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Wagifa Island
Wagifa Island is an island of Papua New Guinea. It is located to the south east of Goodenough Island. A small village is located on the island and aside from fishing, the people only grow limited cassava. As such the primary means of food for local inhabitants comes from trade off the island and at the rural market on Goodenough island. Wagifa Island is entirely volcanic in geological origin. References

Islands of Papua New Guinea {{PapuaNewGuinea-geo-stub ...
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Papua New Guinea
Papua New Guinea (abbreviated PNG; , ; tpi, Papua Niugini; ho, Papua Niu Gini), officially the Independent State of Papua New Guinea ( tpi, Independen Stet bilong Papua Niugini; ho, Independen Stet bilong Papua Niu Gini), is a country in Oceania that comprises the eastern half of the island of New Guinea and its offshore islands in Melanesia (a region of the southwestern Pacific Ocean north of Australia). Its capital, located along its southeastern coast, is Port Moresby. The country is the world's third largest island country, with an area of . At the national level, after being ruled by three external powers since 1884, including nearly 60 years of Australian administration starting during World War I, Papua New Guinea established its sovereignty in 1975. It became an independent Commonwealth realm in 1975 with Elizabeth II as its queen. It also became a member of the Commonwealth of Nations in its own right. There are 839 known languages of Papua New Guinea, on ...
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Provinces Of Papua New Guinea
For administrative purposes, Papua New Guinea is divided into administrative divisions called provinces. There are 22 provincial-level divisions, which include 20 provinces, the Autonomous Region of Bougainville, and the National Capital District of Port Moresby. In 2009, the National Parliament of Papua New Guinea created two additional provinces, that officially came into being on 17 May 2012."PNG’S new province Hela, Jiwaka declared"
, ''The National'', 17 May 2012
They were Hela Province, which was split from
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Milne Bay Province
Milne Bay is a province of Papua New Guinea. Its capital is Alotau. The province covers 14,345 km² of land and 252,990 km² of sea, within the province there are more than 600 islands, about 160 of which are inhabited. The province has about 276,000 inhabitants, speaking about 48 languages, most of which belong to the Eastern Malayo-Polynesian branch of the Austronesian language family. Economically the province is dependent upon tourism, oil palm, and gold mining on Misima Island; in addition to these larger industries there are many small-scale village projects in cocoa and copra cultivation. The World War II Battle of Milne Bay took place in the province. Culturally the Milne Bay region is sometimes referred to as "the Massim," a term originating from the name of Misima Island. Massim societies are usually characterized by matrilineal descent, elaborate mortuary sequences and complex systems of ritual exchange including the Kula ring. From island group to island ...
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Local-level Governments Of Papua New Guinea
Papua New Guinea has 326 local-level governments (LLGs) comprising 6,112 wards as of 2018. ''Note'': LLG names with slashes (/) are listed with dashes (-) due to technical limitations on previous versions of the Wikipedia software. Administrative divisions At the highest level, Papua New Guinea is divided into four regions, namely the Highlands, Islands, Momase, and Southern regions. Below, Papua New Guinea has 22 province-level divisions: 20 integrated provinces, the autonomous province of North Solomons (Bougainville) and the National Capital District. Each province has one or more districts, and each district has one or more local-level government (LLG) areas. For census purposes, the LLG areas are subdivided into wards and those into census units. Wards typically consist of a few hundred to a few thousand individuals, and are the lowest level of government administration under LLGs. Wards are further divided into census units (CU). List of local-level governments by ...
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Kiriwina-Goodenough District
Kiriwina-Goodenough District is a district of the Milne Bay Province of Papua New Guinea Papua New Guinea (abbreviated PNG; , ; tpi, Papua Niugini; ho, Papua Niu Gini), officially the Independent State of Papua New Guinea ( tpi, Independen Stet bilong Papua Niugini; ho, Independen Stet bilong Papua Niu Gini), is a country i .... Its capital is Kiriwina. The population of the district was 63,916 at the 2011 census.Districts of Papua New Guinea
at statoids.com


References

Districts of Papua New Guinea Milne Bay Province {{MilneBayProvince-geo-stub ...
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Goodenough Island Rural LLG
Goodenough Island Rural LLG is a local-level government (LLG) of Milne Bay Province, Papua New Guinea Papua New Guinea (abbreviated PNG; , ; tpi, Papua Niugini; ho, Papua Niu Gini), officially the Independent State of Papua New Guinea ( tpi, Independen Stet bilong Papua Niugini; ho, Independen Stet bilong Papua Niu Gini), is a country i .... Wards *01. Waibula *02. Ufaufa *03. Watuluma Upper *04. Watuluma Lower *05. Idakamenai *06. Ulutuya *07. Wakonai *08. Vivigani *09. Eweli *10. Kalauna *11. Belebele *12. Mataita West *13. Mataita East *14. Faiava *15. Ufu'ufu *16. Bwadoga East *17. Bwadoga West *18. Wagifa *19. Abolu *20. Kilia *21. Lauwela *22. Awale *23. Utalo *24. Diodio *25. Yauyaula *26. Awaya *27. Ibawana *28. Kalimtabutabu References * * Local-level governments of Milne Bay Province {{MilneBayProvince-geo-stub ...
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Goodenough Island
Goodenough Island in the Solomon Sea, also known as Nidula Island, is the westernmost of the three large islands of the D'Entrecasteaux Islands in Milne Bay Province of Papua New Guinea. It lies to the east of mainland New Guinea and southwest of the Trobriand Islands. It is roughly circular in shape, measuring with an area of and a shoreline of . From a coastal belt varying in width from in width, the island rises sharply to the summit of Mount Vineuo, above sea level, making it one of the most precipitous islands in the world. The small outlier Wagifa Island lies to the south-east of the island, and is included within Goodenough's administration. Climate and vegetation Like much of New Guinea, the climate is tropical with high temperatures and humidity throughout the year. The northwest monsoon season lasts from December to March and brings sudden rain squalls. From May to October southeasterly winds are cooler and more gentle. Tropical cyclones are infrequent. ...
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Cassava
''Manihot esculenta'', commonly called cassava (), manioc, or yuca (among numerous regional names), is a woody shrub of the spurge family, Euphorbiaceae, native to South America. Although a perennial plant, cassava is extensively cultivated as an annual crop in tropical and subtropical regions for its edible starchy tuberous root, a major source of carbohydrates. Though it is often called ''yuca'' in parts of Spanish America and in the United States, it is not related to yucca, a shrub in the family Asparagaceae. Cassava is predominantly consumed in boiled form, but substantial quantities are used to extract cassava starch, called tapioca, which is used for food, animal feed, and industrial purposes. The Brazilian farinha, and the related ''garri'' of West Africa, is an edible coarse flour obtained by grating cassava roots, pressing moisture off the obtained grated pulp, and finally drying it (and roasting both in the case of farinha and garri). Cassava is the third-largest so ...
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Volcanic
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic pl ...
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