List Of Volcanoes In Fiji
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List Of Volcanoes In Fiji
This is a list of active and extinct volcanoes in Fiji. References *Islands of Fiji Island Directory, United Nations Environment Programme {{Fiji topics Fiji Volcanoes 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 ...
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Volcano
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 plates slide ...
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Fiji
Fiji ( , ,; fj, Viti, ; Fiji Hindi: फ़िजी, ''Fijī''), officially the Republic of Fiji, is an island country in Melanesia, part of Oceania in the South Pacific Ocean. It lies about north-northeast of New Zealand. Fiji consists of an archipelago of more than 330 islands—of which about 110 are permanently inhabited—and more than 500 islets, amounting to a total land area of about . The most outlying island group is Ono-i-Lau. About 87% of the total population of live on the two major islands, Viti Levu and Vanua Levu. About three-quarters of Fijians live on Viti Levu's coasts: either in the capital city of Suva; or in smaller urban centres such as Nadi—where tourism is the major local industry; or in Lautoka, where the Sugarcane, sugar-cane industry is dominant. The interior of Viti Levu is sparsely inhabited because of its terrain. The majority of Fiji's islands were formed by Volcano, volcanic activity starting around 150 million years ago. Some geo ...
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Geographic Coordinates
The geographic coordinate system (GCS) is a spherical or ellipsoidal coordinate system for measuring and communicating positions directly on the Earth as latitude and longitude. It is the simplest, oldest and most widely used of the various spatial reference systems that are in use, and forms the basis for most others. Although latitude and longitude form a coordinate tuple like a cartesian coordinate system, the geographic coordinate system is not cartesian because the measurements are angles and are not on a planar surface. A full GCS specification, such as those listed in the EPSG and ISO 19111 standards, also includes a choice of geodetic datum (including an Earth ellipsoid), as different datums will yield different latitude and longitude values for the same location. History The invention of a geographic coordinate system is generally credited to Eratosthenes of Cyrene, who composed his now-lost ''Geography'' at the Library of Alexandria in the 3rd century  ...
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Koro Island
Koro ('''village in Fijian) is a volcanic island of Fiji that forms part of the Lomaiviti Archipelago. The Koro Sea is named after this volcanic island, which has a chain of basaltic cinder cones extending from north to south along its crest. With a land area of 103.2 square kilometers (42.1 square Miles), it is the seventh largest island (approximately 5x10 miles) of Fiji. Its latitude is 17.18°; its longitude is 179.24°. Its population as of 2017 census was 2,937 spread across 14 villages on the island. A roll-on, roll-off ferry services Koro weekly from Suva, and also connects Koro to Vanua Levu to the North. Fiji Link provides one scheduled flight per week to Koro, usually on Friday from Nausori Airport. The island has been accurately and exotically described by no one better than Captain Bligh of His Majesty’s ship “Providence”. During his historical journey from Tahiti to Batavia in 1789, he wrote, “the island of Koro is of good height, it is easternmost of ...
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Nabukelevu
Nabukelevu is a volcano located on the southwest portion of Kadavu Island in Fiji. It is tall, and last erupted around 1660. It has formed lava domes Nabukelevu is the only area in west Kadavu Island that retains extensive old-growth forest. A area centred on Nabukelevu is the Nabukelevu Important Bird Area. It supports populations of Vulnerable species, vulnerable Collared Petrel and Crimson shining parrot, and Near-threatened species, near threatened Whistling fruit dove and Kadavu fantail. The Collared Petrel breeding site and unique landscape of the mountain contribute to its national significance as outlined in Fiji's Biodiversity Strategy and Action Plan. References

Volcanoes of Fiji Kadavu Group Preliminary Register of Sites of National Significance in Fiji Important Bird Areas of Fiji {{Fiji-geo-stub ...
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Rotuma
Rotuma is a Fijian dependency, consisting of Rotuma Island and nearby islets. The island group is home to a large and unique Polynesian indigenous ethnic group which constitutes a recognisable minority within the population of Fiji, known as "Rotumans". Its population at the 2017 census was 1,594, although many more Rotumans live on mainland Fijian islands, totaling 10,000. Geography and geology The Rotuma group of volcanic islands are located (Suva to Ahau) north of Fiji. Rotuma Island itself is long and wide, with a land area of approximately , making it the 12th-largest of the Fiji islands. The island is bisected by an isthmus into a larger eastern part and a western peninsula. The isthmus is low and narrow, only wide, and is the site of Motusa village ( Itutiu district). North of the isthmus is Maka Bay, and in the south is Hapmafau Bay. There is a large population of coral reefs in these bays, and there are boat passages through them. Rotuma is a shield volcano m ...
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Taveuni (volcano)
Taveuni is elongated shield volcano on Taveuni Island, Fiji, and its peak (Mount Uluigalau) reaches 1,241 meters above sea level. History Volcanism on Taveuni began circa 780,000 years ago, but most volcanic activity took place during the Holocene Epoch, which started about 11,000 years ago. Holocene Activity Since 9500 B.C. 167 volcanic vents have formed, mainly along the southern inland tip. The youngest vent formed sometime between 4690 and 4900 B.C. Eruptions occurred at an interval of about 70 years, but since 1200 B.C., there have been six periods of time with frequent eruptions, each spanning between 200 and 400 years. Hazards If an eruption does occur, Taveuni's economy could easily be destroyed. Nearly all farms will catch on Fire and nearly every port in Taveuni is in a hydrovolcanic hazard zone or a lahar hazard zone, and all imports/exports would be completely stopped until the ports are repaired. Lava Flows Unlike many other volcanoes, the largest hazard from Tav ...
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United Nations Environment Programme
The United Nations Environment Programme (UNEP) is responsible for coordinating responses to environmental issues within the United Nations system. It was established by Maurice Strong, its first director, after the United Nations Conference on the Human Environment in Stockholm in June 1972. Its mandate is to provide leadership, deliver science and develop solutions on a wide range of issues, including climate change, the management of marine and terrestrial ecosystems, and green economic development. The organization also develops international environmental agreements; publishes and promotes environmental science and helps national governments achieve environmental targets. As a member of the United Nations Development Group, UNEP aims to help the world meet the 17 Sustainable Development Goals. UNEP hosts the secretariats of several multilateral environmental agreements and research bodies, including The Convention on Biological Diversity (CBD), The Minamata Convention on M ...
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Lists Of Volcanoes
These lists cover volcanoes by type and by location. Type * List of extraterrestrial volcanoes * List of largest volcanic eruptions * List of shield volcanoes * List of stratovolcanoes * List of subglacial volcanoes * List of submarine volcanoes * List of volcanoes by elevation Location Africa * List of volcanoes in Algeria * List of volcanoes in Cameroon * List of volcanoes in Cape Verde *List of volcanoes in Chad * List of volcanoes in the Comoros *List of volcanoes in the Democratic Republic of the Congo * List of volcanoes in Djibouti *List of volcanoes in Equatorial Guinea * List of volcanoes in Eritrea *List of volcanoes in Ethiopia *List of volcanoes in Kenya * List of volcanoes in Libya *List of volcanoes in Madagascar *In Nigeria all the volcanoes are in the Biu Plateau *List of volcanoes in Réunion *List of volcanoes in Rwanda *São Tomé and Príncipe has only one volcano, Pico de São Tomé * List of volcanoes in South Africa *List of volcanoes in Sudan *List of ...
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Volcanoes Of Fiji
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 plates slide pa ...
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