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Tooting (crater) : ウィキペディア英語版 | Tooting (crater)
Tooting is a multi-layered fluidized ejecta crater (a type of rampart crater) at 23.1°N, 207.1°E, in Amazonis Planitia (Amazonis quadrangle), due west of the volcano Olympus Mons, on Mars. .〔(【引用サイトリンク】title=Gazetteer of Planetary Nomenclature )〕 It was identified by planetary geologist Peter Mouginis-Mark 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.〔(【引用サイトリンク】title=Tooting Crater's Tangled Tale )〕 A later study confirms this order of magnitude estimate.〔(【引用サイトリンク】url=http://www.lpi.usra.edu/meetings/chron2006/pdf/6030.pdf )〕 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 - 1625. Further papers have more recently 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 - 389), and a 2012 review paper by P.J. Mouginis-Mark and J.M. Boyce in "Chemie der Erde Geochemistry", vol. 72, p. 1 - 23. A geologic map has also been submitted in 2012 to the U.S. Geological Survey for consideration and future publication. ==Naming== Tooting is named after the London suburb of the same name. This is in accordance with the International Astronomical Union's rules for planetary nomenclature, which specify that craters on Mars less than 60 km in diameter should be named after "villages of the world with a population of less than 100,000".〔(【引用サイトリンク】title=Categories for Naming Features on Planets and Satellites )〕 The discoverer named it after his home town because he "thought () mum and brother would get a kick out of having their home town paired with a land form on Mars". This caused a stir in the British press, with many well-known media outlets reporting on the issue.
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