Tooting (crater)
Tooting is a multi-layered Volcanic 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 . . [1] 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. [2] A later study confirms this order of magnitude estimate. [3] 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.
Page Revisions
| Year | Metadata | Sections | Top Words | First Paragraph |
| 2018 |
89087 characters 6 sections 6 paragraphs 5 images 664 internal links 15 external links |
tooting 0.563 mouginis 0.233 ejecta 0.146 crater 0.141 pits 0.134 amazonis 0.127 icarus 0.124 1625 0.117 369 0.117 3872 0.117 boyce 0.117 chemie 0.117 meteoritics 0.117 mum 0.117 1615 0.105 |
Tooting is a multi-layered Volcanic 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 . . [1] 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. [2] A later study confirms this order of magnitude estimate. [3] 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. |
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| 2017 |
48976 characters 6 sections 8 paragraphs 9 images 174 internal links 15 external links |
tooting 0.597 mouginis 0.212 ejecta 0.198 pits 0.162 crater 0.149 amazonis 0.116 icarus 0.112 1625 0.106 369 0.106 3872 0.106 boyce 0.106 chemie 0.106 meteoritics 0.106 mum 0.106 1615 0.096 |
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 . . [1] 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. [2] A later study confirms this order of magnitude estimate. [3] 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. |
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| 2016 |
54833 characters 7 sections 10 paragraphs 9 images 173 internal links 17 external links |
tooting 0.527 mouginis 0.187 ejecta 0.175 deltas 0.159 crater 0.151 pits 0.143 cracks 0.142 craters 0.136 amazonis 0.102 icarus 0.099 1625 0.094 369 0.094 3872 0.094 boyce 0.094 chemie 0.094 |
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 . . [1] 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. [2] A later study confirms this order of magnitude estimate. [3] 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. |
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| 2015 |
53731 characters 6 sections 9 paragraphs 9 images 171 internal links 16 external links |
tooting 0.475 mouginis 0.197 ejecta 0.184 deltas 0.167 pits 0.151 cracks 0.149 craters 0.143 crater 0.139 amazonis 0.108 icarus 0.104 1625 0.098 369 0.098 3872 0.098 boyce 0.098 chemie 0.098 |
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 . . [1] 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. [2] A later study confirms this order of magnitude estimate. [3] 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. |
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| 2014 |
53750 characters 6 sections 9 paragraphs 9 images 171 internal links 16 external links |
tooting 0.475 mouginis 0.197 ejecta 0.184 deltas 0.167 pits 0.151 cracks 0.149 craters 0.143 crater 0.139 amazonis 0.108 icarus 0.104 1625 0.098 369 0.098 3872 0.098 boyce 0.098 chemie 0.098 |
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 . . [1] 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. [2] A later study confirms this order of magnitude estimate. [3] 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. |
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| 2013 |
43182 characters 4 sections 7 paragraphs 6 images 171 internal links 14 external links |
tooting 0.558 mouginis 0.231 ejecta 0.180 crater 0.140 pits 0.133 amazonis 0.126 icarus 0.123 1625 0.116 369 0.116 3872 0.116 boyce 0.116 chemie 0.116 meteoritics 0.116 mum 0.116 1615 0.104 |
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 . . [1] 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. [2] A later study confirms this order of magnitude estimate. [3] 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. |
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| 2012 |
21873 characters 4 sections 7 paragraphs 2 images 28 internal links 14 external links |
tooting 0.558 mouginis 0.231 ejecta 0.180 crater 0.140 pits 0.133 amazonis 0.126 icarus 0.123 1625 0.116 369 0.116 3872 0.116 boyce 0.116 chemie 0.116 meteoritics 0.116 mum 0.116 1615 0.104 |
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 . . [1] 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. [2] A later study confirms this order of magnitude estimate. [3] 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. |
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| 2011 |
20413 characters 4 sections 6 paragraphs 2 images 28 internal links 14 external links |
tooting 0.507 amazonis 0.172 crater 0.159 1625 0.158 3872 0.158 meteoritics 0.158 mouginis 0.158 mum 0.158 ejecta 0.147 1615 0.142 suburb 0.142 stir 0.142 fluidized 0.133 flatness 0.127 town 0.126 |
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 . . [1] It was identified by planetary geologist Pete 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. [2] A later study confirms this order of magnitude estimate. [3] . A paper describing the geology and geometry of Tooting has been published in 2007 by the journal "Meteoritics and Planetary Science", vol. 42, pages 1615 - 1625. |
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| 2010 |
20363 characters 4 sections 6 paragraphs 2 images 27 internal links 14 external links |
tooting 0.507 amazonis 0.172 crater 0.159 1625 0.158 3872 0.158 meteoritics 0.158 mouginis 0.158 mum 0.158 ejecta 0.147 1615 0.142 suburb 0.142 stir 0.142 fluidized 0.133 flatness 0.127 town 0.126 |
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 . . [1] It was identified by planetary geologist Pete 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. [2] A later study confirms this order of magnitude estimate. [3] . A paper describing the geology and geometry of Tooting has been published in 2007 by the journal "Meteoritics and Planetary Science", vol. 42, pages 1615 - 1625. |
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| 2009 |
20107 characters 4 sections 6 paragraphs 2 images 27 internal links 14 external links |
tooting 0.507 amazonis 0.172 crater 0.159 1625 0.158 3872 0.158 meteoritics 0.158 mouginis 0.158 mum 0.158 ejecta 0.147 1615 0.142 suburb 0.142 stir 0.142 fluidized 0.133 flatness 0.127 town 0.126 |
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 . . [1] It was identified by planetary geologist Pete 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. [2] A later study confirms this order of magnitude estimate. [3] . A paper describing the geology and geometry of Tooting has been published in 2007 by the journal "Meteoritics and Planetary Science", vol. 42, pages 1615 - 1625. |
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| 2008 |
19262 characters 4 sections 5 paragraphs 1 images 26 internal links 14 external links |
tooting 0.411 1625 0.170 3872 0.170 meteoritics 0.170 mouginis 0.170 mum 0.170 ejecta 0.159 crater 0.154 1615 0.154 suburb 0.154 stir 0.154 fluidized 0.144 flatness 0.137 town 0.136 rampart 0.132 |
Tooting is a multi-layered fluidized ejecta crater (a type of rampart crater ) at 23.1°N, 207.1°E, in Amazonis Planitia , due west of the volcano Olympus Mons , on Mars . . [1] It was identified by planetary geologist Pete 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. [2] A later study confirms this order of magnitude estimate. [3] . A paper describing the geology and geometry of Tooting has been published in 2007 by the journal "Meteoritics and Planetary Science", vol. 42, pages 1615 - 1625. |
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| 2007 |
18850 characters 4 sections 5 paragraphs 1 images 24 internal links 13 external links |
tooting 0.410 crater 0.171 1625 0.170 3872 0.170 meteoritics 0.170 mouginis 0.170 mum 0.170 ejecta 0.159 1615 0.153 suburb 0.153 stir 0.153 fluidized 0.143 flatness 0.137 town 0.136 rampart 0.131 |
Tooting is a multi-layered fluidized ejecta crater (a type of rampart crater ) at 23.1°N, 207.1°E, in Amazonis Planitia , due west of the volcano Olympus Mons , on Mars . . [1] It was identified by planetary geologist Pete 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. [2] A later study confirms this order of magnitude estimate. [3] . A paper describing the geology and geometry of Tooting Crater has been published in 2007 by the journal "Meteoritics and Planetary Science", vol. 42, pages 1615 - 1625. |