Trouvelot (Martian crater)
Trouvelot is a crater on Mars , located in the Oxia Palus quadrangle at 16.2° north latitude and 13.1° west longitude near the crustal dichotomy in the circum- Chryse region. It is roughly located along the dichotomy between Arabia Terra to the northeast and the southernmost of the circum-Chryse outflow channels to the southwest. Trouvelot crater measures approximately 149 kilometers in diameter and was named after Étienne Léopold Trouvelot , a French astronomer (1827–1895). The naming was adopted by IAU's Working Group for Planetary System Nomenclature in 1973. [1]
Page Revisions
| Year | Metadata | Sections | Top Words | First Paragraph |
| 2018 |
88143 characters 3 sections 10 paragraphs 6 images 666 internal links 8 external links |
trouvelot 0.603 layers 0.298 deltas 0.173 circum 0.152 chryse 0.142 sulfates 0.132 craters 0.131 places 0.119 hydrated 0.118 minerals 0.113 dichotomy 0.109 léopold 0.102 shardi 0.102 étienne 0.102 clays 0.096 |
Trouvelot is a crater on Mars , located in the Oxia Palus quadrangle at 16.2° north latitude and 13.1° west longitude near the crustal dichotomy in the circum- Chryse region. It is roughly located along the dichotomy between Arabia Terra to the northeast and the southernmost of the circum-Chryse outflow channels to the southwest. Trouvelot crater measures approximately 149 kilometers in diameter and was named after Étienne Léopold Trouvelot , a French astronomer (1827–1895). The naming was adopted by IAU's Working Group for Planetary System Nomenclature in 1973. [1] |
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| 2017 |
46295 characters 3 sections 10 paragraphs 9 images 174 internal links 8 external links |
trouvelot 0.568 layers 0.328 deltas 0.190 sulfates 0.145 craters 0.144 places 0.130 hydrated 0.130 minerals 0.124 léopold 0.112 shardi 0.112 étienne 0.112 clays 0.105 1827 0.101 oxia 0.100 toned 0.096 |
Trouvelot is a crater on Mars , located in the Oxia Palus quadrangle at 16.2° north latitude and 13.1° west longitude. It measures approximately 149 kilometers in diameter and was named after Étienne Léopold Trouvelot , a French astronomer (1827–1895). The naming was adopted by IAU's Working Group for Planetary System Nomenclature in 1973. [1] |
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| 2016 |
43540 characters 3 sections 8 paragraphs 8 images 162 internal links 8 external links |
trouvelot 0.568 layers 0.327 craters 0.198 deltas 0.190 minerals 0.186 sulfates 0.145 places 0.130 hydrated 0.130 léopold 0.112 étienne 0.112 clays 0.105 1827 0.101 toned 0.096 water 0.093 crater 0.090 |
Trouvelot Crater is a crater on Mars, located in the Oxia Palus quadrangle at 16.2° north latitude and 13.1° west longitude. It 154.7 km in diameter and was named after Étienne Léopold Trouvelot , a French astronomer (1827–1895). [1] Impact craters generally have a rim with ejecta around them, in contrast volcanic craters usually do not have a rim or ejecta deposits. As craters get larger (greater than 10 km in diameter) they usually have a central peak. [2] The peak is caused by a rebound of the crater floor following the impact. [3] There is a part of Trouvelot that displays many thin, light-toned layers; these may be evidence that a lake was present in the past. Many craters once contained lakes. [4] [5] [6] Because some crater floors show deltas, we know that water had to be present for some time. Dozens of deltas have been spotted on Mars. [7] Deltas form when sediment is washed in from a stream entering a quiet body of water. It takes a bit of time to form a delta, so the presence of a delta is exciting; it means water was there for a time, maybe for many years. Primitive organisms may have developed in such lakes; hence, some craters may be prime targets for the search for evidence of life on the Red Planet. [8] |
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| 2015 |
43538 characters 3 sections 8 paragraphs 8 images 162 internal links 8 external links |
trouvelot 0.568 layers 0.327 craters 0.198 deltas 0.190 minerals 0.186 sulfates 0.145 places 0.130 hydrated 0.130 léopold 0.112 étienne 0.112 clays 0.105 1827 0.101 toned 0.096 water 0.093 crater 0.090 |
Trouvelot Crater is a crater on Mars, located in the Oxia Palus quadrangle at 16.2° north latitude and 13.1° west longitude. It 154.7 km in diameter and was named after Étienne Léopold Trouvelot , a French astronomer (1827–1895). [1] Impact craters generally have a rim with ejecta around them, in contrast volcanic craters usually do not have a rim or ejecta deposits. As craters get larger (greater than 10 km in diameter) they usually have a central peak. [2] The peak is caused by a rebound of the crater floor following the impact. [3] There is a part of Trouvelot that displays many thin, light-toned layers; these may be evidence that a lake was present in the past. Many craters once contained lakes. [4] [5] [6] Because some crater floors show deltas, we know that water had to be present for some time. Dozens of deltas have been spotted on Mars. [7] Deltas form when sediment is washed in from a stream entering a quiet body of water. It takes a bit of time to form a delta, so the presence of a delta is exciting; it means water was there for a time, maybe for many years. Primitive organisms may have developed in such lakes; hence, some craters may be prime targets for the search for evidence of life on the Red Planet. [8] |
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| 2014 |
46060 characters 3 sections 9 paragraphs 10 images 167 internal links 8 external links |
trouvelot 0.568 layers 0.327 craters 0.198 deltas 0.190 minerals 0.186 sulfates 0.145 places 0.130 hydrated 0.130 léopold 0.112 étienne 0.112 clays 0.105 1827 0.101 toned 0.096 water 0.093 crater 0.090 |
Trouvelot Crater is a crater on Mars, located in the Oxia Palus quadrangle at 16.2° north latitude and 13.1° west longitude. It 154.7 km in diameter and was named after Étienne Léopold Trouvelot , a French astronomer (1827–1895). [1] Impact craters generally have a rim with ejecta around them, in contrast volcanic craters usually do not have a rim or ejecta deposits. As craters get larger (greater than 10 km in diameter) they usually have a central peak. [2] The peak is caused by a rebound of the crater floor following the impact. [3] There is a part of Trouvelot that displays many thin, light-toned layers; these may be evidence that a lake was present in the past. Many craters once contained lakes. [4] [5] [6] Because some crater floors show deltas, we know that water had to be present for some time. Dozens of deltas have been spotted on Mars. [7] Deltas form when sediment is washed in from a stream entering a quiet body of water. It takes a bit of time to form a delta, so the presence of a delta is exciting; it means water was there for a time, maybe for many years. Primitive organisms may have developed in such lakes; hence, some craters may be prime targets for the search for evidence of life on the Red Planet. [8] |
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| 2013 |
29011 characters 1 sections 2 paragraphs 8 images 157 internal links 1 external links |
trouvelot 0.763 léopold 0.301 étienne 0.301 1827 0.272 1895 0.199 154 0.172 oxia 0.134 french 0.111 palus 0.105 crater 0.091 astronomer 0.080 16 0.071 13 0.071 floor 0.069 longitude 0.063 |
Trouvelot Crater is a crater on Mars, located in the Oxia Palus quadrangle at 16.2° north latitude and 13.1° west longitude. It 154.7 km in diameter and was named after Étienne Léopold Trouvelot , a French astronomer (1827–1895). [1] |
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| 2012 |
7722 characters 1 sections 3 paragraphs 4 images 12 internal links 1 external links |
trouvelot 0.763 léopold 0.301 étienne 0.301 1827 0.272 1895 0.199 154 0.172 oxia 0.134 french 0.111 palus 0.105 crater 0.091 astronomer 0.080 16 0.071 13 0.071 floor 0.069 longitude 0.063 |
Trouvelot Crater is a crater on Mars, located in the Oxia Palus quadrangle at 16.2° north latitude and 13.1° west longitude. It 154.7 km in diameter and was named after Étienne Léopold Trouvelot , a French astronomer (1827–1895). [1] |
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| 2011 |
7722 characters 1 sections 3 paragraphs 5 images 12 internal links 1 external links |
trouvelot 0.763 léopold 0.301 étienne 0.301 1827 0.272 1895 0.199 154 0.172 oxia 0.134 french 0.111 palus 0.105 crater 0.091 astronomer 0.080 16 0.071 13 0.071 floor 0.069 longitude 0.063 |
Trouvelot Crater is a crater on Mars, located in the Oxia Palus quadrangle at 16.2° north latitude and 13.1° west longitude. It 154.7 km in diameter and was named after Étienne Léopold Trouvelot , a French astronomer (1827–1895). [1] |
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| 2009 |
6999 characters 1 sections 3 paragraphs 5 images 9 internal links 1 external links |
trouvelot 0.698 léopold 0.275 étienne 0.275 1827 0.248 oxia 0.246 palus 0.192 1895 0.182 154 0.157 collapsed 0.126 labeled 0.116 chaos 0.115 quadrangle 0.102 french 0.101 outflow 0.100 river 0.084 |
Trouvelot Crater is a crater on Mars, located in the Oxia Palus quadrangle at 16.2° north latitude and 13.1° west longitude. It 154.7 km in diameter and was named after Étienne Léopold Trouvelot , a French astronomer (1827-1895). [1] |