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Mehetia
Meheti'a or Me'eti'a is a volcanic island in the Windward Islands, in the east of the Society Islands in French Polynesia. This island is a very young active stratovolcano east of the Taiarapu Peninsula of Tahiti. It belongs to the Teahiti'a-Mehetia hotspot. The island has an area of and its highest point is 435 metres (1,427 ft). The peak is a well-defined volcanic crater. In 1981 the island was the centre of earthquakes. History Tahitian oral tradition holds that navigators stopped at Mehiti'a, which was regarded as sacred, on their long voyage to New Zealand. This oral history correlates with geological evidence found in southern New Zealand which can be traced back to Mehiti'a. The early Polynesian voyagers commonly gave Polynesian ancestral names and symbolism to new places. The high point of Mehetia is Mount Hiurai (Hi’ura’i/Hikurangi) The name Hikurangi in Aotearoa / New Zealand probably came from Mehetia and the name Hi’ura’i probably has its o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Windward Islands (Society Islands)
The Windward Islands (french: Îles du Vent) are the eastern group of the Society Islands in French Polynesia, an overseas collectivity of France in the southern Pacific Ocean. These islands were also previously named the Georgian Islands in honour of King George III of the United Kingdom. Geography The archipelago comprises an administrative division (french: subdivision administrative) of French Polynesia, and includes the following islands: *Tahiti * Moorea * Mehetia * Tetiaroa *Maiao The capital of the administrative district is Papeete on the island of Tahiti. Tahiti, Moorea, and Mehetia are high islands. Tetiaroa and Maiao are coral atolls. Culture The majority of the population speaks French and Tahitian (co-official with French throughout French Polynesia). Administrative The Windward Islands form the administrative subdivision of the Windward Islands (''subdivision administrative des Îles du Vent''), one of French Polynesia's five administrative subdivisions. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tahiti
Tahiti (; Tahitian ; ; previously also known as Otaheite) is the largest island of the Windward group of the Society Islands in French Polynesia. It is located in the central part of the Pacific Ocean and the nearest major landmass is Australia. Divided into two parts, ''Tahiti Nui'' (bigger, northwestern part) and ''Tahiti Iti'' (smaller, southeastern part), the island was formed from volcanic activity; it is high and mountainous with surrounding coral reefs. Its population was 189,517 in 2017, making it by far the most populous island in French Polynesia and accounting for 68.7% of its total population. Tahiti is the economic, cultural and political centre of French Polynesia, an overseas collectivity and an overseas country of the French Republic. The capital of French Polynesia, Papeete, is located on the northwest coast of Tahiti. The only international airport in the region, Faaā International Airport, is on Tahiti near Papeete. Tahiti was originally settled by Polyn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Hikurangi (Gisborne District)
Mount Hikurangi (or ''Te Ara ki Hikurangi'' in Māori) is a peak in the eastern corner of New Zealand's North Island, about north of Gisborne, and southwest of the East Cape Lighthouse. On a spur of the Raukumara Range in the Waiapu Valley, it is the North Island's highest non-volcanic peak. Mount Hikurangi is within the rohe of Ngāti Porou and Ngati and is the iwi's most significant icon. In Māori mythology, it was the first part of the North Island to emerge when Māui pulled it as a giant fish from the ocean. According to these beliefs, his waka, '' Nukutaimemeha'', became stranded on the mountain, and lies petrified between the mountain's peaks in Lake Hinetakawhiti. Nearby summits include Whanokao (), Aorangi (), Wharekia () and Taitai (). Together, these mountains provide what '' Te Ara: The Encyclopedia of New Zealand'' calls an "awe-inspiring vista". The early arrivals to Aotearoa commonly gave Polynesian ancestral names and symbolism to New Zealand pla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
French Polynesia
)Territorial motto: ( en, "Great Tahiti of the Golden Haze") , anthem = , song_type = Regional anthem , song = "Ia Ora 'O Tahiti Nui" , image_map = French Polynesia on the globe (French Polynesia centered).svg , map_alt = Location of French Polynesia , map_caption = Location of French Polynesia (circled in red) , mapsize = 290px , subdivision_type = Sovereign state , subdivision_name = , established_title = Protectorate proclaimed , established_date = 9 September 1842 , established_title2 = Territorial status , established_date2 = 27 October 1946 , established_title3 = Collectivity status , established_date3 = 28 March 2003 , established_title4 = Country status (nominal title) , established_date4 = 27 February 2004 , official_languages = French , regional_languages = , capital = Papeete , coordinates = , largest_city = Fa'a'ā , demonym = French Polynesian , ethnic_groups = 66.5% unmixed Polynesians7.1% mixed Polynesians9.3% Demis11. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taiarapu-Est
Ta'iarapu-Est (literally "Tai'arapu East") is a commune of French Polynesia, an overseas territory of France in the Pacific Ocean. The commune of Tai'arapu-Est is located on the island of Tahiti, in the administrative subdivision of the Windward Islands, themselves part of the Society Islands.Décret n° 2005-1611 du 20 décembre 2005 pris pour l'application du statut d'autonomie de la Polynésie française At the 2017 census it had a population of 12,701. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Volcanoes In French Polynesia
This is a list of active and extinct volcanoes. References External links Volcanoes of Hawaii and the Pacific Ocean French Polynesia )Territorial motto: ( en, "Great Tahiti of the Golden Haze") , anthem = , song_type = Regional anthem , song = "Ia Ora 'O Tahiti Nui" , image_map = French Polynesia on the globe (French Polynesia centered).svg , map_alt = Location of French ... French Polynesia-related lists {{FrenchPolynesia-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Teahitia
Teahitia ("Standing Fire") is a submarine volcano, located northeast of the southeast tip of Tahiti of the Society Islands in the Pacific Ocean The Pacific Ocean is the largest and deepest of Earth's five oceanic divisions. It extends from the Arctic Ocean in the north to the Southern Ocean (or, depending on definition, to Antarctica) in the south, and is bounded by the conti ..., with its peak 1600 meters below the water surface. It belongs to the Society hotspot. Teahitia's last eruption occurred in 1985. The seamount has four prominent cones. Submersible dives in 1986 and 1989 found two active hydrothermal fields on the volcano's flanks. A further dive in 2013 found ongoing hydrothermal venting. Earthquake swarms in March 1982, July 1983, December 1983, and January 1985 have been associated with submarine eruptions. On 16 March 2008 Teahitia was the epicentre of an earthquake measuring 3.2 on the Richter scale. The weak tremor was felt in Tahiti, causing the be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Society Islands
The Society Islands (french: Îles de la Société, officially ''Archipel de la Société;'' ty, Tōtaiete mā) are an archipelago located in the South Pacific Ocean. Politically, they are part of French Polynesia, an overseas country of the French Republic. Geographically, they form part of Polynesia. The archipelago is believed to have been named by Captain James Cook during his first voyage in 1769, supposedly in honour of the Royal Society, the sponsor of the first British scientific survey of the islands; however, Cook wrote in his journal that he called the islands ''Society'' "as they lay contiguous to one another." History Dating colonization The first Polynesians are understood to have arrived on these islands around 1000AD. Oral history origin The islanders explain their origins in term of a orally transmitted story. The feathered god Ta'aroa lay in his shell. He called out but no-one answered, so he went back into his shell, where he stayed for aeons. When h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Louis Antoine De Bougainville
Louis-Antoine, Comte de Bougainville (, , ; 12 November 1729 – August 1811) was a French admiral and explorer. A contemporary of the British explorer James Cook, he took part in the Seven Years' War in North America and the American Revolutionary War against Britain. Bougainville later gained fame for his expeditions, including a circumnavigation of the globe in a scientific expedition in 1763, the first recorded settlement on the Falkland Islands, and voyages into the Pacific Ocean. Bougainville Island of Papua New Guinea as well as the Bougainvillea flower were named after him. Biography Early career Bougainville was born in Paris, the capital of the Kingdom of France, the son of notary Pierre-Yves de Bougainville (1688-1756), on either 11 or 12 November 1729. In early life, he studied law, but soon abandoned the profession. In 1753 he entered the French Army in the corps of musketeers. At the age of twenty-five he published a treatise on integral calculus, as a supplem ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pacific Ocean
The Pacific Ocean is the largest and deepest of Earth's five oceanic divisions. It extends from the Arctic Ocean in the north to the Southern Ocean (or, depending on definition, to Antarctica) in the south, and is bounded by the continents of Asia and Oceania in the west and the Americas in the east. At in area (as defined with a southern Antarctic border), this largest division of the World Ocean—and, in turn, the hydrosphere—covers about 46% of Earth's water surface and about 32% of its total surface area, larger than Earth's entire land area combined .Pacific Ocean . '' Britannica Concise.'' 2008: Encyclopædia Britannica, Inc. The centers of both the [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Active Volcanoes
An active volcano is a volcano which is either erupting or is likely to erupt in the future. An active volcano which is not currently erupting is known as a dormant volcano. Overview Tlocene Epoch. Most volcanoes are situated on the Pacific Ring of Fire. An estimated 500 million people live near active volcanoes. ''Historical time'' (or recorded history) is another timeframe for ''active''. However, the span of recorded history differs from region to region. In China and the Mediterranean, it reaches back nearly 3,000 years, but in the Pacific Northwest of the United States and Canada, it reaches back less than 300 years, and in Hawaii and New Zealand it is only around 200 years. The incomplete ''Catalogue of the Active Volcanoes of the World'', published in parts between 1951 and 1975 by the International Association of Volcanology, uses this definition, by which there are more than 500 active volcanoes. , the Smithsonian Global Volcanism Program recognizes 560 volcanoes with ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stratovolcanoes Of France
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 volc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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