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Plaine Des Sables
The Plaine des Sables ( en, "Sands Plain") is a volcanic plateau in the mountains of Réunion. Part of the Piton de la Fournaise massif, this volcanic desert is situated at the border of Saint-Joseph and Sainte-Rose, within Réunion National Park Réunion National Park (french: Parc national de La Réunion) is a National Park of France located on the island of Réunion, an overseas department in the western Indian Ocean. Established on 5 March 2007, the park protects the endemic ecosys .... References Sables Sables Sables Volcanic deserts Deserts of Africa Saint-Joseph, Réunion Réunion National Park {{Reunion-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plaine Des Sables 2015
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Plaine may refer to: * Plaine (river), a tributary of the river Meurthe in France * Plaine, Bas-Rhin, a commune in Alsace in north-eastern France * Plaine-Haute, a commune in the Côtes-d'Armor department in Brittany in northwestern France * Plaine Morte Glacier, a glacier in the canton of Bern in Switzerland * Belle Plaine (other) * La Plaine (other) See also * Plain (other) A plain is a flat, sweeping landmass. Plain may also refer to: Places * Plain, Texas, U.S. * Plain, Washington, U.S. * Plain, Wisconsin, U.S. * Plain City (other), several places * Plain Township (other), several places Musi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Plateau
A volcanic plateau is a plateau produced by volcanic activity. There are two main types: lava plateaus and pyroclastic plateaus. Lava plateau Lava plateaus are formed by highly fluid basaltic lava during numerous successive eruptions through numerous vents without violent explosions (quiet eruptions). These eruptions are quiet because of low viscosity of lava, so that it is very fluid and contains a small amount of trapped gases. The resulting sheet lava flows may be extruded from linear fissures or rifts or gigantic volcanic eruptions through multiple vents characteristic of the prehistoric era which produced giant flood basalts. Multiple successive and extensive lava flows cover the original landscape to eventually form a plateau, which may contain lava fields, cinder cones, shield volcanoes and other volcanic landforms. In some cases, a lava plateau may be part of a single volcano. An example is the massive Level Mountain shield volcano in northern British Columbia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Réunion
Réunion (; french: La Réunion, ; previously ''Île Bourbon''; rcf, label= Reunionese Creole, La Rényon) is an island in the Indian Ocean that is an overseas department and region of France. It is located approximately east of the island of Madagascar and southwest of the island of Mauritius. , it had a population of 868,846. Like the other four overseas departments, Réunion also holds the status of a region of France, and is an integral part of the French Republic. Réunion is an outermost region of the European Union and is part of the eurozone. Réunion and the fellow French overseas department of Mayotte are the only eurozone regions located in the Southern Hemisphere. As in the rest of France, the official language of Réunion is French. In addition, a majority of the region's population speaks Réunion Creole. Toponymy When France took possession of the island in the seventeenth century, it was named Bourbon, after the dynasty that then ruled France. To break ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Piton De La Fournaise
Piton de la Fournaise (; en, "Peak of the Furnace") is a shield volcano on the eastern side of Réunion island (a French overseas department and region) in the Indian Ocean. It is currently one of the most active volcanoes in the world, along with Kīlauea in the Hawaiian Islands, Stromboli and Etna in Italy and Mount Erebus in Antarctica. A previous eruption began in August 2006 and ended in January 2007. The volcano erupted again in February 2007, on 21 September 2008, on 9 December 2010, which lasted for two days, and on 1 August 2015. The most recent eruption began on 7 December 2020. The volcano is located within Réunion National Park, a World Heritage Site. Residents of Réunion sometimes refer to Piton de la Fournaise simply as ''le Volcan'' ("the Volcano"). It is a major tourist attraction on Réunion island. Geology The uppermost section of the volcano is occupied by the Enclos Fouqué, a caldera wide. High cliffs, known as ''remparts'' in French, form the calder ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Desert
A volcanic desert is an area devoid of vegetation because of volcanic activity. The term is usually applied to larger areas such as the Highlands of Iceland, the Rangipo Desert in New Zealand or Cordón Caulle in Chile. Occasionally though, it is used for relatively small regions such as the Kaʻū Desert on the island of Hawaiʻi. Volcanic deserts may have enough precipitation to sustain vegetation, but due to repeated covering of tephra and acid rain after eruptions and high percolation and infiltration rates of water, vegetation is scarce. In addition to this volcanic desert shows often poor or little soil formation due to slow chemical weathering caused by cold climate or coarse tephra. This is how the Plaine des Sables, on the island of Réunion, can find itself close to the Commerson Crater, a place which holds several world records of rainfall. Examples * Highlands of Iceland, in Iceland. * Kaʻū Desert, in the United States. * Plaine des Sables, in France. * Pum ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saint-Joseph, Réunion
Saint-Joseph () is a commune in the French overseas department of Réunion. It is located on the extreme south end of the island of Réunion. As such, it features the southernmost point of the European Union. The village Vincendo is part of the commune. Geography Climate Saint-Joseph has a tropical monsoon climate (Köppen climate classification ''Am''). The average annual temperature in Saint-Joseph is . The average annual rainfall is with February as the wettest month. The temperatures are highest on average in February, at around , and lowest in July, at around . The highest temperature ever recorded in Saint-Joseph was on 1 March 1991; the coldest temperature ever recorded was on 25 July 1996. Population See also *Communes of the Réunion department The following is a list of the 24 communes of the Réunion (an overseas department of France), along with the arrondissement (district) in which they are located, and the intercommunality of which they are a member. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sainte-Rose, Réunion
Sainte-Rose () is a Communes of France, commune on the east coast of the France, French island and department of Réunion. Geography The commune is bordered by the communes of La Plaine-des-Palmistes, Saint-Benoît, Réunion, Saint-Benoît, Saint-Joseph, Réunion, Saint-Joseph, Saint-Philippe, Réunion, Saint-Philippe and Le Tampon, Tampon; and by the Rivière de l'Est to the nord. Sainte-Rose is home to the first wind farm on the island, built in 2004. The "Pointe des Cascades", in the commune, is the easternmost part of the island and also the easternmost part of France and of the European Union. Climate Sainte-Rose features a tropical rainforest climate (Köppen climate classification, Köppen ''Af''), with substantial rainfall throughout the course of the year. Its location on the eastern side of Réunion, (Windward and leeward, windward relative to the trade winds), makes it one of the wettest cities in the world, along with Cherrapunji, Quibdó, and López de Micay. At ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Réunion National Park
Réunion National Park (french: Parc national de La Réunion) is a National Park of France located on the island of Réunion, an overseas department in the western Indian Ocean. Established on 5 March 2007, the park protects the endemic ecosystems of ''Les Hauts'', Réunion's mountainous interior, and covers around 42% of the island. Notable endemic species include the Réunion cuckooshrike and the Reunion Island day gecko. Plans for a park date back to 1985, and in a public survey in 2004, the communes of Réunion approved the creation of a national park. It officially came into existence in 2007. The park's volcanic landscape, including the Piton de la Fournaise, an active volcano, was designated a World Heritage Site in 2010, under the name "Pitons, cirques and remparts of Reunion Island" for its imposing rugged terrain and exceptional biodiversity. The park's mission, other than preserving landscape and biodiversity, is to share knowledge and welcome visitors, and to work ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lava Plateaus
Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or underwater, usually at temperatures from . The volcanic rock resulting from subsequent cooling is also often called ''lava''. A lava flow is an outpouring of lava during an effusive eruption. (An explosive eruption, by contrast, produces a mixture of volcanic ash and other fragments called tephra, not lava flows.) The viscosity of most lava is about that of ketchup, roughly 10,000 to 100,000 times that of water. Even so, lava can flow great distances before cooling causes it to solidify, because lava exposed to air quickly develops a solid crust that insulates the remaining liquid lava, helping to keep it hot and inviscid enough to continue flowing. The word ''lava'' comes from Italian and is probably derived from the Latin word ''labes'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateaus Of Africa
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateaus Of France
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Deserts
A volcano is a rupture in the Crust (geology), crust of a Planet#Planetary-mass objects, planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and volcanic gas, gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where list of tectonic plates, tectonic plates are divergent boundary, diverging or convergent boundary, 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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