. . . . . . . . . "\u7559\u5C3C\u65FA\u71B1\u9EDE\uFF08R\u00E9union hotspot\uFF09\u662F\u4E00\u500B\u706B\u5C71\u71B1\u9EDE\uFF0C\u5176\u76EE\u524D\u4F4D\u65BC\u5370\u5EA6\u6D0B\u7559\u5C3C\u65FA\u5CF6\u3002\u800C\u67E5\u6208\u65AF-\u62C9\u514B\u6C99\u7FA4\u5CF6\u548C\u5357\u90E8\u99AC\u65AF\u514B\u6797\u6DF1\u6D77\u9AD8\u539F\u90FD\u662F\u7559\u5C3C\u65FA\u71B1\u9EDE\u7684\u75D5\u8DE1\u4E4B\u4E00\u3002"@zh . . "\u7559\u5C3C\u65FA\u71B1\u9EDE"@zh . "-21.10000038146973"^^ . "Piton de la Fournaise, an active shield volcano formed by the R\u00E9union hotspot"@en . . "Punto caldo della Riunione"@it . "\u7559\u5C3C\u65FA\u71B1\u9EDE\uFF08R\u00E9union hotspot\uFF09\u662F\u4E00\u500B\u706B\u5C71\u71B1\u9EDE\uFF0C\u5176\u76EE\u524D\u4F4D\u65BC\u5370\u5EA6\u6D0B\u7559\u5C3C\u65FA\u5CF6\u3002\u800C\u67E5\u6208\u65AF-\u62C9\u514B\u6C99\u7FA4\u5CF6\u548C\u5357\u90E8\u99AC\u65AF\u514B\u6797\u6DF1\u6D77\u9AD8\u539F\u90FD\u662F\u7559\u5C3C\u65FA\u71B1\u9EDE\u7684\u75D5\u8DE1\u4E4B\u4E00\u3002"@zh . . . . . 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"El punto caliente de Reuni\u00F3n es un punto caliente volc\u00E1nico que se encuentra actualmente bajo la isla Reuni\u00F3n en el Oc\u00E9ano \u00EDndico. La cordillera y la parte sur de la Meseta de las Mascare\u00F1as son huellas volc\u00E1nicas del punto caliente de la Reuni\u00F3n. \u200B"@es . . . . . "\u30EC\u30E6\u30CB\u30AA\u30F3\u30FB\u30DB\u30C3\u30C8\u30B9\u30DD\u30C3\u30C8\uFF08\u82F1\u8A9E: R\u00E9union hotspot\uFF09\u306F\u30A4\u30F3\u30C9\u6D0B\u306E\u30EC\u30E6\u30CB\u30AA\u30F3\u5CF6\u76F4\u4E0B\u306B\u3042\u308B\u30DB\u30C3\u30C8\u30B9\u30DD\u30C3\u30C8\u3002\u3084\u30DE\u30B9\u30AB\u30EA\u30F3\u6D77\u53F0\u5357\u90E8\u306F\u30EC\u30E6\u30CB\u30AA\u30F3\u30FB\u30DB\u30C3\u30C8\u30B9\u30DD\u30C3\u30C8\u306E\u706B\u5C71\u6D3B\u52D5\u306B\u3088\u308B\u3082\u306E\u3067\u3042\u308B\u3002 \u30EC\u30E6\u30CB\u30AA\u30F3\u30FB\u30DB\u30C3\u30C8\u30B9\u30DD\u30C3\u30C8\u306F6600\u4E07\u5E74\u4EE5\u4E0A\u306B\u308F\u305F\u3063\u3066\u6D3B\u52D5\u3057\u3066\u3044\u308B\u3068\u8003\u3048\u3089\u308C\u3066\u3044\u308B\u3002\u3053\u306E\u30DB\u30C3\u30C8\u30B9\u30DD\u30C3\u30C8\u306E6600\u4E07\u5E74\u524D\u306E\u5927\u898F\u6A21\u5674\u706B\u304C\u30A4\u30F3\u30C9\u4E2D\u592E\u90E8\u306E\u30C7\u30AB\u30F3\u30FB\u30C8\u30E9\u30C3\u30D7\u3092\u5F62\u6210\u3057\u3001\u307E\u305F\u30A4\u30F3\u30C9\u3092\u30DE\u30B9\u30AB\u30EA\u30F3\u6D77\u53F0\u304B\u3089\u5206\u96E2\u3055\u305B\u305F\u3068\u8003\u3048\u3089\u308C\u308B\u3002\u30A4\u30F3\u30C9\u304C\u5317\u3078\u5411\u304B\u3063\u305F\u5F8C\u3082\u30DB\u30C3\u30C8\u30B9\u30DD\u30C3\u30C8\u306F\u6D3B\u52D5\u3092\u7D9A\u3051\u30016000\u304B\u30894500\u4E07\u5E74\u524D\u306B\u304B\u3051\u3066\u30E9\u30C3\u30AB\u30C7\u30A3\u30F4\u8AF8\u5CF6\u3084\u30E2\u30EB\u30C7\u30A3\u30D6\u8AF8\u5CF6\u3001\u30C1\u30E3\u30B4\u30B9\u8AF8\u5CF6\u3092\u5F62\u6210\u3057\u305F\u3002\u304A\u3088\u305D4500\u4E07\u5E74\u524D\u306B\u4E2D\u592E\u6D77\u5DBA\u304C\u30DB\u30C3\u30C8\u30B9\u30DD\u30C3\u30C8\u3092\u6A2A\u5207\u308A\u3001\u30EC\u30E6\u30CB\u30AA\u30F3\u30FB\u30DB\u30C3\u30C8\u30B9\u30DD\u30C3\u30C8\u306F\u30A2\u30D5\u30EA\u30AB\u30D7\u30EC\u30FC\u30C8\u306E\u4E0B\u306B\u79FB\u3063\u305F\u3002 4500\u304B\u30891000\u4E07\u5E74\u524D\u306E\u9593\u306F\u3001\u30DB\u30C3\u30C8\u30B9\u30DD\u30C3\u30C8\u306E\u6D3B\u52D5\u306F\u4F4E\u8ABF\u3067\u3042\u3063\u305F\u3002\u305D\u306E\u5F8C\u6D3B\u52D5\u3092\u518D\u958B\u3057\u30DE\u30B9\u30AB\u30EA\u30F3\u8AF8\u5CF6\u3092\u5F62\u6210\u3057\u305F\u3002\u30E2\u30FC\u30EA\u30B7\u30E3\u30B9\u3084\u30ED\u30C9\u30EA\u30B2\u30B9\u6D77\u5DBA\u306F1000\u304B\u3089800\u4E07\u5E74\u524D\u306B\u3001\u30ED\u30C9\u30EA\u30B2\u30B9\u5CF6\u3084\u30EC\u30E6\u30CB\u30AA\u30F3\u5CF6\u306F\u904E\u53BB200\u4E07\u5E74\u306E\u9593\u306B\u51FA\u6765\u305F\u3002\u30EC\u30E6\u30CB\u30AA\u30F3\u5CF6\u306E\u30D4\u30C8\u30F3\u30FB\u30C9\u30A5\u30FB\u30E9\u30FB\u30D5\u30EB\u30CD\u30FC\u30BA\u5C71\u306F\u4E16\u754C\u3067\u3082\u6D3B\u767A\u306B\u6D3B\u52D5\u3057\u3066\u3044\u308B\u706B\u5C71\u306E\u4E00\u3064\u3067\u3042\u308A\u3001\u6700\u8FD1\u3067\u306F2015\u5E748\u6708\u306B\u5674\u706B\u3057\u3066\u3044\u308B\u3002"@ja . . "1055908"^^ . . "France"@en . . . . . . . . . . . "The R\u00E9union hotspot is a volcanic hotspot which currently lies under the island of R\u00E9union in the Indian Ocean. The Chagos-Laccadive Ridge and the southern part of the Mascarene Plateau are volcanic traces of the R\u00E9union hotspot."@en . . . "R\u00E9union hotspot"@en . . . . . . . . . "Punto caliente de Reuni\u00F3n"@es . "Le point chaud de La R\u00E9union est un point chaud volcanique qui se trouve sous La R\u00E9union, dans l'oc\u00E9an Indien."@fr . . . "R\u00E9union hotspot"@en . "1113102158"^^ . . "Point chaud de La R\u00E9union"@fr . . . . 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"POINT(55.5 -21.10000038147)"^^ . . "-21.1 55.5" . "4695"^^ . "El punto caliente de Reuni\u00F3n es un punto caliente volc\u00E1nico que se encuentra actualmente bajo la isla Reuni\u00F3n en el Oc\u00E9ano \u00EDndico. La cordillera y la parte sur de la Meseta de las Mascare\u00F1as son huellas volc\u00E1nicas del punto caliente de la Reuni\u00F3n. \u200B Se cree que este punto caliente ha estado activo durante m\u00E1s de 65 millones de a\u00F1os. Se cree que una enorme erupci\u00F3n de este punto caliente hace 65 millones de a\u00F1os form\u00F3 las escaleras del Dec\u00E1n, un vasto lecho de lava bas\u00E1ltica que cubre parte de la India central, y abri\u00F3 una grieta que separ\u00F3 la India de la meseta Seychelles. La erupci\u00F3n de las escaleras del Dec\u00E1n coincidi\u00F3 aproximadamente con la ant\u00EDpoda del impacto de Chicxulub y la extinci\u00F3n masiva del Cret\u00E1cico-Pale\u00F3geno, que provoc\u00F3 la desaparici\u00F3n de los dinosaurios. Existe una considerable especulaci\u00F3n sobre si los tres eventos estuvieron relacionados.\u200B\u200B A medida que la placa India se desplazaba hacia el norte, el punto caliente continu\u00F3 perforando la placa, creando una cadena de islas volc\u00E1nicas y mesetas submarinas. Las Islas Laquedivas, las Maldivas, y el archipi\u00E9lago de Chagos son atolones que descansan sobre antiguos volcanes creados hace 45-60 millones de a\u00F1os que posteriormente quedaron sumergidos en el mar. Hace aproximadamente 45 millones de a\u00F1os, la Cordillera India Central el punto caliente, y este pas\u00F3 bajo la placa Africana. El punto caliente de Reuni\u00F3n parece haber estado relativamente tranquilo desde hace 45 a 10 millones de a\u00F1os, cuando se reanud\u00F3 su actividad, creando las Islas Mascare\u00F1as, que incluyen Mauricio, Reuni\u00F3n, y Rodrigues. Mauricio y la cordillera Rodrigues fueron creadas hace 8-10 millones de a\u00F1os, y Rodrigues y las islas Reuni\u00F3n en los \u00FAltimos dos millones de a\u00F1os. El Pit\u00F3n de la Fournaise, un volc\u00E1n en escudo en el extremo sureste de Reuni\u00F3n, es uno de los volcanes m\u00E1s activos del mundo, que entr\u00F3 en erupci\u00F3n por \u00FAltima vez en octubre de 2019.\u200B"@es . "Le point chaud de La R\u00E9union est un point chaud volcanique qui se trouve sous La R\u00E9union, dans l'oc\u00E9an Indien."@fr . . . . "The R\u00E9union hotspot is a volcanic hotspot which currently lies under the island of R\u00E9union in the Indian Ocean. The Chagos-Laccadive Ridge and the southern part of the Mascarene Plateau are volcanic traces of the R\u00E9union hotspot. The hotspot is believed to have been active for over 65 million years. A huge eruption of this hotspot 65 million years ago is thought to have laid down the Deccan Traps, a vast bed of basalt lava that covers part of central India, and opened a rift which separated India from the Seychelles Plateau. The Deccan Traps eruption coincided roughly with the nearly antipodal Chicxulub impactor and the Cretaceous\u2013Paleogene extinction of the dinosaurs, and there is considerable speculation that the three events were related. As the Indian plate drifted north, the hotspot continued to punch through the plate, creating a string of volcanic islands and undersea plateaux. The Laccadive Islands, the Maldives, and the Chagos Archipelago are atolls resting on former volcanoes created 60\u201345 million years ago that subsequently submerged below sea level. About 45 million years ago the Central Indian Ridge crossed over the hotspot, and the hotspot passed under the African Plate. The hotspot appears to have been relatively quiet 45\u201310 million years ago, when activity resumed, creating the Mascarene Islands, which include Mauritius, R\u00E9union, and Rodrigues. Mauritius and Rodrigues Ridge were created 8\u201310 million years ago, and Rodrigues and R\u00E9union Islands in the last two million years. Piton de la Fournaise, a shield volcano on the southeastern corner of R\u00E9union, is one of the most active volcanoes in the world, erupting last in December 2020."@en . . . "\u0420\u0435\u044E\u043D\u044C\u0439\u043E\u043D (\u0433\u0430\u0440\u044F\u0447\u0430 \u0442\u043E\u0447\u043A\u0430)"@uk . . . "Il punto caldo della Riunione \u00E8 un punto caldo vulcanico che attualmente giace al di sotto dell'isola della Riunione (La R\u00E9union in francese), un dipartimento d'oltremare francese nell'arcipelago delle isole Mascarene, nell'Oceano Indiano occidentale. La dorsale Chagos-Laccadive e la parte meridionale del pianoro delle Mascarene sono tracce evidenti dell'attivit\u00E0 vulcanica di questo punto caldo. Si pensa che il punto caldo di Riunione sia stato attivo per oltre 66 milioni di anni e si ritiene che una sua enorme eruzione, 66 milioni di anni fa, abbia originato i trappi del Deccan, una serie di vaste colate di lava basaltica solidificata che copre parte dell'India centrale arrivando a uno spessore di 2.000 m e a un'estensione totale di 500.000 km\u00B2, generando anche lo sciame di faglie che ha portato alla divisione dell'India dall'arcipelago delle Seychelles e quindi dal pianoro della Mascarene. Tale eruzione all'origine della formazione dei trappi del Deccan \u00E8 avvenuta grosso modo in coincidenza con l'estinzione dei dinosauri e ci\u00F2 ha quindi portato ad alcune ipotesi circa la correlazione dei due avvenimenti. Man mano che la placca indiana si \u00E8 spostata verso nord-ovest il punto caldo ha continuato la sua attivit\u00E0 portando alla formazione di una serie di isole vulcaniche e plateau oceanici. Resti di questa attivit\u00E0, formati tra i 60 e i 45 milioni di anni fa, sono gli arcipelaghi delle isole Laccadive, Maldive e Chagos che sono via via emersi dal fondo marino. Circa 45 milioni di anni fa, quella che era ancora una zona di rift e che sarebbe diventata poi la dorsale medio-indiana e quindi un vero e proprio margine divergente, oltrepass\u00F2, nel movimento delle placche verso nord-ovest, il punto caldo di Riunione a una latitudine di circa 18-20\u00B0S, facendolo cos\u00EC passare al di sotto della placca africana da quella che allora era la placca indo-australiana. Sembra che il punto caldo abbia fortemente rallentato la sua attivit\u00E0 in un periodo che va da 45 a 10 milioni di anni fa per poi riattivarsi del tutto e portare alla formazione delle isole Mauritius, Riunione (o R\u00E9union) e Rodrigues. In particolare, l'isola di Mauritius e la dorsale di Rodrigues si sono formate tra i 10 e gli 8 milioni di anni fa mentre le isole di Rodrigues e di Riunione sono state create negli ultimi due milioni di anni. Il Piton de la Fournaise, un vulcano a scudo nella regione sudorientale di Riunione, di cui costituisce circa il 40% della superficie, \u00E8 uno dei vulcani pi\u00F9 attivi del mondo, le sue ultime eruzioni risalgono a giugno 2014, ad agosto 2015 e a maggio-giugno 2016."@it . . . . . . . "55.5"^^ . . . "\u30EC\u30E6\u30CB\u30AA\u30F3\u30FB\u30DB\u30C3\u30C8\u30B9\u30DD\u30C3\u30C8"@ja . . . "Il punto caldo della Riunione \u00E8 un punto caldo vulcanico che attualmente giace al di sotto dell'isola della Riunione (La R\u00E9union in francese), un dipartimento d'oltremare francese nell'arcipelago delle isole Mascarene, nell'Oceano Indiano occidentale. La dorsale Chagos-Laccadive e la parte meridionale del pianoro delle Mascarene sono tracce evidenti dell'attivit\u00E0 vulcanica di questo punto caldo."@it . . .