Futuna (Wallis and Futuna): Difference between revisions
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{{Short description|Island in the Hoorn island group}} |
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{{Multiple issues| |
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{{for|the island in Vanuatu|Futuna Island (Vanuatu)}} |
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{{tone|date=April 2015}} |
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{{Infobox islands|archipelago=[[Hoorn Islands|Îles Horne]]|area_km2=80 |
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{{refimprove|date=April 2015}} |
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|coordinates={{coord|14|16|30|S|178|08|24|W|type:isle|display=inline,title}}|country=[[French overseas departments and territories]]|country_admin_divisions=[[Wallis and Futuna]]|country_admin_divisions_title=Province|country_largest_city=|country_largest_city_population=|density_km2=|elevation_m=524|ethnic_groups=[[Melanesia]]ns|highest_mount=[[Mont Puke]]|location=[[South Pacific Ocean]]|name=Futuna|population=3225|population_as_of=2018|image_caption=The Hoorn Islands Futuna and Alofi. Futuna Island in the northwest.|image_name=File:Futuna alofi.jpg|image_map={{Infobox mapframe |zoom=4}}}} |
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'''Futuna''' ({{IPAc-en|f|uː|ˈ|t|uː|n|ə}}; {{IPA|fr|fu.tu.na|lang}}) is the largest island in [[Hoorn Islands]] or Îles Horne, located in the Pacific Ocean, part of the [[French overseas departments and territories|French overseas collectivity]] (''[[collectivité d'outre-mer]]'') of [[Wallis and Futuna]].<ref name=Szitkar2020>{{harvnb|Szitkar|Dyment|Fouquet|2020|loc=2 Geological Context}}</ref> The island occupies an area of {{Convert|80|km2||-1|abbr=on|adj=on}} and as of 2018 it has a population of 10,912. |
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[[File:Futuna alofi.jpg|thumb|350px|Hoorn Islands (Futuna and Alofi)<br>with Futuna Island in the northwest]] |
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'''Futuna''' ({{IPAc-en|f|uː|ˈ|t|uː|n|ə}}; {{IPA-fr|fu.tu.na|lang}}) is an island in the [[Pacific Ocean]] occupying area of {{Convert|80|km2||-1|abbr=on|adj=on}} with a population of 10,912. It belongs to the [[French overseas departments and territories|French overseas collectivity]] (''[[collectivité d'outre-mer]]'', or ''COM'') of [[Wallis and Futuna]]. It is one of the [[Hoorn Islands]] or '''Îles Horne'''; nearby [[Alofi Island|Alofi]] is the other. They are both remnants of the same ancient, [[extinct volcano]], now bordered with a [[fringing reef]]. Futuna has a maximum elevation of {{Convert|500|m||abbr=on}}. |
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==History== |
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⚫ | Futuna and Alofi were first mapped by Europeans in 1616 by [[Willem Schouten]] and [[Jacob Le Maire]] during their [[circumnavigation]] of the globe on the ship ''Eendracht''. After sailing to [[Niuafo'ou|Niuafo{{okina}}ou]], they suddenly changed course from west to northwest and discovered the two islands. The islands were named Hoorn Eylanden, after the city of [[Hoorn]], Schouten's birthplace. This became ''Horne'' in French and English. They also discovered a natural harbor along the southwest coast of Futuna, which they named Eendrachts baai (Unity Bay) after their ship. It is thought that their landing place was the site of the Anse de Sigave near what is today called Leava. |
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⚫ | Schouten and Le Maire had learned from earlier experiences how to approach islanders successfully. Upon landing, they went ashore, and, when approached by some of the natives, they made a show of force. This opened the way for a peaceful barter, with the natives offering coconuts, yams, and hogs in exchange for the sailors’ iron nails, beads and knives. The sailors went on to get fresh water and meet the king, who told his subjects that their guests were not to be disturbed by petty thieving. This way, the [[Netherlands|Dutch]] sailors were able to replenish their stocks without risk of theft. A few days after they arrived, the king of the other island, Alofi, came to visit, bringing with him 300 men. A feast was prepared and a [[kava]] ceremony and [[Earth oven|{{okina}}umu]] were organised. Schouten and Le Maire were likely the first Europeans to witness these ceremonies. |
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⚫ | Without the risk of theft or hostilities, Schouten and Le Maire were able to study Futuna more thoroughly than had been possible for them in the case of the [[Niuatoputapu|Niua]] islands. They did not visit Alofi. Their description of the islanders’ appearance and behavior was not flattering. Although they praise the men for being well-proportioned, they found the women ugly and ill-shaped, with breasts hanging down to their bellies like empty satchels. The people were said to all go naked, and to copulate in public, even in front of their king. |
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⚫ | In the 19th century, [[whaling]] ships from the [[United States]] and elsewhere called at Futuna for water, wood, and food. The first one known to have called was the ''Independence'' in 1827.<ref>Robert Langdon (ed.) Where the whalers went: an index to the Pacific ports and islands visited by American whalers (and some other ships) in the 19th century, Canberra, Pacific Manuscripts Bureau, 1984, p.32.</ref> |
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==Geography== |
==Geography== |
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Futuna and Alofi are both remnants of the same [[extinct volcano]], now bordering with a [[fringing reef]]. Futuna's highest point is [[Mont Puke]] at {{Convert|524|m||abbr=on}} above sea level,<ref name=CIA>{{cite web|url=https://www.cia.gov/the-world-factbook/countries/wallis-and-futuna/ |title=The World Factbook:Wallis and Futuna|access-date=21 October 2023}}</ref> and the island has an area of {{Convert|83|km2||abbr=on|adj=on}},<ref name=Goff2011s>{{harvnb|Goff|Lamarche|Pelletier|Chagué-Goff|2011|loc=Setting}}</ref> with {{Convert|53|km2||abbr=on|adj=on}} in Sigave and {{Convert|30|km2||abbr=on|adj=on}} in Alo. It is separated from [[Wallis (island)|Wallis Island]] to the north by water deeper than {{convert|4500|m|abbr=on}} in the [[Vitiaz Trench]].<ref name=Szitkar2020/> |
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===Geology=== |
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Futuna island has large [[Upper Pliocene]] volcanic lava flows, as well as breccias and [[hyaloclastite]] deposits from underwater eruptions.<ref name=Szitkar2020/> |
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===Tectonics=== |
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Futuna is on the Futuna Ridge (Futuna–Alofi volcanic ridge) that lies along a boundary of interaction between the colliding [[Pacific plate|Pacific]] and [[Australia plate]], between the North Fiji transform fault to the south and the now inactive tectonically Vitiaz Trench.<ref name=Goff2011t>{{harvnb|Goff|Lamarche|Pelletier|Chagué-Goff|2011|loc=Tectonics}}</ref><ref name=Szitkar2020/> However the full tectonic role of the ridge and associated features is still not understood.<ref name=Szitkar2022r>{{harvnb|Szitkar|Dyment|Pelleter|Thomas|2022|loc= 2. Regional geological context}}</ref> As recently as March 2000 this ridge was discovered to be a spreading center extending over a distance of more than {{convert|200|km|abbr=on}} from the north of [[Fiji]] to the northwest of Futuna Island and a boundary of the [[Futuna plate]] which is a slightly ill defined microplate with triple junctions with the Pacific and Australian plates. The northern part of the ridge contains basaltic volcanoes such as Utu Uli that are younger than 780,000 years old and at depths of more than {{convert|1000|m|abbr=on}} precluding exposive eruptions, so that their eruptions are effusive.<ref name=Szitkar2022c>{{harvnb|Szitkar|Dyment|Pelleter|Thomas|2022|loc=5. Disscussion, 6.Conclusion}}</ref> There is a {{convert|30|km|abbr=on}} wide area of seafloor to the east of Futuna, with a WSW-ENE orientation, and with many volcanoes known as the South-East Futuna Volcanic Zone (SEFVZ).<ref name=Szitkar2020/> This contains the significant volcanoes of Ono, Tasi Tulo, Fatu Kapa and Kulo Lasi all south of the Vitiaz Trench.<ref name=Szitkar2020/> The young seafloor produced by these volcanoes in the SEFVZ means that the past tectonics is poorly understood as timings from say magnetic field changes cannot be obtained. The area is interacting with the spreading centers in the [[Lau Basin]] further to the east and southeast. |
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===Tsunami risk=== |
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The island was affected by the [[2009 Samoa earthquake and tsunami]] with a run up height to {{convert|4.4|m|abbr=on}} and up to {{convert|95|m|abbr=on}} inland inundation.<ref name=Goff2011i>{{harvnb|Goff|Lamarche|Pelletier|Chagué-Goff|2011|loc=Introduction}}</ref> Studies afterwards revealed past tsunami events have occurred.<ref name=Goff2011c>{{harvnb|Goff|Lamarche|Pelletier|Chagué-Goff|2011|loc=Abstract,Conclusions}}</ref> |
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===Climate=== |
===Climate=== |
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Futuna (Maopoopo weather station) has a [[tropical rainforest climate]] ([[Köppen climate classification]] ''Af''). The average annual temperature in Maopoopo is {{cvt|27. |
Futuna (Maopoopo weather station) has a [[tropical rainforest climate]] ([[Köppen climate classification]] ''Af''). The average annual temperature in Maopoopo is {{cvt|27.5|C}}. The average annual rainfall is {{cvt|3333.6|mm}} with December as the wettest month. The temperatures are highest on average in February, at around {{cvt|28.2|C}}, and lowest in August, at around {{convert|26.5|C}}. The highest temperature ever recorded in Maopoopo was {{cvt|35.8|C}} on 10 January 2016; the coldest temperature ever recorded was {{cvt|19.0|C}} on 12 August 1980. |
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{{Weather box |
{{Weather box |
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|location = Futuna (Maopoopo weather station |
|location = Futuna <small>(Maopoopo weather station, 1991–2020 averages, extremes 1979−present)</small> |
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|metric first = yes |
|metric first = yes |
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|single line = yes |
|single line = yes |
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Line 34: | Line 47: | ||
|Dec record high C = 34.6 |
|Dec record high C = 34.6 |
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|year record high C = 35.8 |
|year record high C = 35.8 |
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|Jan high C = |
|Jan high C = 31.2 |
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|Feb high C = |
|Feb high C = 31.2 |
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|Mar high C = |
|Mar high C = 31.1 |
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|Apr high C = 30. |
|Apr high C = 30.7 |
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|May high C = 29. |
|May high C = 29.9 |
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|Jun high C = |
|Jun high C = 29.1 |
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|Jul high C = 28. |
|Jul high C = 28.6 |
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|Aug high C = 28. |
|Aug high C = 28.7 |
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|Sep high C = |
|Sep high C = 29.2 |
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|Oct high C = 29. |
|Oct high C = 29.7 |
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|Nov high C = 30. |
|Nov high C = 30.4 |
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|Dec high C = 30. |
|Dec high C = 30.9 |
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|year high C = |
|year high C = 30.1 |
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|Jan mean C = |
|Jan mean C = 28.2 |
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|Feb mean C = |
|Feb mean C = 28.2 |
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|Mar mean C = |
|Mar mean C = 28.2 |
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|Apr mean C = 27. |
|Apr mean C = 27.9 |
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|May mean C = 27. |
|May mean C = 27.4 |
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|Jun mean C = |
|Jun mean C = 27.0 |
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|Jul mean C = 26. |
|Jul mean C = 26.5 |
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|Aug mean C = 26. |
|Aug mean C = 26.5 |
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|Sep mean C = 26. |
|Sep mean C = 26.8 |
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|Oct mean C = |
|Oct mean C = 27.1 |
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|Nov mean C = 27. |
|Nov mean C = 27.6 |
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|Dec mean C = |
|Dec mean C = 28.0 |
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|year mean C = 27. |
|year mean C = 27.5 |
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|Jan low C = |
|Jan low C = 25.2 |
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|Feb low C = 25. |
|Feb low C = 25.2 |
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|Mar low C = |
|Mar low C = 25.2 |
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|Apr low C = |
|Apr low C = 25.2 |
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|May low C = 24. |
|May low C = 24.9 |
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|Jun low C = 24. |
|Jun low C = 24.8 |
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|Jul low C = 24. |
|Jul low C = 24.3 |
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|Aug low C = |
|Aug low C = 24.2 |
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|Sep low C = 24. |
|Sep low C = 24.4 |
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|Oct low C = 24. |
|Oct low C = 24.5 |
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|Nov low C = 24. |
|Nov low C = 24.8 |
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|Dec low C = |
|Dec low C = 25.1 |
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|year low C = 24. |
|year low C = 24.8 |
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|Jan record low C = 21.3 |
|Jan record low C = 21.3 |
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|Feb record low C = 21.9 |
|Feb record low C = 21.9 |
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Line 87: | Line 100: | ||
|year record low C = 19.0 |
|year record low C = 19.0 |
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|precipitation colour = green |
|precipitation colour = green |
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|Jan precipitation mm = |
|Jan precipitation mm = 329.2 |
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|Feb precipitation mm = |
|Feb precipitation mm = 354.1 |
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|Mar precipitation mm = |
|Mar precipitation mm = 341.3 |
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|Apr precipitation mm = |
|Apr precipitation mm = 308.3 |
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|May precipitation mm = |
|May precipitation mm = 262.6 |
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|Jun precipitation mm = |
|Jun precipitation mm = 185.6 |
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|Jul precipitation mm = |
|Jul precipitation mm = 175.1 |
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|Aug precipitation mm = |
|Aug precipitation mm = 181.8 |
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|Sep precipitation mm = |
|Sep precipitation mm = 225.6 |
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|Oct precipitation mm = |
|Oct precipitation mm = 244.2 |
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|Nov precipitation mm = |
|Nov precipitation mm = 324.1 |
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|Dec precipitation mm = |
|Dec precipitation mm = 401.7 |
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|year precipitation mm = |
|year precipitation mm = 3333.6 |
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|unit precipitation days = 1.0 mm |
|unit precipitation days = 1.0 mm |
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|Jan precipitation days = |
|Jan precipitation days = 19.7 |
||
|Feb precipitation days = 18. |
|Feb precipitation days = 18.7 |
||
|Mar precipitation days = 20. |
|Mar precipitation days = 20.5 |
||
|Apr precipitation days = 19. |
|Apr precipitation days = 19.1 |
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|May precipitation days = |
|May precipitation days = 16.2 |
||
|Jun precipitation days = |
|Jun precipitation days = 14.7 |
||
|Jul precipitation days = 13. |
|Jul precipitation days = 13.9 |
||
|Aug precipitation days = |
|Aug precipitation days = 14.5 |
||
|Sep precipitation days = |
|Sep precipitation days = 15.2 |
||
|Oct precipitation days = |
|Oct precipitation days = 16.7 |
||
|Nov precipitation days = |
|Nov precipitation days = 18.2 |
||
|Dec precipitation days = |
|Dec precipitation days = 20.1 |
||
|year precipitation days = |
|year precipitation days = 207.6 |
||
|Jan sun = |
|Jan sun = 175.7 |
||
|Feb sun = |
|Feb sun = 160.2 |
||
|Mar sun = n/a |
|Mar sun = n/a |
||
|Apr sun = |
|Apr sun = 154.4 |
||
|May sun = |
|May sun = n/a |
||
|Jun sun = |
|Jun sun = 120.1 |
||
|Jul sun = |
|Jul sun = 121.3 |
||
|Aug sun = |
|Aug sun = 125.5 |
||
|Sep sun = |
|Sep sun = 135.0 |
||
|Oct sun = |
|Oct sun = 154.9 |
||
|Nov sun = |
|Nov sun = 165.8 |
||
|Dec sun = |
|Dec sun = 180.3 |
||
|year sun = n/a |
|year sun = n/a |
||
|source 1 = [[Météo France]]<ref>{{cite web |url=https://donneespubliques.meteofrance.fr/FichesClim/FICHECLIM_98611001.pdf |title=Climate of Maopoopo 1991-2020 |language=fr |publisher=[[Météo-France]] |access-date=August 26, 2022 |archive-date=November 3, 2022 |archive-url=https://web.archive.org/web/20221103174813/https://donneespubliques.meteofrance.fr/FichesClim/FICHECLIM_98611001.pdf |url-status=live }}</ref>}} |
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|source 1 = [[Météo France]]<ref>{{cite web |
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| url = https://donneespubliques.meteofrance.fr/FichesClim/FICHECLIM_98611001.pdf |
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| title=Climate of Maopoopo 1981-2010 |
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| language = fr |
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| publisher = [[Météo-France]] |
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| access-date = June 3, 2022}}</ref>}} |
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== |
== Demographics == |
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As of the 2018 [[census]], the population of the island was 3,225, with 1,950 residing in the [[Alo (Wallis and Futuna)|Alo]] district and 1,275 in [[Sigave]]. Futuna makes up approximately 27.9% of the population of Wallis and Futuna.<ref>{{Cite web |date= |title=Les populations légales de Wallis et Futuna en 2018 |url=https://www.insee.fr/fr/statistiques/3685976?sommaire=2121453 |access-date=2023-05-16 |archive-date=2019-04-14 |archive-url=https://web.archive.org/web/20190414053320/https://www.insee.fr/fr/statistiques/3685976?sommaire=2121453 |url-status=live }}</ref> The most spoken languages on Futuna are [[Futunan]] (94.5%), French (5.3%), and [[Wallisian]] (0.2%).<ref>{{Cite web |title="Recensement 2018 - Tableau Pop_06_6 : Population selon le sexe, la langue la plus couramment parlée en famille, l'âge décennal et par village de résidence" |url=https://www.statistique.wf/download/43/recensement-2018/1157/principaux_tableaux_population_2018.ods |access-date=2023-05-16 |archive-date=2023-05-20 |archive-url=https://web.archive.org/web/20230520134633/https://www.statistique.wf/download/43/recensement-2018/1157/principaux_tableaux_population_2018.ods |url-status=live }}</ref> |
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⚫ | Futuna and Alofi were |
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⚫ | Schouten and Le Maire had learned from earlier experiences how to approach islanders successfully. Upon landing, they went ashore, and, when approached by some of the natives, they made a show of force. This opened the way a peaceful barter, with the natives offering coconuts, yams and hogs in exchange for the sailors’ iron nails, beads and knives. |
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⚫ | |||
⚫ | In the 19th century, [[whaling]] ships from the [[United States]] and elsewhere called at Futuna for water, wood and food. The first one known to have called was the ''Independence'' in 1827.<ref>Robert Langdon (ed.) Where the whalers went: an index to the Pacific ports and islands visited by American whalers (and some other ships) in the 19th century, Canberra, Pacific Manuscripts Bureau, 1984, p.32.</ref> |
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==Culture== |
==Culture == |
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[[File:Futuna and Alofi.jpg|thumb|Futuna and Alofi (photo: NASA)]] |
[[File:Futuna and Alofi.jpg|thumb|Futuna and Alofi (photo: NASA)]] |
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Two kings, elected from the local nobility every few years, rule the population in conjunction with French authorities. They are the king of Sigave, the western province, and the king of Alo, the eastern province including Alofi. Except for Poi all villages are along the southwest coast, and they are from west to east: Toloke, Fiua, Vaisei, Nuku, and Leava (capital with the wharf) in Sigave, and Taoa, Mala{{okina}}e, Ono, Kolia and Vele (at the airstrip) in Alo. |
Two kings, elected from the local nobility every few years, rule the population in conjunction with French authorities. They are the king of Sigave, the western province, and the king of Alo, the eastern province including Alofi. Except for Poi all villages are along the southwest coast, and they are from west to east: Toloke, Fiua, Vaisei, Nuku, and Leava (capital with the wharf) in Sigave, and Taoa, Mala{{okina}}e, Ono, Kolia and Vele (at the airstrip) in Alo. |
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99% of the population of Wallis and Futuna are Catholic.<ref>{{cite web |title=Wallis and Futuna |url=https://www.cia.gov/the-world-factbook/countries/wallis-and-futuna/ |publisher=CIA World Factbook |access-date=18 June 2022}}</ref> Although the island is closer to [[Tonga]] and farther from [[Samoa]] than {{okina}}Uvea, the vernacular and culture are more Samoan |
99% of the population of Wallis and Futuna are Catholic.<ref>{{cite web |title=Wallis and Futuna |url=https://www.cia.gov/the-world-factbook/countries/wallis-and-futuna/ |publisher=CIA World Factbook |access-date=18 June 2022 |archive-date=24 April 2021 |archive-url=https://web.archive.org/web/20210424005145/https://www.cia.gov/the-world-factbook/countries/wallis-and-futuna |url-status=live }}</ref> Although the island is closer to [[Tonga]] and farther from [[Samoa]] than {{okina}}Uvea, the vernacular and culture are more Samoan. |
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==Education== |
==Education== |
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There are six primary schools on Futuna.<ref name="Educ">"[http://www.wallis-et-futuna.pref.gouv.fr/content/download/930/6048/file/Livret%20d'accueil%20version%20site%20final%202.pdf LIVRET D'ACCUEIL Wallis et Futuna]." Wallis and Futuna. p. 22 (22/28). Retrieved on September 14, 2016.</ref> The island also has two junior high schools (''collèges''): Fiua de Sigave and Sisia d'Ono. Residents are served by a senior high school/sixth-form college, [[Lycée d'Etat de Wallis et Futuna]], on Wallis.<ref>"[https://web.archive.org/web/20160624145135/https://www.ac-wf.wf/-Colleges-Lycee-.html Cartographie des établissements du second degré]." Wallis and Futuna. June 24, 2016. Retrieved on September 14, 2016.</ref> |
There are six primary schools on Futuna.<ref name="Educ">"[http://www.wallis-et-futuna.pref.gouv.fr/content/download/930/6048/file/Livret%20d'accueil%20version%20site%20final%202.pdf LIVRET D'ACCUEIL Wallis et Futuna] {{Webarchive|url=https://web.archive.org/web/20171010195840/http://www.wallis-et-futuna.pref.gouv.fr/content/download/930/6048/file/Livret%20d%27accueil%20version%20site%20final%202.pdf |date=2017-10-10 }}." Wallis and Futuna. p. 22 (22/28). Retrieved on September 14, 2016.</ref> The island also has two junior high schools (''collèges''): Fiua de Sigave and Sisia d'Ono. Residents are served by a senior high school/sixth-form college, [[Lycée d'Etat de Wallis et Futuna]], on Wallis.<ref>"[https://web.archive.org/web/20160624145135/https://www.ac-wf.wf/-Colleges-Lycee-.html Cartographie des établissements du second degré]." Wallis and Futuna. June 24, 2016. Retrieved on September 14, 2016.</ref> |
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==See also== |
==See also== |
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* |
*[[Pointe Vele Airport]] |
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* |
*[[Peter Chanel]] |
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*[[Customary kingdoms of Wallis and Futuna]] |
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==References== |
==References== |
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*https://www.worldometers.info/world-population/wallis-and-futuna-islands-population/ |
*https://www.worldometers.info/world-population/wallis-and-futuna-islands-population/ |
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*Robert Kerr (1824): [http://www.gutenberg.org/files/13130/13130-h/13130-h.htm#chapter4-6 Voyage round the world, in 1615-1617, by William Cornelison Schouten and Jacques le Maire, going round Cape Horn.] The comments of the editor to the original ship's journals are completely wrong, however. |
*Robert Kerr (1824): [http://www.gutenberg.org/files/13130/13130-h/13130-h.htm#chapter4-6 Voyage round the world, in 1615-1617, by William Cornelison Schouten and Jacques le Maire, going round Cape Horn.] The comments of the editor to the original ship's journals are completely wrong, however. |
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*[[Percy Smith (ethnologist)|Percy Smith]] (1892): [http://www.jps.auckland.ac.nz/document/Volume_1_1892/Volume_1%2C_No._1%2C_1892/Futuna%2C_or_Horne_Island_and_its_people%2C_p.33-52/p1?action=null "Futuna; or, Horne Island and its People"], ''Journal of the [[Polynesian Society]]'', vol.1, pp. 33–52 |
*[[Percy Smith (ethnologist)|Percy Smith]] (1892): [http://www.jps.auckland.ac.nz/document/Volume_1_1892/Volume_1%2C_No._1%2C_1892/Futuna%2C_or_Horne_Island_and_its_people%2C_p.33-52/p1?action=null "Futuna; or, Horne Island and its People"] {{Webarchive|url=https://web.archive.org/web/20180204212223/http://www.jps.auckland.ac.nz/document/Volume_1_1892/Volume_1%2C_No._1%2C_1892/Futuna%2C_or_Horne_Island_and_its_people%2C_p.33-52/p1?action=null |date=2018-02-04 }}, ''Journal of the [[Polynesian Society]]'', vol.1, pp. 33–52 |
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*{{cite journal| last1=Goff | first1=J| last2=Lamarche |first2=G| last3=Pelletier| first3=B| last4=Chagué-Goff| first4=C| last5=Strotz| first5=L| title=Predecessors to the 2009 South Pacific tsunami in the Wallis and Futuna archipelago| journal=Earth-Science Reviews| year=2011 | volume=107| issue=1–2| pages=91–106| doi=10.1016/j.earscirev.2010.11.003| bibcode=2011ESRv..107...91G}}<!---{{harvnb|Goff|Lamarche|Pelletier|Chagué-Goff|2011}}---> |
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*{{cite journal| last1=Szitkar | first1=F| last2=Dyment |first2=J| last3= Fouquet| first3= Y|title= Widespread volcanism Southeast of Futuna Island (SW Pacific Ocean): Near-seafloor magnetic dating and regional consequences| journal= Journal of Volcanology and Geothermal Research| date=15 November 2020| volume=406| issue=107064|doi= 10.1016/j.jvolgeores.2020.107064| bibcode=2020JVGR..40607064S| doi-access=free}} <!--{{harvnb|Szitkar|Dyment|Fouquet|2020}} ----> |
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*{{cite journal| last1 = Szitkar | first1 = F | last2 = Dyment | first2 = J | last3 = Pelleter | first3 =E | last4 = Thomas | first4 =Y | last5 = Marsset | first5 =B | last6 = Ker | first6 =S | last7 = Fouquet | first7 =Y | title= Effusive and explosive volcanism on the northern Futuna Ridge, Lau Basin: A combined bathymetric, magnetic and seismic investigation | journal=Journal of Volcanology and Geothermal Research| year = 2022 | volume = 431 |issue=107646 | doi=10.1016/j.jvolgeores.2022.107646| bibcode = 2022JVGR..43107646S | doi-access = free }}<!-- {{harvnb|Szitkar|Dyment|Pelleter|Thomas|2022}} --> |
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Latest revision as of 19:54, 24 December 2024
Geography | |
---|---|
Location | South Pacific Ocean |
Coordinates | 14°16′30″S 178°08′24″W / 14.27500°S 178.14000°W |
Archipelago | Îles Horne |
Area | 80 km2 (31 sq mi) |
Highest elevation | 524 m (1719 ft) |
Highest point | Mont Puke |
Administration | |
Province | Wallis and Futuna |
Demographics | |
Population | 3225 (2018) |
Ethnic groups | Melanesians |
Futuna (/fuːˈtuːnə/; French: [fu.tu.na]) is the largest island in Hoorn Islands or Îles Horne, located in the Pacific Ocean, part of the French overseas collectivity (collectivité d'outre-mer) of Wallis and Futuna.[1] The island occupies an area of 80 km2 (30 sq mi) and as of 2018 it has a population of 10,912.
Futuna takes its name from an endonym derived from the local futu, meaning fish-poison tree.[2]
History
[edit]Futuna and Alofi were first mapped by Europeans in 1616 by Willem Schouten and Jacob Le Maire during their circumnavigation of the globe on the ship Eendracht. After sailing to Niuafoʻou, they suddenly changed course from west to northwest and discovered the two islands. The islands were named Hoorn Eylanden, after the city of Hoorn, Schouten's birthplace. This became Horne in French and English. They also discovered a natural harbor along the southwest coast of Futuna, which they named Eendrachts baai (Unity Bay) after their ship. It is thought that their landing place was the site of the Anse de Sigave near what is today called Leava.
Schouten and Le Maire had learned from earlier experiences how to approach islanders successfully. Upon landing, they went ashore, and, when approached by some of the natives, they made a show of force. This opened the way for a peaceful barter, with the natives offering coconuts, yams, and hogs in exchange for the sailors’ iron nails, beads and knives. The sailors went on to get fresh water and meet the king, who told his subjects that their guests were not to be disturbed by petty thieving. This way, the Dutch sailors were able to replenish their stocks without risk of theft. A few days after they arrived, the king of the other island, Alofi, came to visit, bringing with him 300 men. A feast was prepared and a kava ceremony and ʻumu were organised. Schouten and Le Maire were likely the first Europeans to witness these ceremonies.
Without the risk of theft or hostilities, Schouten and Le Maire were able to study Futuna more thoroughly than had been possible for them in the case of the Niua islands. They did not visit Alofi. Their description of the islanders’ appearance and behavior was not flattering. Although they praise the men for being well-proportioned, they found the women ugly and ill-shaped, with breasts hanging down to their bellies like empty satchels. The people were said to all go naked, and to copulate in public, even in front of their king.
In the 19th century, whaling ships from the United States and elsewhere called at Futuna for water, wood, and food. The first one known to have called was the Independence in 1827.[3]
Geography
[edit]Futuna and Alofi are both remnants of the same extinct volcano, now bordering with a fringing reef. Futuna's highest point is Mont Puke at 524 m (1,719 ft) above sea level,[2] and the island has an area of 83 km2 (32 sq mi),[4] with 53 km2 (20 sq mi) in Sigave and 30 km2 (12 sq mi) in Alo. It is separated from Wallis Island to the north by water deeper than 4,500 m (14,800 ft) in the Vitiaz Trench.[1]
Geology
[edit]Futuna island has large Upper Pliocene volcanic lava flows, as well as breccias and hyaloclastite deposits from underwater eruptions.[1]
Tectonics
[edit]Futuna is on the Futuna Ridge (Futuna–Alofi volcanic ridge) that lies along a boundary of interaction between the colliding Pacific and Australia plate, between the North Fiji transform fault to the south and the now inactive tectonically Vitiaz Trench.[5][1] However the full tectonic role of the ridge and associated features is still not understood.[6] As recently as March 2000 this ridge was discovered to be a spreading center extending over a distance of more than 200 km (120 mi) from the north of Fiji to the northwest of Futuna Island and a boundary of the Futuna plate which is a slightly ill defined microplate with triple junctions with the Pacific and Australian plates. The northern part of the ridge contains basaltic volcanoes such as Utu Uli that are younger than 780,000 years old and at depths of more than 1,000 m (3,300 ft) precluding exposive eruptions, so that their eruptions are effusive.[7] There is a 30 km (19 mi) wide area of seafloor to the east of Futuna, with a WSW-ENE orientation, and with many volcanoes known as the South-East Futuna Volcanic Zone (SEFVZ).[1] This contains the significant volcanoes of Ono, Tasi Tulo, Fatu Kapa and Kulo Lasi all south of the Vitiaz Trench.[1] The young seafloor produced by these volcanoes in the SEFVZ means that the past tectonics is poorly understood as timings from say magnetic field changes cannot be obtained. The area is interacting with the spreading centers in the Lau Basin further to the east and southeast.
Tsunami risk
[edit]The island was affected by the 2009 Samoa earthquake and tsunami with a run up height to 4.4 m (14 ft) and up to 95 m (312 ft) inland inundation.[8] Studies afterwards revealed past tsunami events have occurred.[9]
Climate
[edit]Futuna (Maopoopo weather station) has a tropical rainforest climate (Köppen climate classification Af). The average annual temperature in Maopoopo is 27.5 °C (81.5 °F). The average annual rainfall is 3,333.6 mm (131.24 in) with December as the wettest month. The temperatures are highest on average in February, at around 28.2 °C (82.8 °F), and lowest in August, at around 26.5 °C (79.7 °F). The highest temperature ever recorded in Maopoopo was 35.8 °C (96.4 °F) on 10 January 2016; the coldest temperature ever recorded was 19.0 °C (66.2 °F) on 12 August 1980.
Climate data for Futuna (Maopoopo weather station, 1991–2020 averages, extremes 1979−present) | |||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
Record high °C (°F) | 35.8 (96.4) |
35.0 (95.0) |
34.2 (93.6) |
33.9 (93.0) |
33.4 (92.1) |
32.6 (90.7) |
31.9 (89.4) |
32.3 (90.1) |
33.0 (91.4) |
33.9 (93.0) |
33.8 (92.8) |
34.6 (94.3) |
35.8 (96.4) |
Mean daily maximum °C (°F) | 31.2 (88.2) |
31.2 (88.2) |
31.1 (88.0) |
30.7 (87.3) |
29.9 (85.8) |
29.1 (84.4) |
28.6 (83.5) |
28.7 (83.7) |
29.2 (84.6) |
29.7 (85.5) |
30.4 (86.7) |
30.9 (87.6) |
30.1 (86.2) |
Daily mean °C (°F) | 28.2 (82.8) |
28.2 (82.8) |
28.2 (82.8) |
27.9 (82.2) |
27.4 (81.3) |
27.0 (80.6) |
26.5 (79.7) |
26.5 (79.7) |
26.8 (80.2) |
27.1 (80.8) |
27.6 (81.7) |
28.0 (82.4) |
27.5 (81.5) |
Mean daily minimum °C (°F) | 25.2 (77.4) |
25.2 (77.4) |
25.2 (77.4) |
25.2 (77.4) |
24.9 (76.8) |
24.8 (76.6) |
24.3 (75.7) |
24.2 (75.6) |
24.4 (75.9) |
24.5 (76.1) |
24.8 (76.6) |
25.1 (77.2) |
24.8 (76.6) |
Record low °C (°F) | 21.3 (70.3) |
21.9 (71.4) |
21.2 (70.2) |
21.8 (71.2) |
20.9 (69.6) |
21.5 (70.7) |
20.1 (68.2) |
19.0 (66.2) |
19.5 (67.1) |
20.7 (69.3) |
20.9 (69.6) |
20.6 (69.1) |
19.0 (66.2) |
Average precipitation mm (inches) | 329.2 (12.96) |
354.1 (13.94) |
341.3 (13.44) |
308.3 (12.14) |
262.6 (10.34) |
185.6 (7.31) |
175.1 (6.89) |
181.8 (7.16) |
225.6 (8.88) |
244.2 (9.61) |
324.1 (12.76) |
401.7 (15.81) |
3,333.6 (131.24) |
Average precipitation days (≥ 1.0 mm) | 19.7 | 18.7 | 20.5 | 19.1 | 16.2 | 14.7 | 13.9 | 14.5 | 15.2 | 16.7 | 18.2 | 20.1 | 207.6 |
Mean monthly sunshine hours | 175.7 | 160.2 | — | 154.4 | — | 120.1 | 121.3 | 125.5 | 135.0 | 154.9 | 165.8 | 180.3 | — |
Source: Météo France[10] |
Demographics
[edit]As of the 2018 census, the population of the island was 3,225, with 1,950 residing in the Alo district and 1,275 in Sigave. Futuna makes up approximately 27.9% of the population of Wallis and Futuna.[11] The most spoken languages on Futuna are Futunan (94.5%), French (5.3%), and Wallisian (0.2%).[12]
Culture
[edit]Two kings, elected from the local nobility every few years, rule the population in conjunction with French authorities. They are the king of Sigave, the western province, and the king of Alo, the eastern province including Alofi. Except for Poi all villages are along the southwest coast, and they are from west to east: Toloke, Fiua, Vaisei, Nuku, and Leava (capital with the wharf) in Sigave, and Taoa, Malaʻe, Ono, Kolia and Vele (at the airstrip) in Alo.
99% of the population of Wallis and Futuna are Catholic.[13] Although the island is closer to Tonga and farther from Samoa than ʻUvea, the vernacular and culture are more Samoan.
Futuna is where Pierre Chanel was martyred in 1841, becoming Polynesia's only Catholic saint. The cathedral of Poi now stands on the site where he was martyred.
Education
[edit]There are six primary schools on Futuna.[14] The island also has two junior high schools (collèges): Fiua de Sigave and Sisia d'Ono. Residents are served by a senior high school/sixth-form college, Lycée d'Etat de Wallis et Futuna, on Wallis.[15]
See also
[edit]References
[edit]- ^ a b c d e f Szitkar, Dyment & Fouquet 2020, 2 Geological Context
- ^ a b "The World Factbook:Wallis and Futuna". Retrieved 21 October 2023.
- ^ Robert Langdon (ed.) Where the whalers went: an index to the Pacific ports and islands visited by American whalers (and some other ships) in the 19th century, Canberra, Pacific Manuscripts Bureau, 1984, p.32.
- ^ Goff et al. 2011, Setting
- ^ Goff et al. 2011, Tectonics
- ^ Szitkar et al. 2022, 2. Regional geological context
- ^ Szitkar et al. 2022, 5. Disscussion, 6.Conclusion
- ^ Goff et al. 2011, Introduction
- ^ Goff et al. 2011, Abstract,Conclusions
- ^ "Climate of Maopoopo 1991-2020" (PDF) (in French). Météo-France. Archived (PDF) from the original on November 3, 2022. Retrieved August 26, 2022.
- ^ "Les populations légales de Wallis et Futuna en 2018". Archived from the original on 2019-04-14. Retrieved 2023-05-16.
- ^ ""Recensement 2018 - Tableau Pop_06_6 : Population selon le sexe, la langue la plus couramment parlée en famille, l'âge décennal et par village de résidence"". Archived from the original on 2023-05-20. Retrieved 2023-05-16.
- ^ "Wallis and Futuna". CIA World Factbook. Archived from the original on 24 April 2021. Retrieved 18 June 2022.
- ^ "LIVRET D'ACCUEIL Wallis et Futuna Archived 2017-10-10 at the Wayback Machine." Wallis and Futuna. p. 22 (22/28). Retrieved on September 14, 2016.
- ^ "Cartographie des établissements du second degré." Wallis and Futuna. June 24, 2016. Retrieved on September 14, 2016.
References
[edit]- Cartes institut géographique national (4902F)
- https://www.worldometers.info/world-population/wallis-and-futuna-islands-population/
- Robert Kerr (1824): Voyage round the world, in 1615-1617, by William Cornelison Schouten and Jacques le Maire, going round Cape Horn. The comments of the editor to the original ship's journals are completely wrong, however.
- Percy Smith (1892): "Futuna; or, Horne Island and its People" Archived 2018-02-04 at the Wayback Machine, Journal of the Polynesian Society, vol.1, pp. 33–52
- Goff, J; Lamarche, G; Pelletier, B; Chagué-Goff, C; Strotz, L (2011). "Predecessors to the 2009 South Pacific tsunami in the Wallis and Futuna archipelago". Earth-Science Reviews. 107 (1–2): 91–106. Bibcode:2011ESRv..107...91G. doi:10.1016/j.earscirev.2010.11.003.
- Szitkar, F; Dyment, J; Fouquet, Y (15 November 2020). "Widespread volcanism Southeast of Futuna Island (SW Pacific Ocean): Near-seafloor magnetic dating and regional consequences". Journal of Volcanology and Geothermal Research. 406 (107064). Bibcode:2020JVGR..40607064S. doi:10.1016/j.jvolgeores.2020.107064.
- Szitkar, F; Dyment, J; Pelleter, E; Thomas, Y; Marsset, B; Ker, S; Fouquet, Y (2022). "Effusive and explosive volcanism on the northern Futuna Ridge, Lau Basin: A combined bathymetric, magnetic and seismic investigation". Journal of Volcanology and Geothermal Research. 431 (107646). Bibcode:2022JVGR..43107646S. doi:10.1016/j.jvolgeores.2022.107646.