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Tanga Islands
The Tanga Islands are an island group in Papua New Guinea, located north-east of New Ireland and part of the Bismarck Archipelago. Tanga is made up of four main islands — Boang, Maledok, Lif and Tefa — and a number of smaller, uninhabited islands. Boang (ca. 27 km2) consists entirely of a raised, relatively flat-topped plateau of Pleistocene, coralline limestone, which rises up to 170 m above sea level (asl.) and has sheer cliffs around a large part of its perimeter. The islands are the remnants of a stratovolcano which collapsed to form a caldera A caldera ( ) is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcano eruption. When large volumes of magma are erupted over a short time, structural support for the rock above the magma chamber is .... Lif (283 m), Tefa (155 m), and Malendok (472 m) islands are on the caldera rim, while Bitlik and Bitbok islands are lava domes constructed near the center of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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, one of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lava Dome
In volcanology, a lava dome is a circular mound-shaped protrusion resulting from the slow extrusion of viscous lava from a volcano. Dome-building eruptions are common, particularly in convergent plate boundary settings. Around 6% of eruptions on Earth are lava dome forming. The geochemistry of lava domes can vary from basalt (e.g. Semeru, 1946) to rhyolite (e.g. Chaiten, 2010) although the majority are of intermediate composition (such as Santiaguito, dacite-andesite, present day) The characteristic dome shape is attributed to high viscosity that prevents the lava from flowing very far. This high viscosity can be obtained in two ways: by high levels of silica in the magma, or by degassing of fluid magma. Since viscous basaltic and andesitic domes weather fast and easily break apart by further input of fluid lava, most of the preserved domes have high silica content and consist of rhyolite or dacite. Existence of lava domes has been suggested for some domed structures on the Mo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Ireland Province
New Ireland Province, formerly New Mecklenburg (german: Neu-Mecklenburg), and Nova Hibernia, is the northeasternmost province of Papua New Guinea. Physical geography The largest island of the province is New Ireland. Also part of the province are numerous smaller islands, including Saint Matthias Group (Mussau, Emirau), New Hanover, Djaul, Tabar Group ( Tabar, Tatau, Simberi), Lihir, Tanga Group (Malendok, Boang), Feni Islands (Ambitle, Babase) and Anir. The land area of the province is around 9 560 km². The sea area within the Exclusive Economic Zone (EEZ) of New Ireland Province is around 230,000 km². Ecology In the early days of the French Revolution while searching for a lost scientific expedition the vessel La Recherche passed by New Ireland. On board was the prominent botanist Jacques-Julien Houtou de Labillardière who noted in his journal fine stands of teak (tectona grandis) trees growing at the southern end of the island. This marks the easter ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sumsuma
Sumsuma (1903?–1965), the leader of the Rabaul Strike of 1929 was from Sasa village on Boang Island and Tefa Island in the Tanga Islands of New Ireland Province New Ireland Province, formerly New Mecklenburg (german: Neu-Mecklenburg), and Nova Hibernia, is the northeasternmost province of Papua New Guinea. Physical geography The largest island of the province is New Ireland. Also part of the province a ..., Papua New Guinea. He united people from all tribes to protest against the Australians in Rabaul on 29,January,1929. He was assisted by Ndramei of Manus and Kateo of Wewak. References 1900s births 1965 deaths People from New Ireland Province People from Namatanai People from Tanga Islands {{PapuaNewGuinea-bio-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sir Julius Chan
Sir Julius Chan (born 29 August 1939) served as Prime Minister of Papua New Guinea from 1980 to 1982 and from 1994 to 1997. He is Member of Parliament for New Ireland Province, having won the seat in the 2007 national election. He is also the current Governor of New Ireland Province, since 2007. On 26 May 2019, Prime Minister Peter O'Neill announced he would soon resign and that he wished for Sir Julius to succeed him. An outgoing Prime Minister does not, however, have the power to appoint his successor, and the following day O'Neill delayed his own formal resignation. He was also a leading figure in his country during the years-long Bougainville conflict. Early life Chan was born as the fifth child out of seven children on the Tanga Islands in the Territory of New Guinea, in what is now New Ireland Province, the son of Chin Pak (陳柏), a trader from Taishan, China and Miriam Tinkoris, a native New Irelander. He was educated at Marist College Ashgrove in Brisbane, Queensland, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prime Minister Of Papua New Guinea
The prime minister of the Independent State of Papua New Guinea ( tpi, Prai Minista bilong Papua Niugini) is Papua New Guinea's head of government, consequent on being the leader of the party or coalition with majority support in the National Parliament. The prime minister serves as the head of his party, the head of the coalition government, and the chairman of the National Executive Council. The office of Prime Minister was preceded by the Chief Ministry. 2011–2012 constitutional crisis From December 2011, the office was disputed between Peter O'Neill of the People's National Congress Party and Sir Michael Somare of the National Alliance Party; the latter eventually supported O'Neill as Prime Minister on 3 August 2012, thus ending the constitutional crisis. List of prime ministers of Papua New Guinea (1975–present) See also * Monarch of Papua New Guinea *Governor-General of Papua New Guinea Notes References {{Prime Minister Papua New Guinea, Prime Minis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tanga People
Tanga people are a tribe of Papua New Guinea that lives in the Tanga Islands and Feni Islands of Tanir Rural LLG and three villages (Sena, Muliama and Warangansau) in the Matalai Rural LLG of Namatanai District of New Ireland Province. They speak the Tangga language which has since been split into three separate languages which are now spoken by the Tangans. These languages are: Niwer Mil, Warwar Feni and Fanamaket. Their population according to the 2011 Papua New Guinea Census Report is 12,466 people. Tubuan, Sokapana and Ingiet are the secret societies practised by the Tanga people. F.L.S. Bell has a collection on Tanga Islands in the University of Sydney The University of Sydney (USYD), also known as Sydney University, or informally Sydney Uni, is a public research university located in Sydney, Australia. Founded in 1850, it is the oldest university in Australia and is one of the country's si ... Library in Australia.https://library.sydney.edu.au/collections/rare-books/do ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stratovolcano
A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as . Stratovolcanoes are sometimes called composite volcanoes because of their composite stratified structure, built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stratovolcano
A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as . Stratovolcanoes are sometimes called composite volcanoes because of their composite stratified structure, built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boang Island
Boang Island is an island of the Tanga Islands 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 ..., located to the east of New Ireland. It is located to the north-east of Malendok Island, and although smaller it is more populous and considered the socio-economic hub of the islands. References Islands of Papua New Guinea {{PapuaNewGuinea-island-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bismarck Archipelago
The Bismarck Archipelago (, ) is a group of islands off the northeastern coast of New Guinea in the western Pacific Ocean and is part of the Islands Region of Papua New Guinea. Its area is about 50,000 square km. History The first inhabitants of the archipelago arrived around 30–40,000 years ago. They may have traveled from New Guinea, by boat across the Bismarck Sea or via a temporary land bridge, created by an uplift in the Earth's Crust (geology), crust. Later arrivals included the Lapita people. The first European to visit these islands was Dutch explorer Willem Schouten in 1616. The islands remained unsettled by western Europeans until they were annexed as part of the German protectorate of German New Guinea in 1884. The area was named in honour of the Chancellor of Germany (German Reich), Chancellor Otto von Bismarck. On 1888 Ritter Island eruption and tsunami, 13 March 1888, a volcano erupted on Ritter Island causing a megatsunami. Almost the entire volcano fell into t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
