"\u675C\u4E01\u649E\u64CA\u5751\uFF08\u82F1\u8A9E\uFF1ATooting\uFF09\u662F\u4E00\u500B\u4F4D\u65BC\u706B\u661F\u4E9E\u99AC\u905C\u5E73\u539F\uFF08\u4E9E\u99AC\u905C\u5340\uFF09\u7684\u4E00\u500B\uFF08Rampart crater\uFF09\uFF0C\u4E2D\u5FC3\u5EA7\u6A1923.1\u00B0N, 207.1\u00B0E\uFF0C\u4F4D\u5728\u706B\u5C71\u5967\u6797\u5E15\u65AF\u5C71\u897F\u65B9\u3002"@zh . . "1088241864"^^ . . "7521"^^ . . "London suburb"@en . . "11289364"^^ . . . . . . . . . . "Tooting \u00E8 un cratere sulla superficie di Marte."@it . . . . . . . . . . . "Tooting is an impact crater (of the type rampart crater) with volcanic features at 23.1\u00B0N, 207.1\u00B0E, in Amazonis Planitia (Amazonis quadrangle), due west of the volcano Olympus Mons, on Mars. It was identified by planetary geologist in September 2004. Scientists estimate that its age is on the order of hundreds of thousands of years, which is relatively young for a Martian crater. A later study confirms this order of magnitude estimate. A preliminary paper describing the geology and geometry of Tooting was published in 2007 by the journal Meteoritics and Planetary Science, vol. 42, pages 1615\u20131625. Further papers have been published, including a 2010 analysis of flows on the walls of Tooting crater by A. R. Morris et al. (Icarus vol. 209, p. 369\u2013389), and a 2012 review paper by P.J. Mouginis-Mark and J.M. Boyce in Chemie der Erde Geochemistry, vol. 72, p. 1\u201323. A geologic map has also been submitted in 2012 to the U.S. Geological Survey for consideration and future publication."@en . . "Tooting (crater)"@es . . "300"^^ . . . . . "Tooting"@en . . . "#FA8072"@en . . . . . "Cratere Tooting"@it . . . "Tooting (crater)"@en . . . . . . . "\u675C\u4E01\u649E\u64CA\u5751\uFF08\u82F1\u8A9E\uFF1ATooting\uFF09\u662F\u4E00\u500B\u4F4D\u65BC\u706B\u661F\u4E9E\u99AC\u905C\u5E73\u539F\uFF08\u4E9E\u99AC\u905C\u5340\uFF09\u7684\u4E00\u500B\uFF08Rampart crater\uFF09\uFF0C\u4E2D\u5FC3\u5EA7\u6A1923.1\u00B0N, 207.1\u00B0E\uFF0C\u4F4D\u5728\u706B\u5C71\u5967\u6797\u5E15\u65AF\u5C71\u897F\u65B9\u3002"@zh . "Tooting \u00E8 un cratere sulla superficie di Marte."@it . . . . . . . . "Tooting is an impact crater (of the type rampart crater) with volcanic features at 23.1\u00B0N, 207.1\u00B0E, in Amazonis Planitia (Amazonis quadrangle), due west of the volcano Olympus Mons, on Mars. It was identified by planetary geologist in September 2004. Scientists estimate that its age is on the order of hundreds of thousands of years, which is relatively young for a Martian crater. A later study confirms this order of magnitude estimate. A preliminary paper describing the geology and geometry of Tooting was published in 2007 by the journal Meteoritics and Planetary Science, vol. 42, pages 1615\u20131625. Further papers have been published, including a 2010 analysis of flows on the walls of Tooting crater by A. R. Morris et al. (Icarus vol. 209, p. 369\u2013389), and a 2012 review paper by P.J. Mougin"@en . "\u675C\u4E01\u649E\u64CA\u5751"@zh . . . . . . . . . . "Tooting es un cr\u00E1ter de impacto con caracter\u00EDsticas volc\u00E1nicas a (23,1 \u00B0Norte, 207,1 \u00B0Este), en la zona conocida como Amazonis Planitia, al oeste del volc\u00E1n Olympus Mons, en Marte . \u200B Fue identificado por el ge\u00F3logo planetario Peter Mouginis-Mark en septiembre de 2004. Los cient\u00EDficos estiman que la edad es del orden de cientos de miles de a\u00F1os, lo que es relativamente joven para un cr\u00E1ter marciano. \u200B Un estudio posterior confirma esta estimaci\u00F3n de magnitud. \u200B Un art\u00EDculo preliminar que describe la geolog\u00EDa y geometr\u00EDa de Tooting fue publicado en 2007 por la revista Meteoritics and Planetary Science, vol. 42, p\u00E1ginas 1615\u20131625. Se han publicado m\u00E1s art\u00EDculos m\u00E1s recientemente, incluido un an\u00E1lisis de 2010 de los flujos en las paredes del cr\u00E1ter Tooting por A. R. Morris y col. ( Icarus vol. 209, p. 369\u2013389), y un art\u00EDculo de revisi\u00F3n de 2012 de PJ Mouginis-Mark y JM Boyce en Chemie der Erde Geochemistry, vol. 72, p\u00E1g. 1-23. Tambi\u00E9n se envi\u00F3 un mapa geol\u00F3gico en 2012 al Servicio Geol\u00F3gico de EE. UU. Para su consideraci\u00F3n y publicaci\u00F3n futura."@es . . . . . . . . "Tooting es un cr\u00E1ter de impacto con caracter\u00EDsticas volc\u00E1nicas a (23,1 \u00B0Norte, 207,1 \u00B0Este), en la zona conocida como Amazonis Planitia, al oeste del volc\u00E1n Olympus Mons, en Marte . \u200B Fue identificado por el ge\u00F3logo planetario Peter Mouginis-Mark en septiembre de 2004. Los cient\u00EDficos estiman que la edad es del orden de cientos de miles de a\u00F1os, lo que es relativamente joven para un cr\u00E1ter marciano. \u200B Un estudio posterior confirma esta estimaci\u00F3n de magnitud. \u200B Un art\u00EDculo preliminar que describe la geolog\u00EDa y geometr\u00EDa de Tooting fue publicado en 2007 por la revista Meteoritics and Planetary Science, vol. 42, p\u00E1ginas 1615\u20131625. Se han publicado m\u00E1s art\u00EDculos m\u00E1s recientemente, incluido un an\u00E1lisis de 2010 de los flujos en las paredes del cr\u00E1ter Tooting por A. R. Morris y col. ( Icarus vol"@es . "Mars"@en .