Futuna (Wallis and Futuna)

Short description: Island in the Hoorn island group

Futuna

The Hoorn Islands Futuna and Alofi. Futuna Island in the northwest.

Geography
Location| South Pacific Ocean
Coordinates|  [ ⚑ ] : 14°16′30″S 178°08′24″W﻿ / ﻿14.275°S 178.14°W﻿ / -14.275; -178.14
Archipelago| Îles Horne
Area| 80 km2 (31 sq mi)
Highest elevation| 524 m (1719 ft)
Highest point| Mont Puke
Administration

French overseas departments and territories

Province| Wallis and Futuna
Demographics
Population| 3225 (2018)
Ethnic groups| Melanesians
The Hoorn Islands.

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]

## Contents

* 1 History
* 2 Geography
* 2.1 Geology
* 2.2 Tectonics
* 2.3 Tsunami risk
* 2.4 Climate
* 3 Demographics
* 4 Culture
* 5 Education
* 6 See also
* 7 References
* 8 References

## History

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

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

Futuna island has large Upper Pliocene volcanic lava flows, as well as breccias and hyaloclastite deposits from underwater eruptions.[1]

### Tectonics

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

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

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. Script error: No such module "weather box".

## Demographics

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

Futuna and Alofi (photo: NASA)

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

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

* Pointe Vele Airport
* Peter Chanel

## References

1. ↑ 1.0 1.1 1.2 1.3 1.4 1.5 Szitkar, Dyment & Fouquet 2020, 2 Geological Context
2. ↑ 2.0 2.1 "The World Factbook:Wallis and Futuna". https://www.cia.gov/the-world-factbook/countries/wallis-and-futuna/.
3. ↑ 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.
4. ↑ Goff et al. 2011, Setting
5. ↑ Goff et al. 2011, Tectonics
6. ↑ Szitkar et al. 2022, 2. Regional geological context
7. ↑ Szitkar et al. 2022, 5. Disscussion, 6.Conclusion
8. ↑ Goff et al. 2011, Introduction
9. ↑ Goff et al. 2011, Abstract,Conclusions
10. ↑ "Climate of Maopoopo 1991-2020" (in fr). Météo-France. https://donneespubliques.meteofrance.fr/FichesClim/FICHECLIM_98611001.pdf.
11. ↑ "Les populations légales de Wallis et Futuna en 2018". https://www.insee.fr/fr/statistiques/3685976?sommaire=2121453.
12. ↑ ""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"". https://www.statistique.wf/download/43/recensement-2018/1157/principaux_tableaux_population_2018.ods.
13. ↑ "Wallis and Futuna". CIA World Factbook. https://www.cia.gov/the-world-factbook/countries/wallis-and-futuna/.
14. ↑ "LIVRET D'ACCUEIL Wallis et Futuna ." Wallis and Futuna. p. 22 (22/28). Retrieved on September 14, 2016.
15. ↑ "Cartographie des établissements du second degré." Wallis and Futuna. June 24, 2016. Retrieved on September 14, 2016.

## References

* 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", 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. doi:10.1016/j.earscirev.2010.11.003. Bibcode: 2011ESRv..107...91G.
* 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). doi:10.1016/j.jvolgeores.2020.107064. Bibcode: 2020JVGR..40607064S.
* 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). doi:10.1016/j.jvolgeores.2022.107646. Bibcode: 2022JVGR..43107646S.

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