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Futuna Plate
The Futuna Plate is a very small tectonic plate located near the south Pacific island of Futuna. It is sandwiched between the Pacific Plate to the north and the Australian Plate to the south with the Niuafo'ou Plate The Niuafo'ou Plate is a small tectonic plate located west of the islands of Tonga. This plate is sandwiched between the Pacific Plate to the north, the very unstable Tonga Plate to the east and the Australian Plate The Australian Plate is a ... to the east. References * Bird, P. (2003) An updated digital model of plate boundaries, ''Geochemistry, Geophysics, Geosystems'', 4(3), 1027, Tectonic plates Geology of the Pacific Ocean {{tectonics-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Balmoral Reef And Conway Reef Plates Map-fr
Balmoral Castle is a residence of King Charles III in Aberdeenshire, Scotland. Balmoral may also refer to: Places Australia * Balmoral, New South Wales, a locality of Sydney * Balmoral, New South Wales (Lake Macquarie) * Balmoral, New South Wales (Southern Highlands) * Balmoral, Queensland * Balmoral, Victoria Belgium * Balmoral, a hamlet near the town of Spa, Belgium Canada * Balmoral, British Columbia * Balmoral, New Brunswick * Balmoral Parish, New Brunswick * Balmoral Mills, Nova Scotia * Balmoral, Ontario, a community in Haldimand County * Balmoral Grist Mill Museum, Balmoral Mills, Nova Scotia * Balmoral, Manitoba New Zealand * Balmoral, New Zealand, a suburb of Auckland Northern Ireland * Balmoral (District Electoral Area), an area in south Belfast * Balmoral railway station, Belfast * Balmoral Golf Club, Belfast * The Balmoral Show, an agricultural show that takes place annually near Belfast * Balmoral Park, Lisburn, the new location of the Balm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tectonic Plate
Plate tectonics (from the la, label=Late Latin, tectonicus, from the grc, τεκτονικός, lit=pertaining to building) is the generally accepted scientific theory that considers the Earth's lithosphere to comprise a number of large tectonic plates which have been slowly moving since about 3.4 billion years ago. The model builds on the concept of ''continental drift'', an idea developed during the first decades of the 20th century. Plate tectonics came to be generally accepted by geoscientists after seafloor spreading was validated in the mid to late 1960s. Earth's lithosphere, which is the rigid outermost shell of the planet (the crust and upper mantle), is broken into seven or eight major plates (depending on how they are defined) and many minor plates or "platelets". Where the plates meet, their relative motion determines the type of plate boundary: '' convergent'', '' divergent'', or ''transform''. Earthquakes, volcanic activity, mountain-building, and oceanic tren ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Futuna Island, Wallis And Futuna
Futuna (; ) is an island in the Pacific Ocean occupying area of with a population of 10,912. It belongs to the French overseas collectivity (''collectivité d'outre-mer'', or ''COM'') of Wallis and Futuna. It is one of the Hoorn Islands or Îles Horne; nearby Alofi is the other. They are both remnants of the same ancient, extinct volcano, now bordered with a fringing reef. Futuna has a maximum elevation of . 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. Futuna takes its name from an endonym derived from the local ''futu'', meaning fish-poison tree. Geography The population was 10,765 (as of the 2022 census);. Futuna's highest point is Mont Puke at above sea level, and the island has an area of , with in Sigave and in Alo. Climate Futuna (Maopoopo weather station) has a tropical rainforest climate (Köppen climate classification ''Af''). The average annual ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pacific Plate
The Pacific Plate is an oceanic tectonic plate that lies beneath the Pacific Ocean. At , it is the largest tectonic plate. The plate first came into existence 190 million years ago, at the triple junction between the Farallon, Phoenix, and Izanagi Plates. The Pacific Plate subsequently grew to where it underlies most of the Pacific Ocean basin. This reduced the Farallon Plate to a few remnants along the west coast of North America and the Phoenix Plate to a small remnant near the Drake Passage, and destroyed the Izanagi Plate by subduction under Asia. The Pacific Plate contains an interior hot spot forming the Hawaiian Islands. Boundaries The north-eastern side is a divergent boundary with the Explorer Plate, the Juan de Fuca Plate and the Gorda Plate forming respectively the Explorer Ridge, the Juan de Fuca Ridge and the Gorda Ridge. In the middle of the eastern side is a transform boundary with the North American Plate along the San Andreas Fault, and a boundary with the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Australian Plate
The Australian Plate is a major tectonic plate in the eastern and, largely, southern hemispheres. Originally a part of the ancient continent of Gondwana, Australia remained connected to India and Antarctica until approximately when India broke away and began moving north. Australia and Antarctica began rifting and completely separated roughly . The Australian plate later fused with the adjacent Indian Plate beneath the Indian Ocean to form a single Indo-Australian Plate. However, recent studies suggest that the two plates have once again split apart and have been separate plates for at least 3 million years and likely longer. The Australian Plate includes the continent of Australia, including Tasmania, as well as portions of New Guinea, New Zealand and the Indian Ocean basin. Scope The continental crust of this plate covers the whole of Australia, the Gulf of Carpentaria, southern New Guinea, the Arafura Sea, the Coral Sea. The continental crust also includes northwestern N ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Niuafo'ou Plate
The Niuafo'ou Plate is a small tectonic plate located west of the islands of Tonga. This plate is sandwiched between the Pacific Plate to the north, the very unstable Tonga Plate to the east and the Australian Plate The Australian Plate is a major tectonic plate in the eastern and, largely, southern hemispheres. Originally a part of the ancient continent of Gondwana, Australia remained connected to India and Antarctica until approximately when India broke ... to the west. It is primarily surrounded by divergent boundaries. This plate is riddled with active faults thus making the area extremely earthquake prone. See also * References * {{DEFAULTSORT:Niuafo'ou Plate Tectonic plates Geology of the Pacific Ocean ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tectonic Plates
Plate tectonics (from the la, label=Late Latin, tectonicus, from the grc, τεκτονικός, lit=pertaining to building) is the generally accepted scientific theory that considers the Earth's lithosphere to comprise a number of large tectonic plates which have been slowly moving since about 3.4 billion years ago. The model builds on the concept of ''continental drift'', an idea developed during the first decades of the 20th century. Plate tectonics came to be generally accepted by geoscientists after seafloor spreading was validated in the mid to late 1960s. Earth's lithosphere, which is the rigid outermost shell of the planet (the crust and upper mantle), is broken into seven or eight major plates (depending on how they are defined) and many minor plates or "platelets". Where the plates meet, their relative motion determines the type of plate boundary: '' convergent'', '' divergent'', or ''transform''. Earthquakes, volcanic activity, mountain-building, and oceanic tren ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
