=http://stadnamn.npolar.no/stadnamn/Sj%C3%B8elefantstranda?ident=901938&lang=en |publisher=[[Norwegian Polar Institute]] |access-date=11 May 2012 |archive-date=14 March 2013 |archive-url=https://web.archive.org/web/20130314122952/http://stadnamn.npolar.no/stadnamn/Sj%C3%B8elefantstranda?ident=901938&lang=en |url-status=live |df=dmy-all}}</ref>
After rounding Cape Fie, the coast along the south side is known as Vogtkysten.<ref>{{cite web|title=Vogtkysten|url=http://stadnamn.npolar.no/stadnamn/Svartstranda?ident=902185&lang=en|publisher=[[Norwegian Polar Institute]]|access-date=11 May 2012|archive-date=14 March 2013|archive-url=https://web.archive.org/web/20130314122945/http://stadnamn.npolar.no/stadnamn/Vogtkysten?ident=902470&lang=en|url-status=live}}</ref> The westernmost part of it is the {{cvt|300|m}} long shore of Sjøelefantstranda.<ref>{{cite web|title=Sjøelefantstranda|url=http://stadnamn.npolar.no/stadnamn/Sj%C3%B8elefantstranda?ident=901938&lang=en|publisher=[[Norwegian Polar Institute]]|access-date=11 May 2012|archive-date=14 March 2013|archive-url=https://web.archive.org/web/20130314122952/http://stadnamn.npolar.no/stadnamn/Sj%C3%B8elefantstranda?ident=901938&lang=en|url-status=live}}</ref>


Off Catoodden, on the south-western corner, lies [[Larsøya]], the only island of any size off Bouvetøya.<ref name=larsoya /> The western coast from Catoodden north to Nyrøysa, is known as Esmarchkysten. Midway up the coast lies Norvegiaodden (Kapp Norvegia)<ref>{{cite web |title=Norvegiaodden |url=http://stadnamn.npolar.no/stadnamn/Vogtkysten?ident=902470&lang=en |publisher=[[Norwegian Polar Institute]] |access-date=11 May 2012 |archive-date=25 May 2024 |archive-url=https://archive.today/20240525234640/https://www.webcitation.org/67aMdkwEq?url=http://stadnamn.npolar.no/stadnamn/Norvegiaodden%3Fident=901511&lang=en |url-status=live |df=dmy-all}}</ref> and {{cvt|0.5|km}} off it the skerries of Bennskjæra.<ref>{{cite web |title=Bennskjæra |url=http://stadnamn.npolar.no/stadnamn/Bennskjera?ident=902575&lang=en |publisher=[[Norwegian Polar Institute]] |access-date=11 May 2012 |archive-date=14 March 2013 |archive-url=https://web.archive.org/web/20130314123011/http://stadnamn.npolar.no/stadnamn/Bennskjera?ident=902575&lang=en |url-status=live |df=dmy-all}}</ref>
Off Catoodden, on the south-western corner, lies [[Larsøya]], the only island of any size off Bouvetøya.<ref name="larsoya"/> The western coast from Catoodden north to Nyrøysa, is known as Esmarchkysten. Midway up the coast lies Norvegiaodden ([[Cape Norvegia]])<ref>{{cite web|title=Norvegiaodden|url=http://stadnamn.npolar.no/stadnamn/Vogtkysten?ident=902470&lang=en|publisher=[[Norwegian Polar Institute]]|access-date=11 May 2012|archive-date=25 May 2024|archive-url=https://archive.today/20240525234640/https://www.webcitation.org/67aMdkwEq?url=http://stadnamn.npolar.no/stadnamn/Norvegiaodden%3Fident=901511&lang=en|url-status=live}}</ref> and {{cvt|0.5|km}} off it the skerries of Bennskjæra.<ref>{{cite web|title=Bennskjæra|url=http://stadnamn.npolar.no/stadnamn/Bennskjera?ident=902575&lang=en|publisher=[[Norwegian Polar Institute]]|access-date=11 May 2012|archive-date=14 March 2013|archive-url=https://web.archive.org/web/20130314123011/http://stadnamn.npolar.no/stadnamn/Bennskjera?ident=902575&lang=en|url-status=live}}</ref>


Ninety-three percent of the island is covered by [[glacier]]s, giving it a domed shape.<ref name="Barr-1987" />{{rp|page=59}} The summit region of the island is Wilhelmplatået, slightly to the west of the island's center.<ref name="Baker-1967" /> The [[plateau]] is {{cvt|3.5|km}} across<ref name="SI-Volcanism-Bouvet" /> and surrounded by several peaks.<ref name="Baker-1967" /> The tallest is [[Olavtoppen]], {{cvt|780|m}} [[above mean sea level]] (AMSL),<ref name="Barr-1987" />{{rp|page=59}} followed by [[Lykketoppen]] ({{cvt|766|m|disp=or}} AMSL)<ref>{{cite web |url=http://geonames.usgs.gov/pls/gnispublic/f?p=gnispq:5:::NO::P5_ANTAR_ID:9163 |title=Lykke Peak |publisher=[[Geographic Names Information System]] |access-date=12 May 2012 |archive-date=25 May 2024 |archive-url=https://archive.today/20240525234802/https://www.webcitation.org/67bIa4cd7?url=http://geonames.usgs.gov/pls/gnispublic/f%3Fp=gnispq:5:1080405097172969::NO::P5_ANTAR_ID:9163 |url-status=live |df=dmy-all}}</ref> and [[Mosbytoppane]] ({{cvt|670|m|disp=or}} AMSL).<ref>{{cite web |url=http://geonames.usgs.gov/pls/gnispublic/f?p=gnispq:5:::NO::P5_ANTAR_ID:10304 |title=Mosby Peak |publisher=[[Geographic Names Information System]] |access-date=12 May 2012 |archive-date=25 May 2024 |archive-url=https://archive.today/20240525234841/https://www.webcitation.org/67bIfeYqD?url=http://geonames.usgs.gov/pls/gnispublic/f%3Fp=gnispq:5:3949913289827917::NO::P5_ANTAR_ID:10304 |url-status=live |df=dmy-all}}</ref> Below Wilhelmplatået is the main [[caldera]] responsible for creating the island.<ref name="Baker-1967" /> The last [[eruption]] took place 2000&nbsp;BCE, producing a [[lava]] flow at Kapp Meteor.<ref name="SI-Volcanism-Bouvet" /> The volcano is presumed to be in a declining state.<ref name="Baker-1967" /> The temperature {{cvt|30|cm}} below the surface is {{cvt|25|C}}.<ref name="Barr-1987" />{{rp|page=59}}
Ninety-three percent of the island is covered by [[glacier]]s, giving it a domed shape.<ref name="Barr-1987"/>{{rp|page=59}} The summit region of the island is Wilhelmplatået, slightly to the west of the island's centre.<ref name="Baker-1967"/> The [[plateau]] is {{cvt|3.5|km}} across<ref name="SI-Volcanism-Bouvet"/> and surrounded by several peaks.<ref name="Baker-1967"/> The tallest is [[Olavtoppen]], {{cvt|780|m}} [[above mean sea level]] (AMSL),<ref name="Barr-1987"/>{{rp|page=59}} followed by [[Lykketoppen]] ({{cvt|766|m|disp=or}} AMSL)<ref>{{cite web|url=http://geonames.usgs.gov/pls/gnispublic/f?p=gnispq:5:::NO::P5_ANTAR_ID:9163|title=Lykke Peak|publisher=[[Geographic Names Information System]]|access-date=12 May 2012|archive-date=25 May 2024|archive-url=https://archive.today/20240525234802/https://www.webcitation.org/67bIa4cd7?url=http://geonames.usgs.gov/pls/gnispublic/f%3Fp=gnispq:5:1080405097172969::NO::P5_ANTAR_ID:9163|url-status=live}}</ref> and [[Mosbytoppane]] ({{cvt|670|m|disp=or}} AMSL).<ref>{{cite web|url=http://geonames.usgs.gov/pls/gnispublic/f?p=gnispq:5:::NO::P5_ANTAR_ID:10304|title=Mosby Peak|publisher=[[Geographic Names Information System]]|access-date=12 May 2012|archive-date=25 May 2024|archive-url=https://archive.today/20240525234841/https://www.webcitation.org/67bIfeYqD?url=http://geonames.usgs.gov/pls/gnispublic/f%3Fp=gnispq:5:3949913289827917::NO::P5_ANTAR_ID:10304|url-status=live}}</ref> Below Wilhelmplatået is the main [[caldera]] responsible for creating the island.<ref name="Baker-1967"/> The last [[eruption]] took place circa 2000&nbsp;BCE, producing a [[lava]] flow at Cape Meteor.<ref name="SI-Volcanism-Bouvet"/> The volcano is presumed to be in a declining state.<ref name="Baker-1967"/> The temperature {{cvt|30|cm}} below the surface is {{cvt|25|C}}.<ref name="Barr-1987"/>{{rp|page=59}}


The island's total coastline is {{cvt|29.6|km}}.<ref name=factbook>{{cite web |url=https://www.cia.gov/the-world-factbook/countries/bouvet-island/ |title=Bouvet Island |work=[[The World Factbook]] |publisher=[[Central Intelligence Agency]] |access-date=9 May 2012 |df=dmy-all}}</ref> Landing on the island is very difficult, as it normally experiences high seas and features a [[steep coast]].<ref name="Barr-1987" />{{rp|page=59}} During the winter, it is surrounded by [[pack ice]].<ref name="placenames-npolar-Bouvetøya" /> The [[Bouvet Triple Junction]] is located {{cvt|275|km}} west of Bouvet Island. It is a [[triple junction]] between the [[South American Plate]], the [[African Plate]] and the [[Antarctic Plate]], and of the Mid-Atlantic Ridge, the Southwest Indian Ridge and the [[American–Antarctic Ridge]].<ref name="Mitchell-Livermore-etal-2000" />
The island's total coastline is {{cvt|29.6|km}}.<ref name="factbook"/> Landing on the island is very difficult, as it normally experiences high seas and features a [[steep coast]].<ref name="Barr-1987"/>{{rp|page=59}} During the winter, it is surrounded by [[pack ice]].<ref name="placenames-npolar-Bouvetøya"/> The [[Bouvet triple junction]] is located {{cvt|275|km}} west of Bouvet Island. It is a [[triple junction]] between the [[South American plate]], the [[African plate]] and the [[Antarctic plate]], and of the [[Mid-Atlantic Ridge]], the [[Southwest Indian Ridge]] and the [[American–Antarctic Ridge]].<ref name="Mitchell-Livermore-etal-2000"/>
{{Panorama |image=File:Bouvet Island west coast.jpg |height=200 |alt= |caption=West coast of Bouvet Island}}
{{Panorama |image=File:Bouvet Island west coast.jpg |height=200 |alt= |caption=A view of the west coast of Bouvet Island}}


== Climate ==
== Climate ==
The island is located south of the [[Antarctic Convergence]], giving it a marine [[Antarctic climate]] dominated by heavy clouds and fog. It experiences a mean temperature of {{cvt|−1|C}},<ref name="Barr-1987" />{{rp|page=59}} with January average of {{cvt|1|C}} and September average of {{cvt|−3|C}}.<ref name="npolar" /> The monthly high mean temperatures fluctuate little through the year.<ref name="Climate-Zone-bouvet-island" /> The peak temperature of {{cvt|14|C}} was recorded in March&nbsp;1980, caused by intense sun radiation. Spot temperatures as high as {{cvt|20|C}} have been recorded in sunny weather on rock faces.<ref name="Barr-1987" />{{rp|page=59}} The island predominantly experiences a weak [[west wind]].<ref name="npolar" /> In spite of these severe climate conditions, Bouvet Island actually is located four degrees of latitude closer to the equator than the southernmost tip of Norway, which is located at 58°N. Its latitude – by analogy to Scandinavia – is instead similar to southern [[Denmark]].{{Citation needed|date=October 2023}}
The island is located south of the [[Antarctic Convergence]], giving it a marine [[Antarctic climate]] dominated by heavy clouds and fog. It experiences a mean temperature of {{cvt|−1|C}},<ref name="Barr-1987"/>{{rp|page=59}} with January average of {{cvt|1|C}} and September average of {{cvt|−3|C}}.<ref name="npolar"/> The monthly high mean temperatures fluctuate little through the year.<ref name="Climate-Zone-bouvet-island"/> The peak temperature of {{cvt|14|C}} was recorded in March&nbsp;1980, caused by intense sun radiation. Spot temperatures as high as {{cvt|20|C}} have been recorded in sunny weather on rock faces.<ref name="Barr-1987"/>{{rp|page=59}} The island predominantly experiences a weak [[west wind]].<ref name="npolar"/>
{{Weather box
{{Weather box
|location = Bouvet Island
|location = Bouvet Island
Line 291: Line 293:
|Dec sun =
|Dec sun =
|year sun =
|year sun =
|source 1= Météo climat stats (Norvege)<ref name="Météo-climat-Norvege" />
|source 1= Météo climat stats (Norvege)<ref name="Météo-climat-Norvege"/>
|source 2= Météo Climat stats (Isl. Bouvet)<ref name="Météo-climat-Bouvet" />
|source 2= Météo Climat stats (Isl. Bouvet)<ref name="Météo-climat-Bouvet"/>
}}
}}


== Nature ==
== Nature ==
[[File:Bouvet aerial photo.jpg|thumb|upright=1.3|[[NASA]] image of Bouvet Island from space]]
[[File:Bouvet aerial photo.jpg|thumb|upright=1.3|[[NASA]] image of Bouvet Island from space]]
The harsh climate and ice-bound terrain limits non-animal life to [[fungi]] ([[ascomycetes]] including symbiotic [[lichens]]) and [[non-vascular plant]]s ([[mosses]] and [[liverworts]]). The flora are representative for the maritime Antarctic and are [[phytogeographically]] similar to those of the [[South Sandwich Islands]] and [[South Shetland Islands]]. Vegetation is limited because of the ice cover, although [[snow algae]] are recorded. The remaining vegetation is located in snow-free areas such as [[nunatak]] ridges and other parts of the summit plateau, the coastal cliffs, capes and beaches. At Nyrøysa, five species of moss, six ascomycetes (including five lichens), and twenty algae have been recorded. Most snow-free areas are so steep and subject to frequent [[avalanche]]s that only [[crustose]] lichens and algal formations are sustainable. There are six [[endemic]] ascomycetes, three of which are lichenized.<ref name="Hyser-Bouvetøya-birdlife" />
The harsh climate and ice-bound terrain limits non-animal life to [[fungi]] ([[ascomycetes]] including symbiotic [[lichens]]) and [[non-vascular plant]]s ([[mosses]] and [[liverworts]]). The flora are representative for the maritime Antarctic and are [[phytogeographically]] similar to those of the [[South Sandwich Islands]] and [[South Shetland Islands]]. Vegetation is limited because of the ice cover, although [[snow algae]] are recorded. The remaining vegetation is located in snow-free areas such as [[nunatak]] ridges and other parts of the summit plateau, the coastal cliffs, capes and beaches. At Nyrøysa, five species of moss, six ascomycetes (including five lichens), and twenty algae have been recorded. Most snow-free areas are so steep and subject to frequent [[avalanche]]s that only [[crustose]] lichens and algal formations are sustainable. There are six [[endemic]] ascomycetes, three of which are lichenized.<ref name="Hyser-Bouvetøya-birdlife"/>


[[File:Bouvet island.jpg|thumb|upright=1.3|left|[[Cape Valdivia]], the northernmost point of Bouvet Island, in 2009]]
[[File:Bouvet island.jpg|thumb|upright=1.3|[[Cape Valdivia]], the northernmost point of Bouvet Island, in 2009]]
The island has been designated as an [[Important Bird Area]] by [[BirdLife International]] because of its importance as a [[breeding ground]] for [[seabird]]s. In 1978–1979 there were an estimated 117,000 breeding [[penguins]] on the island, consisting of [[macaroni penguin]]<!--Eudyptes chrysolophus--> and, to a lesser extent, [[chinstrap penguin]]<!--Pygoscelis antarctica--> and [[Adélie penguin]]<!--Pygoscelis adeliae-->, although these were only estimated to be 62,000 in 1989–1990. Nyrøysa is the most important [[bird colony|colony]] for penguins, supplemented by Posadowskybreen, Kapp Circoncision, Norvegiaodden and across from Larsøya. [[Southern fulmar]]<!--Fulmarus glacialoides--> is by far the most common non-penguin bird with 100,000&nbsp;individuals. Other breeding seabirds consist of [[Cape petrel]]<!--Daption capense-->, [[Antarctic prion]]<!--Pachyptila desolata-->, [[Wilson's storm petrel]]<!--Oceanites oceanicus-->, [[black-bellied storm petrel]]<!--Fregetta tropica-->, [[subantarctic skua]]<!--Catharacta antarctica lonnbergi-->, [[southern giant petrel]]<!--Macronectes giganteus-->, [[snow petrel]]<!--Pagodroma nivea-->, [[slender-billed prion]]<!--Pachyptila belcheri--> and [[Antarctic tern]]<!--Sterna vittata-->. [[Kelp gull]]<!--Larus dominicanus--> is thought to have bred on the island earlier. Non-breeding birds which can be found on the island include the [[king penguin]], [[wandering albatross]], [[black-browed albatross]], [[Campbell albatross]], [[Atlantic yellow-nosed albatross]], [[sooty albatross]], [[light-mantled albatross]], [[northern giant petrel]], [[Antarctic petrel]], [[blue petrel]], [[soft-plumaged petrel]], [[Kerguelen petrel]], [[white-headed petrel]], [[fairy prion]], [[white-chinned petrel]], [[great shearwater]], [[common diving petrel]], [[south polar skua]] and [[parasitic jaeger]].<ref name="Hyser-Bouvetøya-birdlife" />
The island has been designated as an [[Important Bird Area]] by [[BirdLife International]] because of its importance as a [[breeding ground]] for [[seabird]]s. In 1978–1979 there were an estimated 117,000 breeding [[penguins]] on the island, consisting of [[macaroni penguin]]<!--Eudyptes chrysolophus--> and, to a lesser extent, [[chinstrap penguin]]<!--Pygoscelis antarctica--> and [[Adélie penguin]]<!--Pygoscelis adeliae-->, although these were only estimated to be 62,000 in 1989–1990. Nyrøysa is the most important [[bird colony|colony]] for penguins, supplemented by Posadowskybreen, Kapp Circoncision, Norvegiaodden and across from Larsøya. [[Southern fulmar]]<!--Fulmarus glacialoides--> is by far the most common non-penguin bird with 100,000&nbsp;individuals. Other breeding seabirds consist of [[Cape petrel]]<!--Daption capense-->, [[Antarctic prion]]<!--Pachyptila desolata-->, [[Wilson's storm petrel]]<!--Oceanites oceanicus-->, [[black-bellied storm petrel]]<!--Fregetta tropica-->, [[subantarctic skua]]<!--Catharacta antarctica lonnbergi-->, [[southern giant petrel]]<!--Macronectes giganteus-->, [[snow petrel]]<!--Pagodroma nivea-->, [[slender-billed prion]]<!--Pachyptila belcheri--> and [[Antarctic tern]]<!--Sterna vittata-->. [[Kelp gull]]<!--Larus dominicanus--> is thought to have bred on the island earlier. Non-breeding birds which can be found on the island include the [[king penguin]], [[wandering albatross]], [[black-browed albatross]], [[Campbell albatross]], [[Atlantic yellow-nosed albatross]], [[sooty albatross]], [[light-mantled albatross]], [[northern giant petrel]], [[Antarctic petrel]], [[blue petrel]], [[soft-plumaged petrel]], [[Kerguelen petrel]], [[white-headed petrel]], [[fairy prion]], [[white-chinned petrel]], [[great shearwater]], [[common diving petrel]], [[south polar skua]] and [[parasitic jaeger]].<ref name="Hyser-Bouvetøya-birdlife"/>


The only non-bird [[vertebrate]]s on the island are [[pinniped|seals]], specifically the [[southern elephant seal]] and [[Antarctic fur seal]], which breed on the island. In 1998–1999, there were 88 elephant seal pups and 13,000&nbsp;fur seal pups at Nyrøysa. [[Southern right whale]], [[humpback whale]], [[fin whale]], [[southern right whale dolphin]], [[hourglass dolphin]], and [[killer whale]] are seen in the surrounding waters.<ref>{{Cite journal |url=https://doi.org/10.1093/jhered/esaa010 |title=Genetic Diversity and Connectivity of Southern Right Whales (Eubalaena australis) Found in the Brazil and Chile–Peru Wintering Grounds and the South Georgia (Islas Georgias del Sur) Feeding Ground |first1=Emma L |last1=Carroll |first2=Paulo H |last2=Ott |first3=Louise F |last3=McMillan |first4=Bárbara |last4=Galletti Vernazzani |first5=Petra |last5=Neveceralova |first6=Els |last6=Vermeulen |first7=Oscar E |last7=Gaggiotti |first8=Artur |last8=Andriolo |first9=C Scott |last9=Baker|first10=Connor|last10=Bamford |first11=Peter |last11=Best |first12=Elsa |last12=Cabrera |first13=Susannah |last13=Calderan |first14=Andrea |last14=Chirife |first15=Rachel M |last15=Fewster |first16=Paulo A C |last16=Flores |first17=Timothy |last17=Frasier |first18=Thales R O |last18=Freitas |first19=Karina |last19=Groch|first20=Pavel|last20=Hulva |first21=Amy |last21=Kennedy |first22=Russell |last22=Leaper |first23=Matthew S |last23=Leslie |first24=Michael |last24=Moore |first25=Larissa |last25=Oliveira |first26=Jon |last26=Seger |first27=Emilie N |last27=Stepien |first28=Luciano O |last28=Valenzuela |first29=Alexandre |last29=Zerbini|first30=Jennifer A|last30=Jackson |date=20 May 2020 |journal=Journal of Heredity |volume=111 |issue=3 |pages=263–276 |via=Silverchair |doi=10.1093/jhered/esaa010 |pmid=32347944 |pmc=7238439}}</ref><ref name="Hyser-Bouvetøya-birdlife" /><ref>{{Cite web |url=https://litografa.wixsite.com/artiolaphotographer/whales |title=Whales |website=artiolaphotographer}}</ref><ref>{{cite web |title=The Bouvet Island Atlantic Odyssey |url=https://www.nhm.uio.no/fakta/zoologi/fugl/ringmerking/PDF/Bouvet_Atlantic.pdf |website=Oceanwide Expeditions |access-date=23 August 2021}}</ref>
The only non-bird [[vertebrate]]s on the island are [[pinniped|seals]], specifically the [[southern elephant seal]] and [[Antarctic fur seal]], which breed on the island. In 1998–1999, there were 88 elephant seal pups and 13,000&nbsp;fur seal pups at Nyrøysa. [[Southern right whale]], [[humpback whale]], [[fin whale]], [[southern right whale dolphin]], [[hourglass dolphin]], and [[orca]] are seen in the surrounding waters.<ref>{{Cite journal|url=https://doi.org/10.1093/jhered/esaa010|title=Genetic Diversity and Connectivity of Southern Right Whales (Eubalaena australis) Found in the Brazil and Chile–Peru Wintering Grounds and the South Georgia (Islas Georgias del Sur) Feeding Ground|first1=Emma L|last1=Carroll|first2=Paulo H|last2=Ott|first3=Louise F|last3=McMillan|first4=Bárbara|last4=Galletti Vernazzani|first5=Petra|last5=Neveceralova|first6=Els|last6=Vermeulen|first7=Oscar E|last7=Gaggiotti|first8=Artur|last8=Andriolo|first9=C Scott|last9=Baker|first10=Connor|last10=Bamford|first11=Peter|last11=Best|first12=Elsa|last12=Cabrera|first13=Susannah|last13=Calderan|first14=Andrea|last14=Chirife|first15=Rachel M|last15=Fewster|first16=Paulo A C|last16=Flores|first17=Timothy|last17=Frasier|first18=Thales R O|last18=Freitas|first19=Karina|last19=Groch|first20=Pavel|last20=Hulva|first21=Amy|last21=Kennedy|first22=Russell|last22=Leaper|first23=Matthew S|last23=Leslie|first24=Michael|last24=Moore|first25=Larissa|last25=Oliveira|first26=Jon|last26=Seger|first27=Emilie N|last27=Stepien|first28=Luciano O|last28=Valenzuela|first29=Alexandre|last29=Zerbini|first30=Jennifer A|last30=Jackson|date=20 May 2020|journal=Journal of Heredity|volume=111|issue=3|pages=263–276|via=Silverchair|doi=10.1093/jhered/esaa010|pmid=32347944|pmc=7238439}}</ref><ref name="Hyser-Bouvetøya-birdlife"/><ref>{{Cite web|url=https://litografa.wixsite.com/artiolaphotographer/whales|title=Whales|website=artiolaphotographer}}</ref><ref>{{cite web|title=The Bouvet Island Atlantic Odyssey|url=https://www.nhm.uio.no/fakta/zoologi/fugl/ringmerking/PDF/Bouvet_Atlantic.pdf|website=Oceanwide Expeditions|access-date=23 August 2021}}</ref>


== Politics and government ==
== Politics and government ==
[[File:Bouvet Island ISS017-E-16161 no text (cropped).JPG|thumb|Image courtesy of the Image Science & Analysis Laboratory, NASA Johnson Space Center]]
[[File:Bouvet Island ISS017-E-16161 no text (cropped).JPG|thumb|Image courtesy of the Image Science & Analysis Laboratory, NASA Johnson Space Center]]
[[File:Nils Olav wide.jpg|thumb|[[Nils Olav]], Baron of the Bouvet Islands]]
Bouvetøya is one of three dependencies of Norway.<ref name="Gisle-1999" /> Unlike [[Peter I Island]] and [[Queen Maud Land]], which are subject to the [[Antarctic Treaty System]],<ref name="Barr-1987" />{{rp|page=65}} Bouvetøya is not disputed.<ref name="factbook" /> The dependency status entails that the island is not part of the Kingdom of Norway, but is still under Norwegian [[sovereignty]]. This implies that the island can be [[cede]]d without violating the first article of the [[Constitution of Norway]].<ref name="Gisle-1999" /> Norwegian administration of the island is handled by the Polar Affairs Department of the [[Ministry of Justice and the Police (Norway)|Ministry of Justice and the Police]], located in [[Oslo]].<ref>{{cite web |title=Polar Affairs Department |url=http://www.regjeringen.no/en/dep/jd/About-the-Ministry-of-Justice-and-the-Po/Organization/Departments/The-Polar-Affairs-Department.html?id=1447 |publisher=[[Norwegian Ministry of the Environment]] |access-date=29 August 2011 |archive-date=8 August 2011 |url-status=dead |archive-url=https://web.archive.org/web/20110808221333/http://www.regjeringen.no/en/dep/jd/About-the-Ministry-of-Justice-and-the-Po/Organization/Departments/The-Polar-Affairs-Department.html?id=1447 |df=dmy-all}}</ref>


Bouvetøya is one of three dependencies of Norway.<ref name="Gisle-1999"/> Unlike [[Peter I Island]] and [[Queen Maud Land]], which are subject to the [[Antarctic Treaty System]],<ref name="Barr-1987"/>{{rp|page=65}} Bouvetøya is not disputed.<ref name="factbook"/> The dependency status entails that the island is not part of the Kingdom of Norway, but is still under Norwegian [[sovereignty]]. This implies that the island can be [[cede]]d without violating the first article of the [[Constitution of Norway]].<ref name="Gisle-1999"/> Norwegian administration of the island is handled by the Polar Affairs Department of the [[Ministry of Justice and the Police (Norway)|Ministry of Justice and the Police]], located in [[Oslo]].<ref>{{cite web|title=Polar Affairs Department|url=http://www.regjeringen.no/en/dep/jd/About-the-Ministry-of-Justice-and-the-Po/Organization/Departments/The-Polar-Affairs-Department.html?id=1447|publisher=[[Norwegian Ministry of the Environment]]|access-date=29 August 2011|archive-date=8 August 2011|url-status=dead|archive-url=https://web.archive.org/web/20110808221333/http://www.regjeringen.no/en/dep/jd/About-the-Ministry-of-Justice-and-the-Po/Organization/Departments/The-Polar-Affairs-Department.html?id=1447}}</ref>
The annexation of the island is regulated by the Dependency Act of 24&nbsp;March 1933. It establishes that Norwegian [[criminal law]], [[private law]] and [[procedural law]] apply to the island, in addition to other laws that explicitly state they are valid on the island. It further establishes that all land belongs to the state, and prohibits the storage and detonation of nuclear products.<ref name="LOV19300227" />


The annexation of the island is regulated by the Dependency Act of 24&nbsp;March 1933. It establishes that Norwegian [[criminal law]], [[private law]] and [[procedural law]] apply to the island, in addition to other laws that explicitly state they are valid on the island. It further establishes that all land belongs to the state, and prohibits the storage and detonation of nuclear products.<ref name="LOV19300227"/>
Bouvet Island has been designated with the [[ISO 3166-2]] code [[ISO 3166-2:BV|BV]]<ref>{{cite web |url=http://www.unece.org/stats/documents/1998/03/migration/5.e.pdf |title=Country classifications in migration statistics – present situation and proposals for a Eurostat standard |last1=Takle |first1=Mona Takle |first2=Kåre |last2=Vassenden |publisher=[[United Nations Statistical Commission]] and [[United Nations Economic Commission for Europe]] |date=March 1998 |access-date=26 January 2011 |archive-url=https://web.archive.org/web/20150713215624/http://www.unece.org/fileadmin/DAM/stats/documents/1998/03/migration/5.e.pdf |archive-date=13 July 2015 |url-status=live |df=dmy-all}}</ref> and was subsequently awarded the [[country code]] [[top-level domain]] [[.bv]] on 21&nbsp;August 1997.<ref>{{cite web |url=https://www.iana.org/domains/root/db/bv.html |title=Delegation Record for .BV |publisher=[[Internet Assigned Numbers Authority]] |date=13 November 2009 |access-date=5 September 2010 |archive-url=https://web.archive.org/web/20100813161615/https://www.iana.org/domains/root/db/bv.html |archive-date=13 August 2010 |url-status=dead |df=dmy-all}}</ref> The domain is managed by [[Norid]] but is not in use.<ref>{{cite web |url=http://www.norid.no/omnorid/bv-sj.en.html |title=The .bv and .sj top level domains |publisher=[[Norid]] |date=3 August 2010 |access-date=5 September 2010 |archive-url=https://web.archive.org/web/20101005074110/http://www.norid.no/omnorid/bv-sj.en.html |archive-date=5 October 2010 |url-status=dead |df=dmy-all}}</ref>


Bouvet Island has been designated with the [[ISO 3166-2]] code [[ISO 3166-2:BV|BV]]<ref>{{cite web|url=http://www.unece.org/stats/documents/1998/03/migration/5.e.pdf|title=Country classifications in migration statistics – present situation and proposals for a Eurostat standard|last1=Takle|first1=Mona Takle|first2=Kåre|last2=Vassenden|publisher=[[United Nations Statistical Commission]] and [[United Nations Economic Commission for Europe]]|date=March 1998|access-date=26 January 2011|archive-url=https://web.archive.org/web/20150713215624/http://www.unece.org/fileadmin/DAM/stats/documents/1998/03/migration/5.e.pdf|archive-date=13 July 2015|url-status=live}}</ref> and was subsequently awarded the [[country code]] [[top-level domain]] [[.bv]] on 21&nbsp;August 1997.<ref>{{cite web|url=https://www.iana.org/domains/root/db/bv.html|title=Delegation Record for .BV|publisher=[[Internet Assigned Numbers Authority]]|date=13 November 2009|access-date=5 September 2010|archive-url=https://web.archive.org/web/20100813161615/https://www.iana.org/domains/root/db/bv.html|archive-date=13 August 2010|url-status=dead}}</ref> The domain is managed by [[Norid]] but is not in use.<ref>{{cite web|url=http://www.norid.no/omnorid/bv-sj.en.html|title=The .bv and .sj top level domains|publisher=[[Norid]]|date=3 August 2010|access-date=5 September 2010|archive-url=https://web.archive.org/web/20101005074110/http://www.norid.no/omnorid/bv-sj.en.html|archive-date=5 October 2010|url-status=dead}}</ref>
The [[exclusive economic zone]] surrounding the island covers an area of {{cvt|441163|km2}}.<ref>{{cite web |url=http://www.seaaroundus.org/eez/74.aspx |title=EEZ Waters of Bouvet Isl. (Norway) |publisher=[[University of British Columbia]] |access-date=9 May 2012 |archive-date=27 January 2012 |archive-url=https://web.archive.org/web/20120127210923/http://www.seaaroundus.org/eez/74.aspx |url-status=live |df=dmy}}</ref> Monitoring of compliance with resource laws and regulations is carried out through the [[Convention for the Conservation of Antarctic Marine Living Resources|Commission for the Conservation of Antarctic Marine Living Resources]] (CCAMLR) which includes 27 member states, including Norway. Utilizing an intelligence-sharing approach, vessels that may have participated in illegal, unregulated or unreported fishing are subject to blacklisting and potential enforcement measures by member states and through [[INTERPOL]].<ref>{{cite web |url=https://www.regjeringen.no/contentassets/cef2a67e958849689aa7e89341159f29/en-gb/pdfs/stm201420150032000engpdfs.pdf |title=Norwegian Interests and Policy in the Antarctic |publisher=Norwegian Ministry of Foreign Affairs |access-date=8 September 2023 |date=12 June 2015}}</ref>


The [[exclusive economic zone]] surrounding the island covers an area of {{cvt|441163|km2}}.<ref>{{cite web|url=http://www.seaaroundus.org/eez/74.aspx|title=EEZ Waters of Bouvet Isl. (Norway)|publisher=[[University of British Columbia]]|access-date=9 May 2012|archive-date=27 January 2012|archive-url=https://web.archive.org/web/20120127210923/http://www.seaaroundus.org/eez/74.aspx|url-status=live}}</ref> Monitoring of compliance with resource laws and regulations is carried out through the [[Convention for the Conservation of Antarctic Marine Living Resources|Commission for the Conservation of Antarctic Marine Living Resources]] (CCAMLR) which includes 27 member states, including Norway. Utilizing an intelligence-sharing approach, vessels that may have participated in illegal, unregulated or unreported fishing are subject to blacklisting and potential enforcement measures by member states and through [[INTERPOL]].<ref>{{cite web|url=https://www.regjeringen.no/contentassets/cef2a67e958849689aa7e89341159f29/en-gb/pdfs/stm201420150032000engpdfs.pdf|title=Norwegian Interests and Policy in the Antarctic|publisher=Norwegian Ministry of Foreign Affairs|access-date=8 September 2023|date=12 June 2015}}</ref>
A [[king penguin]] in [[Edinburgh Zoo]], [[Nils Olav|Major General Sir Nils Olav III]], carries the title ''Baron of the Bouvet Islands''.<ref>{{Cite web |title=A Guard of Honour for Sir Nils Olav – the most famous king penguin in the world |url=https://www.edintattoo.co.uk/news/a-guard-of-honour-for-sir-nils-olav-the-most-famous-king-penguin-in-the-world |access-date=2024-05-30 |website=Royal Edinburgh Military Tattoo |language=en}}</ref>


[[File:Nils Olav wide.jpg|thumb|A [[king penguin]] in [[Edinburgh Zoo]] named [[Nils Olav]], Baron of the Bouvet Islands]]
== In fiction ==

*The island figures prominently in the book ''A Grue of Ice'' (1962), an adventure novel by [[Geoffrey Jenkins]], based on [[Tristan da Cunha]], Bouvet, and the mythical [[Thompson Island (South Atlantic)|Thompson Island]].<ref name="Jenkins-1962" />
A [[king penguin]] in [[Edinburgh Zoo]], [[Nils Olav|Major General Sir Nils Olav III]], carries the title ''Baron of the Bouvet Islands''.<ref>{{Cite web|title=A Guard of Honour for Sir Nils Olav – the most famous king penguin in the world|url=https://www.edintattoo.co.uk/news/a-guard-of-honour-for-sir-nils-olav-the-most-famous-king-penguin-in-the-world|access-date=2024-05-30|website=Royal Edinburgh Military Tattoo}}</ref>
*Bouvet is the setting of the 2004 film ''[[Alien vs. Predator (film)|Alien vs. Predator]]'', which uses its Norwegian name "Bouvetøya".<ref name="Alien-Predator-2004" />


== See also ==
== See also ==
Line 337: Line 337:
== References ==
== References ==
{{reflist|refs=
{{reflist|refs=
<ref name="ARH-NAM-1943">{{cite journal|author1=A.R.H.|author2=N.A.M.|year=1943|title=Review: A New Chart of the Antarctic|journal=[[The Geographical Journal]]|volume=102|issue=1|pages=29–34|doi=10.2307/1789367|jstor=1789367}}</ref>

<ref name=Alien-Predator-2004>{{cite web |title=AVP: Alien vs. Predator |url=https://www.imdb.com/title/tt0370263/ |website=[[IMDb]] |date=13 August 2004 |access-date=7 June 2015 |url-status=live |archive-url=https://web.archive.org/web/20150603150715/http://www.imdb.com/title/tt0370263/ |archive-date=3 June 2015 |df=dmy-all}}</ref>
<ref name="Baker-1967">{{cite journal|author=Baker, P.E.|year=1967|title=Historical and geological notes on Bouvetøya|journal=British Antarctic Survey Bulletin|issue=13|pages=71–84|url=http://www.antarctica.ac.uk/documents/bas_bulletins/bulletin13_06.pdf|access-date=8 May 2012|url-status=dead|archive-url=https://web.archive.org/web/20120316114353/http://www.antarctica.ac.uk/documents/bas_bulletins/bulletin13_06.pdf|archive-date=16 March 2012}}</ref>
<ref name="Barr-1987">{{cite book|last=Barr|first=Susan|year=1987|title=Norway's Polar Territories|location=Oslo|publisher=Aschehoug|isbn=8203156894}}</ref>

<ref name="Berulfsen-1969">{{cite book|last=Berulfsen|first=Bjarne|year=1969|title=Norsk Uttaleordbok|language=no|page=51|publisher=[[Aschehoug|H. Aschehoug & Co (W Nygaard)]]|location=Oslo}}</ref>
<ref name=ARH-NAM-1943>{{cite journal |author1=A.R.H. |author2=N.A.M. |year=1943 |title=Review: A New Chart of the Antarctic |journal=[[The Geographical Journal]] |volume=102 |issue=1 |pages=29–34 |doi=10.2307/1789367 |jstor=1789367}}</ref>
<ref name="Burney-1817">{{cite book|last=Burney|first=James|author-link=James Burney|year=1817|title=A Chronological History of the Discoveries in the South Sea or Pacific Ocean|volume=V|page=35|url=https://books.google.com/books?id=uNI-AAAAYAAJ}}</ref>

<ref name=Baker-1967>{{cite journal |author=Baker, P.E. |year=1967 |title=Historical and geological notes on Bouvetøya |journal=British Antarctic Survey Bulletin |issue=13 |pages=71–84 |url=http://www.antarctica.ac.uk/documents/bas_bulletins/bulletin13_06.pdf |access-date=8 May 2012 |url-status=dead |archive-url=https://web.archive.org/web/20120316114353/http://www.antarctica.ac.uk/documents/bas_bulletins/bulletin13_06.pdf |archive-date=16 March 2012 |df=dmy}}</ref>
<ref name="Climate-Zone-bouvet-island">{{cite report|title=Monthly averages for Bouvet Island|website=Climate Zone|url=http://www.climate-zone.com/climate/bouvet-island/celsius/bouvet-island.htm|access-date=1 January 2011|url-status=live|archive-url=https://web.archive.org/web/20110708165226/http://www.climate-zone.com/climate/bouvet-island/celsius/bouvet-island.htm|archive-date=8 July 2011}}</ref>
<ref name="DX-Bouvet-1989-1990">{{cite web|title=Bouvet (3Y/B)|date=25 December 1989 – 13 January 1990|url=http://www.allatelefonkataloger.com/dagfra/044bouvet.html|access-date=26 February 2018|url-status=live|archive-url=https://web.archive.org/web/20180124042419/http://www.allatelefonkataloger.com/dagfra/044bouvet.html|archive-date=24 January 2018}}</ref>

<ref name="DX-Bouvet-3Y5X">{{cite web|title=Bouvet Island 3Y5X|year=1990|url=http://www.qsl.net/k5mb/bouvet_island.html|access-date=13 May 2017|url-status=live|archive-url=https://web.archive.org/web/20161123033704/http://www.qsl.net/k5mb/bouvet_island.html|archive-date=23 November 2016}}</ref>
<ref name=Barr-1987>{{cite book |last=Barr |first=Susan |year=1987 |title=Norway's Polar Territories |location=Oslo |publisher=Aschehoug |isbn=8203156894}}</ref>
<ref name="DX-Bouvet-3Y0E">{{cite web|author=Stan SQ8X|date=10 February 2008|title=3Y0E is QRT|series=3Y0E Bouvet Island December 2007 – February 2008|website=3Y0E.wordpress.com|url=https://3y0e.wordpress.com/|access-date=26 February 2018|url-status=live|archive-url=https://web.archive.org/web/20180227094333/https://3y0e.wordpress.com/|archive-date=27 February 2018}}</ref>

<ref name="Expedition-Futur-2012-03-12">{{cite press release|title=Making history summiting the most remote land on earth|publisher=Expedition pour le Futur|date=4 March 2012|url=http://notrefutur.org/making-history-summiting-of-the-most-remote-land-on-earth/|access-date=4 March 2012|url-status=live|archive-url=https://web.archive.org/web/20130313180031/http://notrefutur.org/making-history-summiting-of-the-most-remote-land-on-earth/|archive-date=13 March 2013}}</ref>
<ref name=Berulfsen-1969>{{cite book |last=Berulfsen |first=Bjarne |year=1969 |title=Norsk Uttaleordbok |language=no |page=51 |publisher=[[Aschehoug|H. Aschehoug & Co (W Nygaard)]] |location=Oslo}}</ref>
<ref name="Gisle-1999">{{cite book|editor-last=Gisle|editor-first=Jon|year=1999|title=Jusleksikon|language=no|page=38|publisher=Kunnskapsforlaget|isbn=8257308625|url=http://urn.nb.no/URN:NBN:no-nb_digibok_2008092904084}}</ref>

<ref name="Headland-2018">{{cite book|editor-first=R.K.|editor-last=Headland|year=2018|title=Historical Antarctic Sealing Industry|page=168|department=Scott Polar Research Institute|publisher=Cambridge University|isbn=978-0901021267}}</ref>
<ref name=Burney-1817>{{cite book |last=Burney |first=James |author-link=James Burney |year=1817 |title=A Chronological History of the Discoveries in the South Sea or Pacific Ocean |volume=V |page=35 |url=https://books.google.com/books?id=uNI-AAAAYAAJ}}</ref>
<ref name="Hersh-1991">{{cite book|last=Hersh|first=Seymour|year=1991|title=The Samson option: Israel's Nuclear arsenal and American foreign policy|page=271|publisher=Random House|isbn=0394570065}}</ref>

<ref name="Hough-1994">{{cite book|last=Hough|first=Richard|author-link=Richard Hough|year=1994|title=Captain James Cook|page=248|publisher=Hodder and Stoughton|isbn=0340825561}}</ref>
<ref name=Climate-Zone-bouvet-island>{{cite report |title=Monthly averages for Bouvet Island |website=Climate Zone |url=http://www.climate-zone.com/climate/bouvet-island/celsius/bouvet-island.htm |access-date=1 January 2011 |url-status=live |archive-url=https://web.archive.org/web/20110708165226/http://www.climate-zone.com/climate/bouvet-island/celsius/bouvet-island.htm |archive-date=8 July 2011 |df=dmy-all}}</ref>
<ref name="Hyser-Bouvetøya-birdlife">{{cite web|last=Hyser|first=Onno|title=Bouvetøya|website=[[BirdLife International]]|url=http://www.birdlife.org/datazone/userfiles/file/IBAs/AfricaCntryPDFs/Bouvet.pdf|access-date=11 May 2012|url-status=live|archive-url=https://web.archive.org/web/20130313172001/http://www.birdlife.org/datazone/userfiles/file/IBAs/AfricaCntryPDFs/Bouvet.pdf|archive-date=13 March 2013}}</ref>

<ref name="Kyvik-2008">{{cite book|editor-last=Kyvik|editor-first=Helga|year=2008|title=Norge i Antarktis|language=no|location=Oslo|publisher=Schibsted Forlag|isbn=978-8251625890}}</ref>
<ref name=DX-Bouvet-1989-1990>{{cite web |title=Bouvet (3Y/B) |date=25 December 1989 – 13 January 1990 |url=http://www.allatelefonkataloger.com/dagfra/044bouvet.html |access-date=26 February 2018 |url-status=live |archive-url=https://web.archive.org/web/20180124042419/http://www.allatelefonkataloger.com/dagfra/044bouvet.html |archive-date=24 January 2018 |df=dmy-all}}</ref>
<ref name="McGonigal-2003">{{cite book|last=McGonigal|first=David|author-link=David McGonigal|year=2003|title=Antarctica|page=135|location=London|publisher=Frances Lincoln|isbn=978-0711229808|url=https://books.google.com/books?id=8bFcJgX0lIUC&pg=PA135}}</ref>

<ref name=DX-Bouvet-3Y5X>{{cite web |title=Bouvet Island 3Y5X |year=1990 |url=http://www.qsl.net/k5mb/bouvet_island.html |access-date=13 May 2017 |url-status=live |archive-url=https://web.archive.org/web/20161123033704/http://www.qsl.net/k5mb/bouvet_island.html |archive-date=23 November 2016 |df=dmy-all}}</ref>
<ref name="Météo-climat-Bouvet">{{cite report|title=Météo Climat stats for Ile Bouvet|publisher=Météo Climat|url=http://meteo-climat-bzh.dyndns.org/index.php?page=stati&id=20|access-date=8 November 2019}}</ref>
<ref name="Météo-climat-Norvege">{{cite report|title=Moyennes 1981–2010 Norvege (Atlantique Sud)|lang=fr|url=http://meteo-climat-bzh.dyndns.org/listenormale-1981-2010-1-p88.php|access-date=1 November 2019}}</ref>

<ref name="Mill-1905">{{cite book|last=Mill|first=Hugh Robert|author-link=Hugh Robert Mill|year=1905|title=The Siege of the South Pole|publisher=Alston Rivers|location=London}}</ref>
<ref name=DX-Bouvet-3Y0E>{{cite web |author=Stan SQ8X |date=10 February 2008 |title=3Y0E is QRT |series=3Y0E Bouvet Island December 2007 – February 2008 |website=3Y0E.wordpress.com |url=https://3y0e.wordpress.com/ |access-date=26 February 2018 |url-status=live |archive-url=https://web.archive.org/web/20180227094333/https://3y0e.wordpress.com/ |archive-date=27 February 2018 |df=dmy-all}}</ref>
<ref name="Mills-2003">{{cite book|last=Mills|first=William James|year=2003|title=Exploring Polar Frontiers: A historical encyclopedia|volume=1|publisher=ABC-CLIO|isbn=978-1576074220|url=https://books.google.com/books?id=PYdBH4dOOM4C&pg=PA435}}</ref>

<ref name="Mills-2003-1-96">{{cite book|last=Mills|first=William James|date=2003|title=Exploring Polar Frontiers: A Historical Encyclopedia|volume=1|page=96|publisher=ABC-CLIO|isbn=978-1576074220|url=https://books.google.com/books?id=PYdBH4dOOM4C}}</ref>
<!-- Not in use
<ref name="Mitchell-Livermore-etal-2000">{{cite journal|last1=Mitchell|first1=Neil C.|last2=Livermore|first2=Roy A.|last3=Fabretti|first3=Paola|last4=Carrara|first4=Gabriela|year=2000|title=The Bouvet triple junction, 20 to 10 Ma, and extensive transtensional deformation adjacent to the Bouvet and Conrad transforms|journal=[[Journal of Geophysical Research]]|volume=105|issue=B4|pages=8279–8296|doi=10.1029/1999JB900399|doi-access=free|bibcode=2000JGR...105.8279M|url=http://personalpages.manchester.ac.uk/staff/neil.mitchell/pubs/2000JGRBouvet.pdf|access-date=11 May 2012|url-status=live|archive-url=https://web.archive.org/web/20120424230058/http://personalpages.manchester.ac.uk/staff/neil.mitchell/pubs/2000JGRBouvet.pdf|archive-date=24 April 2012}}</ref>
<ref name=DX-Bouvet-3Y0J>{{cite web |title=The Bouvet Island DXpedition 2023 |website=3Y0J |url=https://3y0j.com/ |access-date=14 June 2021}}</ref>
<ref name="placenames-npolar-Bouvetøya">{{cite web|title=Bouvetøya|website=placenames.npolar.no|publisher=[[Norwegian Polar Institute]]|url=http://placenames.npolar.no/stadnamn/Bouvet%C3%B8ya?ident=902593|access-date=8 May 2012|url-status=live|archive-url=https://web.archive.org/web/20130314122934/http://placenames.npolar.no/stadnamn/Bouvet%C3%B8ya?ident=902593|archive-date=14 March 2013}}</ref>
Not in use-->
<ref name="polar-stadnamn-Bouvetøya">{{cite web|title=Bouvetøya|series=Place names in Norwegian polar areas|website=stadnamn.npolar.no|publisher=[[Norwegian Polar Institute]]|url=https://stadnamn.npolar.no/Bouvetøya/Bouvetøya}}</ref>
<ref name=Expedition-Futur-2012-03-12>{{cite press release |title=Making history summiting the most remote land on earth |publisher=Expedition pour le Futur |date=4 March 2012 |url=http://notrefutur.org/making-history-summiting-of-the-most-remote-land-on-earth/ |access-date=4 March 2012 |url-status=live |archive-url=https://web.archive.org/web/20130313180031/http://notrefutur.org/making-history-summiting-of-the-most-remote-land-on-earth/ |archive-date=13 March 2013 |df=dmy-all}}</ref>
<ref name="Rhodes-2011">{{cite book|last=Rhodes|first=Richard|year=2011|title=Twilight of the Bombs: Recent challenges, new dangers, and the prospects for a world without nuclear weapons|pages=164–169|publisher=Random House|isbn=978-0307387417|url=https://books.google.com/books?id=qZgBYgfJvc8}}{{Dead link|date=September 2024 |bot=InternetArchiveBot |fix-attempted=yes}}</ref>

<ref name=Gisle-1999>{{cite book |editor-last=Gisle |editor-first=Jon |year=1999 |title=Jusleksikon |language=no |page=38 |publisher=Kunnskapsforlaget |isbn=8257308625 |url=http://urn.nb.no/URN:NBN:no-nb_digibok_2008092904084}}</ref>
<ref name="Rubin-2005">{{cite book|last=Rubin|first=Jeff|year=2005|title=Antarctica|page=155|publisher=Lonely Planet|isbn=1740590945}}</ref>
<ref name="Schiermeier-2010">{{cite journal|last=Schiermeier|first=Quirin|date=2 September 2010|title=Ecologists fear Antarctic krill crisis|journal=[[Nature (journal)|Nature]]|volume=467|issue=15|page=15|doi=10.1038/467015a|doi-access=free|pmid=20811427}}</ref>

<ref name=Headland-2018>{{cite book |editor-first=R.K. |editor-last=Headland |year=2018 |title=Historical Antarctic Sealing Industry |page=168 |department=Scott Polar Research Institute |publisher=Cambridge University |isbn=978-0901021267}}</ref>
<ref name="Simpson-Housley-1992">{{cite book|last=Simpson-Housley|first=Paul|year=1992|title=Antarctica: Exploration, perception, and metaphor|page=60|publisher=Routledge|location=New York|isbn=978-0415082259}}</ref>
<ref name="SI-Volcanism-Bouvet">{{cite web|title=Bouvet|publisher=Global Volcanism Program|url=http://www.volcano.si.edu/world/volcano.cfm?vnum=1806-02-|access-date=10 May 2012|url-status=live|archive-url=https://web.archive.org/web/20111202222049/http://www.volcano.si.edu/world/volcano.cfm?vnum=1806-02-|archive-date=2 December 2011}}</ref>

<ref name="Weiss-2011">{{cite journal|last=Weiss|first=Leonard|year=2011|title=Israel's 1979 nuclear test and the U.S. cover-up|journal=[[Middle East Policy]]|volume=18|issue=4|pages=83–95|doi=10.1111/j.1475-4967.2011.00512.x|url=http://iis-db.stanford.edu/pubs/23198/Weiss_IsraelNuclearTest.pdf|access-date=12 May 2012|url-status=dead|archive-url=https://web.archive.org/web/20140606232313/http://iis-db.stanford.edu/pubs/23198/Weiss_IsraelNuclearTest.pdf|archive-date=6 June 2014}}</ref>
<ref name=Hersh-1991>{{cite book |last=Hersh |first=Seymour |year=1991 |title=The Samson option: Israel's Nuclear arsenal and American foreign policy |page=271 |publisher=Random House |isbn=0394570065}}</ref>
<ref name="wordpress-abandoned-lifeboat">{{cite web|title=An abandoned lifeboat at world's end|series=A Blast from the Past|url=http://allkindsofhistory.wordpress.com/2011/02/13/an-abandoned-lifeboat-at-worlds-end/|website=allkindsofhistory.wordpress.com|date=13 February 2011|access-date=7 June 2015|url-status=live|archive-url=https://web.archive.org/web/20111102134836/http://allkindsofhistory.wordpress.com/2011/02/13/an-abandoned-lifeboat-at-worlds-end/|archive-date=2 November 2011}}</ref>

<ref name="LOV19300227">{{Cite web|title=Lov om Bouvet-øya, Peter&nbsp;I's øy og Dronning Maud Land m.m. (bilandsloven)|url=http://www.lovdata.no/all/tl-19300227-003-0.html#1|language=no|publisher=Lovdata|access-date=29 August 2011|archive-date=2 December 2013|archive-url=https://web.archive.org/web/20131202231248/http://www.lovdata.no/all/tl-19300227-003-0.html|url-status=live}}</ref>
<ref name=Hough-1994>{{cite book |last=Hough |first=Richard |author-link=Richard Hough |year=1994 |title=Captain James Cook |page=248 |publisher=Hodder and Stoughton |isbn=0340825561}}</ref>
<ref name="FOR19711217">{{cite web|title=Forskrift om fredning av Bouvetøya med tilliggende territorialfarvann som naturreservat|url=http://lovdata.no/for/sf/md/xd-19711217-0009.html|language=no|publisher=Lovdata|access-date=9 May 2012|archive-date=6 June 2014|archive-url=https://web.archive.org/web/20140606224540/http://lovdata.no/for/sf/md/xd-19711217-0009.html|url-status=live}}</ref>

<ref name="radcom199008_3y5x">{{cite magazine|url=https://archive.org/details/RadCom_Magazine_1990-08/page/n11/mode/2up|title=The Club Bouvet 3Y5X Story|magazine=Radio Communication|last1=Enderud|first1=Einar|last2=Pedersen|first2=Kåre|date=August 1990|access-date=24 February 2024|pages=12–13, 61}}</ref>
<ref name=Hyser-Bouvetøya-birdlife>{{cite web |last=Hyser |first=Onno |title=Bouvetøya |website=[[BirdLife International]] |url=http://www.birdlife.org/datazone/userfiles/file/IBAs/AfricaCntryPDFs/Bouvet.pdf |access-date=11 May 2012 |url-status=live |archive-url=https://web.archive.org/web/20130313172001/http://www.birdlife.org/datazone/userfiles/file/IBAs/AfricaCntryPDFs/Bouvet.pdf |archive-date=13 March 2013 |df=dmy}}</ref>
<ref name="larsoya">{{cite web|title=Larsøya|url=http://stadnamn.npolar.no/stadnamn/Lars%C3%B8ya?ident=903010&lang=en|publisher=[[Norwegian Polar Institute]]|access-date=8 May 2012|archive-date=14 March 2013|archive-url=https://web.archive.org/web/20130314123005/http://stadnamn.npolar.no/stadnamn/Lars%C3%B8ya?ident=903010&lang=en|url-status=live}}</ref>

<ref name="npolar">{{cite web|url=http://www.npolar.no/no/antarktis/bouvetoya.html|title=Bouvetøya|publisher=[[Norwegian Polar Institute]]|access-date=10 May 2012|archive-date=15 April 2012|archive-url=https://web.archive.org/web/20120415125957/http://www.npolar.no/no/antarktis/bouvetoya.html|url-status=dead}}</ref>
<ref name=Jenkins-1962>{{cite book |last=Jenkins |first=G |author-link=Geoffrey Jenkins |year=1962 |title=A Grue of Ice |edition=UK |place=London|publisher=Collins}} simultaneously published in the U.S. as ''The Disappearing Island''</ref>
<ref name="factbook">{{cite web|url=https://www.cia.gov/the-world-factbook/countries/bouvet-island/|title=Bouvet Island|work=[[The World Factbook]]|publisher=[[Central Intelligence Agency]]|access-date=9 May 2012}}</ref>

<ref name=Kyvik-2008>{{cite book |editor-last=Kyvik |editor-first=Helga |year=2008 |title=Norge i Antarktis |language=no |location=Oslo |publisher=Schibsted Forlag |isbn=978-8251625890}}</ref>

<ref name=McGonigal-2003>{{cite book |last=McGonigal |first=David |author-link=David McGonigal |year=2003 |title=Antarctica |page=135 |location=London |publisher=Frances Lincoln |isbn=978-0711229808 |url=https://books.google.com/books?id=8bFcJgX0lIUC&pg=PA135}}</ref>

<ref name=Météo-climat-Bouvet>{{cite report |title=Météo Climat stats for Ile Bouvet |publisher=Météo Climat |url=http://meteo-climat-bzh.dyndns.org/index.php?page=stati&id=20 |access-date=8 November 2019}}</ref>

<ref name=Météo-climat-Norvege>{{cite report |title=Moyennes 1981–2010 Norvege (Atlantique Sud) |lang=fr |url=http://meteo-climat-bzh.dyndns.org/listenormale-1981-2010-1-p88.php |access-date=1 November 2019}}</ref>

<ref name=Mill-1905>{{cite book |last=Mill |first=Hugh Robert |author-link=Hugh Robert Mill |year=1905 |title=The Siege of the South Pole |publisher=Alston Rivers |location=London}}</ref>

<ref name=Mills-2003>{{cite book |last=Mills |first=William James |year=2003 |title=Exploring Polar Frontiers: A historical encyclopedia |volume=1 |publisher=ABC-CLIO |isbn=978-1576074220|url=https://books.google.com/books?id=PYdBH4dOOM4C&pg=PA435}}</ref>

<ref name=Mills-2003-1-96>{{cite book |last=Mills |first=William James |date=2003 |title=Exploring Polar Frontiers: A Historical Encyclopedia |volume=1 |page=96 |publisher=ABC-CLIO |isbn=978-1576074220 |url=https://books.google.com/books?id=PYdBH4dOOM4C}}</ref>

<ref name=Mitchell-Livermore-etal-2000>{{cite journal |last1=Mitchell |first1=Neil C. |last2=Livermore |first2=Roy A. |last3=Fabretti |first3=Paola |last4=Carrara |first4=Gabriela |year=2000 |title=The Bouvet triple junction, 20 to 10 Ma, and extensive transtensional deformation adjacent to the Bouvet and Conrad transforms |journal=[[Journal of Geophysical Research]] |volume=105 |issue=B4 |pages=8279–8296 |doi=10.1029/1999JB900399 |doi-access=free |bibcode=2000JGR...105.8279M |url=http://personalpages.manchester.ac.uk/staff/neil.mitchell/pubs/2000JGRBouvet.pdf |access-date=11 May 2012 |url-status=live |archive-url=https://web.archive.org/web/20120424230058/http://personalpages.manchester.ac.uk/staff/neil.mitchell/pubs/2000JGRBouvet.pdf |archive-date=24 April 2012 |df=dmy}}</ref>

<ref name=placenames-npolar-Bouvetøya>{{cite web |title=Bouvetøya |website=placenames.npolar.no |publisher=[[Norwegian Polar Institute]] |url=http://placenames.npolar.no/stadnamn/Bouvet%C3%B8ya?ident=902593 |access-date=8 May 2012 |url-status=live |archive-url=https://web.archive.org/web/20130314122934/http://placenames.npolar.no/stadnamn/Bouvet%C3%B8ya?ident=902593 |archive-date=14 March 2013 |df=dmy}}</ref>

<ref name=polar-stadnamn-Bouvetøya>{{cite web |title=Bouvetøya |series=Place names in Norwegian polar areas |website=stadnamn.npolar.no |publisher=[[Norwegian Polar Institute]] |url=https://stadnamn.npolar.no/Bouvetøya/Bouvetøya}}</ref>

<ref name=Rhodes-2011>{{cite book |last=Rhodes |first=Richard |year=2011 |title=Twilight of the Bombs: Recent challenges, new dangers, and the prospects for a world without nuclear weapons |pages=164–169 |publisher=Random House |isbn=978-0307387417 |url=https://books.google.com/books?id=qZgBYgfJvc8}}</ref>

<ref name=Rubin-2005>{{cite book |last=Rubin |first=Jeff |year=2005 |title=Antarctica |page=155 |publisher=Lonely Planet |isbn=1740590945}}</ref>

<ref name=Schiermeier-2010>{{cite journal |last=Schiermeier |first=Quirin |date=2 September 2010 |title=Ecologists fear Antarctic krill crisis |journal=[[Nature (journal)|Nature]] |volume=467 |issue=15 |page=15 |doi=10.1038/467015a |doi-access=free |pmid=20811427 |df=dmy-all}}</ref>

<ref name=Simpson-Housley-1992>{{cite book |last=Simpson-Housley |first=Paul |year=1992 |title=Antarctica: Exploration, perception, and metaphor |page=60 |publisher=Routledge |location=New York |isbn=978-0415082259}}</ref>

<ref name=SI-Volcanism-Bouvet>{{cite web |title=Bouvet |publisher=[[Smithsonian Institution]] |department=[[Global Volcanism Program]] |website=volcano.si.edu |url=http://www.volcano.si.edu/world/volcano.cfm?vnum=1806-02- |access-date=10 May 2012 |url-status=live |archive-url=https://web.archive.org/web/20111202222049/http://www.volcano.si.edu/world/volcano.cfm?vnum=1806-02- |archive-date=2 December 2011 |df=dmy}}</ref>

<ref name=Weiss-2011>{{cite journal |last=Weiss |first=Leonard |year=2011 |title=Israel's 1979 nuclear test and the U.S. cover-up |journal=[[Middle East Policy]] |volume=18 |issue=4 |pages=83–95 |doi=10.1111/j.1475-4967.2011.00512.x |url=http://iis-db.stanford.edu/pubs/23198/Weiss_IsraelNuclearTest.pdf |access-date=12 May 2012 |url-status=dead |archive-url=https://web.archive.org/web/20140606232313/http://iis-db.stanford.edu/pubs/23198/Weiss_IsraelNuclearTest.pdf |archive-date=6 June 2014 |df=dmy-all}}</ref>

<ref name=wordpress-abandoned-lifeboat>{{cite web |title=An abandoned lifeboat at world's end |series=A Blast from the Past |url=http://allkindsofhistory.wordpress.com/2011/02/13/an-abandoned-lifeboat-at-worlds-end/ |website=allkindsofhistory.wordpress.com |date=13 February 2011 |access-date=7 June 2015 |url-status=live |archive-url=https://web.archive.org/web/20111102134836/http://allkindsofhistory.wordpress.com/2011/02/13/an-abandoned-lifeboat-at-worlds-end/ |archive-date=2 November 2011 |df=dmy-all}}</ref>
}}
}}



Latest revision as of 01:17, 2 December 2024

Bouvet Island
Bouvetøya (Norwegian)
Location of Bouvet Island (circled in red)
Location of Bouvet Island (circled in red, in the Atlantic Ocean)
Country Norway
Annexed by Norway23 January 1928 (1928-01-23)
Dependency status27 February 1930[1]
Nature reserve declared17 December 1971[2]
Official languagesNorwegian
GovernmentDependency under a constitutional monarchy
• Monarch
Harald V
• Administered by
Ministry of Justice and Public Security
• Baron (de jure)
Nils Olav III
Area
• Total
49 km2 (19 sq mi)
93%
Highest elevation
780 m (2,560 ft)
Population
• Estimate
0
ISO 3166 codeBV
Internet TLD
Map

Bouvet Island (/ˈbv/ BOO-vay; Norwegian: Bouvetøya[3] [bʉˈvèːœʏɑ])[4] is an uninhabited subantarctic volcanic island and dependency of Norway. It is a protected nature reserve, and situated in the South Atlantic Ocean at the southern end of the Mid-Atlantic Ridge, it is the world's most remote island. Located north of the Antarctic Circle, Bouvet Island is not part of the southern region covered by the Antarctic Treaty System.

The island lies 1,700 km (1,100 mi) north of the Princess Astrid Coast of Queen Maud Land, Antarctica, 1,870 km (1,160 mi) east of the South Sandwich Islands, 1,845 km (1,146 mi) south of Gough Island, and 2,520 km (1,570 mi) south-southwest of the coast of South Africa. It has an area of 49 km2 (19 sq mi), 93 percent of which is covered by a glacier. The centre of the island is the ice-filled crater of an inactive volcano. Some skerries and one smaller island, Larsøya, lie along its coast. Nyrøysa, created by a rock slide in the late 1950s, is the only easy place to land and is the location of a weather station.

The island was first spotted on 1 January 1739 by the Frenchman Jean-Baptiste Charles Bouvet de Lozier, during a French exploration mission in the South Atlantic with the ships Aigle and Marie. They did not make landfall. He mislabeled the coordinates for the island, and it was not sighted again until 1808, when the British whaler James Lindsay encountered it and named it Lindsay Island.[5] The first claim to have landed on the island was made by the American sailor Benjamin Morrell, although this claim is disputed. In 1825, the island was claimed for the British Crown by George Norris, who named it Liverpool Island. He also reported having sighted another island nearby, which he named Thompson Island, but this was later shown to be a phantom island.

In 1927, the first Norvegia expedition landed on the island, and claimed it for Norway. At that point, the island was given its current name of Bouvet Island ("Bouvetøya" in Norwegian).[6] In 1930, following resolution of a dispute with the United Kingdom over claiming rights, it was declared a Norwegian dependency. In 1971, it was designated a nature reserve.

History

[edit]

Discovery and early sightings

[edit]
Hand-coloured photograph of the southeast coast of Bouvet Island in 1898

The island was discovered on 1 January 1739 by Jean-Baptiste Charles Bouvet de Lozier, commander of the French ships Aigle and Marie.[5] Bouvet, who was searching for a presumed large southern continent, spotted the island through the fog and named the cape he saw Cap de la Circoncision. He was not able to land and did not circumnavigate his discovery, thus not clarifying if it was an island or part of a continent.[7]: 62  His plotting of its position was inaccurate,[8]: 47  leading several expeditions to fail to find the island.[7]: 58  James Cook's second voyage set off from Cape Verde on 22 November 1772 and attempted to find the island, but also failed.[9]

The next expedition to spot the island was in 1808 by James Lindsay, captain of the Samuel Enderby & Sons' (SE&S) snow whaler Swan.[10] Swan and another Enderby whaler, Otter were in company when they reached the island and recorded its position, though they were unable to land.[11][12]: 434–435  Lindsay could confirm that the "cape" was indeed an island.[7]: 62  The next expedition to arrive at the island was American Benjamin Morrell and his seal hunting ship Wasp. Morrell, by his own account, found the island without difficulty (with "improbable ease", in the words of historian William Mills)[12]: 434–435  before landing and hunting 196 seals.[7]: 62  In his subsequent lengthy description, Morrell does not mention the island's most obvious physical feature: Its permanent ice cover.[8]: 106–107  This has caused some commentators to doubt whether he actually visited the island.[12]: 434–435 [13]

On 10 December 1825, SE&S's George Norris, master of the Sprightly, landed on the island,[7]: 62  named it Liverpool Island and claimed it for the British Crown and George IV on 16 December.[7]: 63  The next expedition to spot the island was Joseph Fuller and his ship Francis Allyn in 1893, but he was not able to land on the island. German Carl Chun's Valdivia Expedition arrived at the island in 1898. They were not able to land, but dredged the seabed for geological samples.[14] They were also the first to accurately fix the island's position.[7]: 63  At least three sealing vessels visited the island between 1822 and 1895. A voyage of exploration in 1927–1928 also took seal pelts.[15]

Norris also spotted a second island in 1825, which he named Thompson Island, which he placed 72 km (45 mi) north-northeast of Liverpool Island. Thompson Island was also reported in 1893 by Fuller, but in 1898 Chun did not report seeing such an island, nor has anyone since.[14] However, Thompson Island continued to appear on maps as late as 1943.[16] A 1967 paper suggested that the island might have disappeared in an undetected volcanic eruption, but in 1997 it was discovered that the ocean is more than 2,400 m (7,900 ft) deep in the area.[17]

Norwegian annexation

[edit]
The claiming of the island on 1 December 1927
The first hut, built on Cape Circoncision, in 1929

In 1927, the First Norvegia Expedition, led by Harald Horntvedt and financed by the shipowner and philanthropist Lars Christensen, was the first to make an extended stay on the island. Observations and surveying were conducted on the island and oceanographic measurements performed in the sea around it. At Ny Sandefjord, a small hut was erected and, on 1 December, the Norwegian flag was hoisted and the island claimed for Norway. The annexation was established by a royal decree on 23 January 1928.[7]: 63 

The claim was initially protested by the United Kingdom, on the basis of Norris's landing and annexation. However, the British position was weakened by Norris's sighting of two islands and the uncertainty as to whether he had been on Thompson or Liverpool (i.e. Bouvet) Island. Norris's positioning deviating from the correct location combined with the island's small size and lack of a natural harbour made the UK accept the Norwegian claim.[18]: 52  This resulted in diplomatic negotiations between the two countries, and in November 1929, Britain renounced its claim to the island.[7]: 63 

The Second Norvegia Expedition arrived in 1928 with the intent of establishing a staffed meteorological radio station, but a suitable location could not be found.[7]: 63  By then both the flagpole and hut from the previous year had been washed away. The Third Norvegia Expedition, led by Hjalmar Riiser-Larsen, arrived the following year and built a new hut at Cape Circoncision and on Larsøya. The expedition carried out aerial photography of the island and was the first Antarctic expedition to use aircraft.[7]: 64  The Dependency Act, passed by the Parliament of Norway on 27 February 1930, established Bouvet Island as a Norwegian dependency, along with Peter I Island and Queen Maud Land.[1] The eared seal was protected on and around the island in 1929, and in 1935 all seals around the island were protected.[19]

Recent history

[edit]

In 1955, the South African frigate SAS Transvaal visited the island.[20] Nyrøysa, a rock-strewn ice-free area, the largest such on Bouvet, was created sometime between 1955 and 1958, probably by a landslide.[21]

In 1964, the island was visited by the British naval ship HMS Protector. One of Protector's two Westland Whirlwind helicopters landed a small survey team on the island led by Lieutenant Commander Alan Crawford at Nyrøysa for a brief visit. Shortly after landing, the survey team discovered an abandoned lifeboat in a small lagoon. With very little time, a brief search was made but no other signs of human activity were found, and the identity of the lifeboat remained a mystery for many years.[22]: 177–85 

On 17 December 1971, the entire island and its territorial waters were protected as a nature reserve.[2] A scientific landing was made in 1978, during which the underground temperature was measured to be 25 °C (77 °F).[23] In addition to scientific surveys,[14] the lifeboat found by the Protector team was recovered from Nyrøysa, although no other signs of people were found.[23] The lifeboat was believed to belong to a Soviet scientific reconnaissance vessel.[b]

The Vela incident took place on 22 September 1979, on or above the sea between Bouvetøya and Prince Edward Islands, when the American Vela Hotel satellite 6911 registered an unexplained double flash. This observation has been variously interpreted as a meteor, or an instrumentation glitch, but most independent assessments conclude it was an undeclared joint nuclear test carried out by South Africa and Israel.[23][25][26][27]

In the mid-1980s, Bouvetøya, Jan Mayen, and Svalbard were considered as locations for the new Norwegian International Ship Register, but the flag of convenience registry was ultimately established in Bergen, Norway, in 1987.[18]: 189  In 2007, the island was added to Norway's tentative list of nominations as a World Heritage Site as part of the transnational nomination of the Mid-Atlantic Ridge.[28]

Krill fishing in the Southern Ocean is subject to the Convention for the Conservation of Antarctic Marine Living Resources, which defines maximum catch quotas for a sustainable exploitation of Antarctic krill.[29] Surveys conducted in 2000 showed high concentration of krill around Bouvetøya. In 2004, Aker BioMarine was awarded a concession to fish krill, and additional quotas were awarded from 2008 for a total catch of 620,000 t (610,000 long tons; 680,000 short tons).[30] There is a controversy as to whether the fisheries are sustainable, particularly in relation to krill being important food for whales.[31] In 2009, Norway filed with the UN Commission on the Limits of the Continental Shelf to extend the outer limit of the continental shelf past 200 NM (230 mi; 370 km) surrounding the island.[32]

The expedition ship Hanse Explorer visited Bouvet Island on 20 and 21 February 2012 as part of "Expédition pour le Futur".[33] The expedition's goal was to land and climb the highest point on the island.[c]

Bouvet Island is assigned the amateur radio callsign prefix 3Y0,[34] and several amateur radio DX-peditions have been conducted to the island.[35][36][37][38] The 3Y0J DX-pedition to Bouvet Island took place between January and February 2023, but had to be reduced in scope and eventually cut short due to bad and worsening weather conditions.[39][40]

Norvegia Station

[edit]
Norvegia Station
Map
Coordinates: 54°24′25″S 3°17′16″E / 54.407052°S 3.287791°E / -54.407052; 3.287791
Country Norway
OperatorNorwegian Polar Institute
Established1927 (1927)
Population
 • Summer
6
 • Winter
0
UN/LOCODENO
Active timesEvery summer
StatusOperational
ActivitiesMeteorology
FacilitiesDorms and labs
Websitenpolar.no

Since the 1970s, the island has been visited frequently by Norwegian Antarctic expeditions. In 1977 a temporary five-man station and an automated weather station were constructed and staffed for two months in 1978 and 1979.[7]: 64 

In March 1985, a Norwegian expedition experienced sufficiently clear weather to allow the entire island to be photographed from the air, resulting in the first accurate map of the whole island, 247 years after its discovery.[7]: 59 

The Norwegian Polar Institute established a 36 m2 (390 sq ft) research station, made of shipping containers, at Nyrøysa in 1996. On 23 February 2006, the island experienced a magnitude 6.2 earthquake whose epicentre was about 100 km (62 mi) away,[41] weakening the station's foundation and causing it to be blown to sea during a winter storm.[42][43]

In December 2012, a new research station was sent by ship from Tromsø in Norway, via Cape Town, to Bouvet.[44]

The robust and technically advanced station was assembled in Nyrøysa, on the north-western part of the island, the only place wide enough to land by helicopter. The elevated station is formed by three modules placed on a steel platform fixed into a concrete base. It can accommodate six people for periods of 2–4 months, and it is designed and equipped to resist rough weather conditions. The energy is supplied by wind power, which makes it easier to operate the equipment during the long periods when the station is uninhabited. The base is equipped with an automatic meteorological station that sends data via satellite throughout the year.[45]

Geography and geology

[edit]
Map of Bouvet Island
Glacier on Bouvet Island's west coast

Bouvetøya is a volcanic island constituting the top of a shield volcano just off the Southwest Indian Ridge in the South Atlantic Ocean.[46] The island measures 9.5 by 7 km (5.9 by 4.3 mi) and covers an area of 49 km2 (19 sq mi),[19] including a number of small rocks and skerries and one sizable island, Larsøya.[47]

It is located in the Subantarctic, south of the Antarctic Convergence,[48] which, by some definitions, would place the island in the Southern Ocean.[49]

Bouvet Island is one of the most remote islands in the world.[50] The closest land is Queen Maud Land of Antarctica, which is 1,700 km (1,100 mi) to the south,[7]: 58  and Gough Island, 1,845 km (1,146 mi) to the north.[51] The closest inhabited location is Tristan da Cunha island, 2,250 km (1,400 mi) to the northwest.[19] To its west, the South Sandwich Islands lie about 1,900 km (1,200 mi) away, and to its east are the Prince Edward Islands, about 2,500 km (1,600 mi) away.[citation needed]

Nyrøysa is a 2 by 0.5 km (1.2 by 0.3 mi) terrace located on the north-west coast of the island. Created by a rock slide sometime between 1955 and 1957, it is the island's easiest access point.[7]: 59  It is the site of the automatic weather station.[52] The north-west corner is the peninsula of Cape Circoncision.[53] From there, east to Cape Valdivia, the coast is known as Morgenstiernekysten.[54]

Store Kari is an islet located 1.2 km (0.75 mi) east of the cape.[55] From Cape Valdivia, southeast to Cape Lollo, on the east side of the island, the coast is known as Victoria Terrasse.[56] From there to Cape Fie at the southeastern corner, the coast is known as Mowinckelkysten. Svartstranda is a section of black sand which runs 1.8 km (1.1 mi) along the section from Cape Meteor, south to Cape Fie.[57]

After rounding Cape Fie, the coast along the south side is known as Vogtkysten.[58] The westernmost part of it is the 300 m (980 ft) long shore of Sjøelefantstranda.[59]

Off Catoodden, on the south-western corner, lies Larsøya, the only island of any size off Bouvetøya.[47] The western coast from Catoodden north to Nyrøysa, is known as Esmarchkysten. Midway up the coast lies Norvegiaodden (Cape Norvegia)[60] and 0.5 km (0.31 mi) off it the skerries of Bennskjæra.[61]

Ninety-three percent of the island is covered by glaciers, giving it a domed shape.[7]: 59  The summit region of the island is Wilhelmplatået, slightly to the west of the island's centre.[14] The plateau is 3.5 km (2.2 mi) across[62] and surrounded by several peaks.[14] The tallest is Olavtoppen, 780 m (2,560 ft) above mean sea level (AMSL),[7]: 59  followed by Lykketoppen (766 m or 2,513 ft AMSL)[63] and Mosbytoppane (670 m or 2,200 ft AMSL).[64] Below Wilhelmplatået is the main caldera responsible for creating the island.[14] The last eruption took place circa 2000 BCE, producing a lava flow at Cape Meteor.[62] The volcano is presumed to be in a declining state.[14] The temperature 30 cm (12 in) below the surface is 25 °C (77 °F).[7]: 59 

The island's total coastline is 29.6 km (18.4 mi).[65] Landing on the island is very difficult, as it normally experiences high seas and features a steep coast.[7]: 59  During the winter, it is surrounded by pack ice.[19] The Bouvet triple junction is located 275 km (171 mi) west of Bouvet Island. It is a triple junction between the South American plate, the African plate and the Antarctic plate, and of the Mid-Atlantic Ridge, the Southwest Indian Ridge and the American–Antarctic Ridge.[66]

A view of the west coast of Bouvet Island

Climate

[edit]

The island is located south of the Antarctic Convergence, giving it a marine Antarctic climate dominated by heavy clouds and fog. It experiences a mean temperature of −1 °C (30 °F),[7]: 59  with January average of 1 °C (34 °F) and September average of −3 °C (27 °F).[51] The monthly high mean temperatures fluctuate little through the year.[67] The peak temperature of 14 °C (57 °F) was recorded in March 1980, caused by intense sun radiation. Spot temperatures as high as 20 °C (68 °F) have been recorded in sunny weather on rock faces.[7]: 59  The island predominantly experiences a weak west wind.[51]

Climate data for Bouvet Island
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high °C (°F) 10.2
(50.4)
10.2
(50.4)
10.6
(51.1)
7.7
(45.9)
5.6
(42.1)
5.2
(41.4)
3.8
(38.8)
5.9
(42.6)
7.3
(45.1)
8.7
(47.7)
8.3
(46.9)
10.6
(51.1)
10.6
(51.1)
Mean daily maximum °C (°F) 3.7
(38.7)
4.0
(39.2)
3.3
(37.9)
2.5
(36.5)
1.0
(33.8)
−0.4
(31.3)
−1.2
(29.8)
−1.1
(30.0)
−0.8
(30.6)
0.5
(32.9)
1.8
(35.2)
3.0
(37.4)
1.4
(34.4)
Daily mean °C (°F) 1.7
(35.1)
2.0
(35.6)
1.5
(34.7)
0.9
(33.6)
−0.8
(30.6)
−2.2
(28.0)
−3.3
(26.1)
−3.6
(25.5)
−3.3
(26.1)
−1.8
(28.8)
−0.3
(31.5)
0.9
(33.6)
−0.7
(30.8)
Mean daily minimum °C (°F) −0.3
(31.5)
−0.1
(31.8)
−0.4
(31.3)
−0.8
(30.6)
−2.5
(27.5)
−3.9
(25.0)
−5.3
(22.5)
−6.0
(21.2)
−5.8
(21.6)
−4.1
(24.6)
−2.5
(27.5)
−1.2
(29.8)
−2.7
(27.1)
Record low °C (°F) −2.6
(27.3)
−2.2
(28.0)
−3.2
(26.2)
−4.7
(23.5)
−9.7
(14.5)
−10.2
(13.6)
−14.8
(5.4)
−15
(5)
−18.7
(−1.7)
−15.2
(4.6)
−8.4
(16.9)
−4.1
(24.6)
−18.7
(−1.7)
Source 1: Météo climat stats (Norvege)[68]
Source 2: Météo Climat stats (Isl. Bouvet)[69]

Nature

[edit]
NASA image of Bouvet Island from space

The harsh climate and ice-bound terrain limits non-animal life to fungi (ascomycetes including symbiotic lichens) and non-vascular plants (mosses and liverworts). The flora are representative for the maritime Antarctic and are phytogeographically similar to those of the South Sandwich Islands and South Shetland Islands. Vegetation is limited because of the ice cover, although snow algae are recorded. The remaining vegetation is located in snow-free areas such as nunatak ridges and other parts of the summit plateau, the coastal cliffs, capes and beaches. At Nyrøysa, five species of moss, six ascomycetes (including five lichens), and twenty algae have been recorded. Most snow-free areas are so steep and subject to frequent avalanches that only crustose lichens and algal formations are sustainable. There are six endemic ascomycetes, three of which are lichenized.[52]

Cape Valdivia, the northernmost point of Bouvet Island, in 2009

The island has been designated as an Important Bird Area by BirdLife International because of its importance as a breeding ground for seabirds. In 1978–1979 there were an estimated 117,000 breeding penguins on the island, consisting of macaroni penguin and, to a lesser extent, chinstrap penguin and Adélie penguin, although these were only estimated to be 62,000 in 1989–1990. Nyrøysa is the most important colony for penguins, supplemented by Posadowskybreen, Kapp Circoncision, Norvegiaodden and across from Larsøya. Southern fulmar is by far the most common non-penguin bird with 100,000 individuals. Other breeding seabirds consist of Cape petrel, Antarctic prion, Wilson's storm petrel, black-bellied storm petrel, subantarctic skua, southern giant petrel, snow petrel, slender-billed prion and Antarctic tern. Kelp gull is thought to have bred on the island earlier. Non-breeding birds which can be found on the island include the king penguin, wandering albatross, black-browed albatross, Campbell albatross, Atlantic yellow-nosed albatross, sooty albatross, light-mantled albatross, northern giant petrel, Antarctic petrel, blue petrel, soft-plumaged petrel, Kerguelen petrel, white-headed petrel, fairy prion, white-chinned petrel, great shearwater, common diving petrel, south polar skua and parasitic jaeger.[52]

The only non-bird vertebrates on the island are seals, specifically the southern elephant seal and Antarctic fur seal, which breed on the island. In 1998–1999, there were 88 elephant seal pups and 13,000 fur seal pups at Nyrøysa. Southern right whale, humpback whale, fin whale, southern right whale dolphin, hourglass dolphin, and orca are seen in the surrounding waters.[70][52][71][72]

Politics and government

[edit]
Image courtesy of the Image Science & Analysis Laboratory, NASA Johnson Space Center

Bouvetøya is one of three dependencies of Norway.[73] Unlike Peter I Island and Queen Maud Land, which are subject to the Antarctic Treaty System,[7]: 65  Bouvetøya is not disputed.[65] The dependency status entails that the island is not part of the Kingdom of Norway, but is still under Norwegian sovereignty. This implies that the island can be ceded without violating the first article of the Constitution of Norway.[73] Norwegian administration of the island is handled by the Polar Affairs Department of the Ministry of Justice and the Police, located in Oslo.[74]

The annexation of the island is regulated by the Dependency Act of 24 March 1933. It establishes that Norwegian criminal law, private law and procedural law apply to the island, in addition to other laws that explicitly state they are valid on the island. It further establishes that all land belongs to the state, and prohibits the storage and detonation of nuclear products.[1]

Bouvet Island has been designated with the ISO 3166-2 code BV[75] and was subsequently awarded the country code top-level domain .bv on 21 August 1997.[76] The domain is managed by Norid but is not in use.[77]

The exclusive economic zone surrounding the island covers an area of 441,163 km2 (170,334 sq mi).[78] Monitoring of compliance with resource laws and regulations is carried out through the Commission for the Conservation of Antarctic Marine Living Resources (CCAMLR) which includes 27 member states, including Norway. Utilizing an intelligence-sharing approach, vessels that may have participated in illegal, unregulated or unreported fishing are subject to blacklisting and potential enforcement measures by member states and through INTERPOL.[79]

A king penguin in Edinburgh Zoo named Nils Olav, Baron of the Bouvet Islands

A king penguin in Edinburgh Zoo, Major General Sir Nils Olav III, carries the title Baron of the Bouvet Islands.[80]

See also

[edit]

Explanatory notes

[edit]
  1. ^ The internet domain suffix .bv is allocated to Bouvetøya, but has never been used.
  2. ^ The scientific reconnaissance vessel 'Slava-9' began its regular 13th cruise with the 'Slava' Antarctic whaling fleet on 22 October 1958 ... On 27 November she got to Bouvet Island. A group of sailors landed, but were unable to leave the island in time because of worsened weather and stayed on it for about 3 days. The people were withdrawn by helicopter on 29 November 1958.[24]
  3. ^ The first four climbers (Aaron Halstead, Will Allen, Bruno Rodi and Jason Rodi) were the first humans to climb the highest peak. A time capsule containing the top visions of the future for 2062 was left behind. The next morning, Aaron Halstead led five other climbers (Sarto Blouin, Seth Sherman, Chakib Bouayed, Cindy Sampson, and Akos Hivekovics) to the top.[33]

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[edit]
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54°25′S 3°22′E / 54.42°S 03.36°E / -54.42; 03.36