Tyrrhenus Mons
Tyrrhenus Mons , [1] formerly Tyrrhena Mons [2] or Tyrrhena Patera , is a large volcano in the Mare Tyrrhenum quadrangle of Mars, located at 21.36° south latitude and 253.47° west longitude. The name "Tyrrhena Patera" now refers only to the central depression, a volcanic crater or caldera. [3] It was named after a classical albedo feature name. [1] Pit chains are found at the summit of Tyrrhenus Mons. They are formed by collapse of material into underground voids. Since they form chains and concentric fractures that are aligned, they are probably caused by extension of the surface. Volcanic processes made the crust pull apart. Voids were formed, then material fell into them, leaving holes. It is one of the oldest volcanoes on Mars. As a consequence of its old age, Tyrrhenus Mons has many radiating gullies on its slope. When it was formed, magma may have gone through frozen ground and then erupted as easily eroded ash, instead of lava flows. [4] [5]
Page Revisions
| Year | Metadata | Sections | Top Words | First Paragraph |
| 2018 |
38320 characters 2 sections 5 paragraphs 10 images 157 internal links 5 external links |
tyrrhenus 0.642 tyrrhena 0.339 mons 0.302 chains 0.228 tyrrhenum 0.197 voids 0.189 patera 0.148 pit 0.142 mare 0.118 volcano 0.114 253 0.106 radiating 0.095 erupted 0.087 caldera 0.084 aligned 0.083 |
Tyrrhenus Mons , [1] formerly Tyrrhena Mons [2] or Tyrrhena Patera , is a large volcano in the Mare Tyrrhenum quadrangle of Mars, located at 21.36° south latitude and 253.47° west longitude. The name "Tyrrhena Patera" now refers only to the central depression, a volcanic crater or caldera. [3] It was named after a classical albedo feature name. [1] Pit chains are found at the summit of Tyrrhenus Mons. They are formed by collapse of material into underground voids. Since they form chains and concentric fractures that are aligned, they are probably caused by extension of the surface. Volcanic processes made the crust pull apart. Voids were formed, then material fell into them, leaving holes. It is one of the oldest volcanoes on Mars. As a consequence of its old age, Tyrrhenus Mons has many radiating gullies on its slope. When it was formed, magma may have gone through frozen ground and then erupted as easily eroded ash, instead of lava flows. [4] [5] |
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| 2017 |
39177 characters 2 sections 5 paragraphs 10 images 158 internal links 7 external links |
tyrrhenus 0.642 tyrrhena 0.339 mons 0.302 chains 0.228 tyrrhenum 0.197 voids 0.189 patera 0.148 pit 0.142 mare 0.118 volcano 0.114 253 0.106 radiating 0.095 erupted 0.087 caldera 0.084 aligned 0.083 |
Tyrrhenus Mons , [1] formerly Tyrrhena Mons [2] or Tyrrhena Patera , is a large volcano in the Mare Tyrrhenum quadrangle of Mars, located at 21.36° south latitude and 253.47° west longitude. The name "Tyrrhena Patera" now refers only to the central depression, a volcanic crater or caldera. [3] It was named after a classical albedo feature name. [1] Pit chains are found at the summit of Tyrrhenus Mons. They are formed by collapse of material into underground voids. Since they form chains and concentric fractures that are aligned, they are probably caused by extension of the surface. Volcanic processes made the crust pull apart. Voids were formed, then material fell into them, leaving holes. It is one of the oldest volcanoes on Mars. As a consequence of its old age, Tyrrhenus Mons has many radiating gullies on its slope. When it was formed, magma may have gone through frozen ground and then erupted as easily eroded ash, instead of lava flows. [4] [5] |
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| 2016 |
37464 characters 2 sections 4 paragraphs 10 images 156 internal links 6 external links |
tyrrhenus 0.642 tyrrhena 0.339 mons 0.302 chains 0.228 tyrrhenum 0.197 voids 0.189 patera 0.148 pit 0.142 mare 0.118 volcano 0.114 253 0.106 radiating 0.095 erupted 0.087 caldera 0.084 aligned 0.083 |
Tyrrhenus Mons , [1] formerly Tyrrhena Mons [2] or Tyrrhena Patera , is a large volcano in the Mare Tyrrhenum quadrangle of Mars, located at 21.36° south latitude and 253.47° west longitude. The name "Tyrrhena Patera" now refers only to the central depression, a volcanic crater or caldera. [3] It was named after a classical albedo feature name. [1] Pit chains are found at the summit of Tyrrhenus Mons. They are formed by collapse of material into underground voids. Since they form chains and concentric fractures that are aligned, they are probably caused by extension of the surface. Volcanic processes made the crust pull apart. Voids were formed, then material fell into them, leaving holes. It is one of the oldest volcanoes on Mars. As a consequence of its old age, Tyrrhenus Mons has many radiating gullies on its slope. When it was formed, magma may have gone through frozen ground and then erupted as easily eroded ash, instead of lava flows. [4] [5] |
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| 2014 |
37463 characters 2 sections 4 paragraphs 10 images 156 internal links 6 external links |
tyrrhenus 0.645 tyrrhena 0.340 mons 0.303 chains 0.229 tyrrhenum 0.198 voids 0.190 patera 0.149 pit 0.142 mare 0.118 volcano 0.114 253 0.106 radiating 0.095 caldera 0.084 aligned 0.083 summit 0.078 |
Tyrrhenus Mons , [1] formerly Tyrrhena Mons [2] or Tyrrhena Patera , is a large volcano in the Mare Tyrrhenum quadrangle of Mars, located at 21.36° south latitude and 253.47° west longitude. The name "Tyrrhena Patera" now refers only to the central depression, a volcanic crater or caldera. [3] It was named after a classical albedo feature name. [1] Pit chains are found at the summit of Tyrrhenus Mons. They are formed by collapse of material into underground voids. Since they form chains and concentric fractures that are aligned, they are probably caused by extension of the surface. Volcanic processes made the crust pull apart. Voids were formed, then material fell into them, leaving holes. It is one of the oldest volcanoes on Mars. As a consequence of its old age, Tyrrhenus Mons has many radiating gullies on its slope. When it was formed, magma may have gone through frozen ground and then eruped as easily eroded ash, instead of lava flows. [4] [5] |
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| 2013 |
35638 characters 1 sections 3 paragraphs 8 images 157 internal links 6 external links |
tyrrhenus 0.611 tyrrhena 0.322 mons 0.287 chains 0.217 tyrrhenum 0.188 voids 0.180 patera 0.141 ehsan 0.137 sanaei 0.137 yazd 0.137 concentric 0.135 pit 0.135 mare 0.112 volcano 0.108 club 0.105 |
Tyrrhenus Mons , [1] formerly Tyrrhena Mons [2] or Tyrrhena Patera , is a large volcano in the Mare Tyrrhenum quadrangle of Mars, located at 21.36° south latitude and 253.47° west longitude. The name "Tyrrhena Patera" now refers only to the central depression, a volcanic crater or caldera. [3] It was named after a classical albedo feature name. [1] Pit chains are found at the summit of Tyrrhenus Mons. They are formed by collapse of material into underground voids. Since they form chains and concentric fractures that are aligned, they are probably caused by extension of the surface. Volcanic processes made the crust pull apart. Voids were formed, then material fell into them, leaving holes. It is one of the oldest volcanoes on Mars. As a consequence of its old age, Tyrrhenus Mons has many radiating gullies on its slope. When it was formed, magma may have gone through frozen ground and then eruped as easily eroded ash, instead of lava flows. [4] [5] |
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| 2012 |
14338 characters 1 sections 4 paragraphs 4 images 12 internal links 6 external links |
tyrrhenus 0.611 tyrrhena 0.322 mons 0.287 chains 0.217 tyrrhenum 0.188 voids 0.180 patera 0.141 ehsan 0.137 sanaei 0.137 yazd 0.137 concentric 0.135 pit 0.135 mare 0.112 volcano 0.108 club 0.105 |
Tyrrhenus Mons , [1] formerly Tyrrhena Mons [2] or Tyrrhena Patera , is a large volcano in the Mare Tyrrhenum quadrangle of Mars, located at 21.36° south latitude and 253.47° west longitude. The name "Tyrrhena Patera" now refers only to the central depression, a volcanic crater or caldera. [3] It was named after a classical albedo feature name. [1] Pit chains are found at the summit of Tyrrhenus Mons. They are formed by collapse of material into underground voids. Since they form chains and concentric fractures that are aligned, they are probably caused by extension of the surface. Volcanic processes made the crust pull apart. Voids were formed, then material fell into them, leaving holes. It is one of the oldest volcanoes on Mars. As a consequence of its old age, Tyrrhenus Mons has many radiating gullies on its slope. When it was formed, magma may have gone through frozen ground and then eruped as easily eroded ash, instead of lava flows. [4] [5] |
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| 2011 |
9108 characters 1 sections 3 paragraphs 3 images 7 internal links 2 external links |
tyrrhena 0.482 patera 0.421 tyrrhenum 0.281 voids 0.269 chains 0.217 mare 0.168 volcano 0.162 253 0.150 radiating 0.135 aligned 0.118 summit 0.111 consequence 0.111 pull 0.105 ash 0.104 formed 0.102 |
Tyrrhena Patera is the central depression of a large volcano in the Mare Tyrrhenum quadrangle of Mars, located at 21.36° south latitude and 253.47° west longitude. It was named after a classical albedo feature name. [1] Pit chains are found at the summit of Tyrrhena Patera. They are formed by collapse of material into underground voids. Since they form chains and concentric fractures that are aligned, they are probably caused by extension of the surface. Volcanic processes made the crust pull apart. Voids were formed, then material fell into them, leaving holes. It is one of the oldest volcanoes on Mars. As a consequence of its old age, Tyrrhena Patera has many radiating gullies on its slope. When it was formed, magma may have gone through frozen ground and then eruped as easily eroded ash, instead of lava flows. [2] [3] |
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| 2010 |
6583 characters 1 sections 3 paragraphs 3 images 6 internal links 1 external links |
tyrrhena 0.499 patera 0.409 chains 0.252 tyrrhenum 0.218 voids 0.209 volcano 0.189 ehsan 0.159 sanaei 0.159 yazd 0.159 concentric 0.157 pit 0.156 mare 0.130 club 0.122 253 0.117 iran 0.115 |
Tyrrhena Patera is the central depression of a large volcano in the Mare Tyrrhenum quadrangle of Mars, located at 21.36° south latitude and 253.47° west longitude. It was named after a classical albedo feature name. [1] Pit chains are found at the summit of Tyrrhena Patera. They are formed by collapse of material into underground voids. Since they form chains and concentric fractures that are aligned, they are probably caused by extension of the surface. Volcanic processes made the crust pull apart. Voids were formed, then material fell into them, leaving holes. It is one of the oldest volcanoes on Mars. As a consequence of its old age, Tyrrhena Patera has many radiating gullies on its slope. When it was formed, magma may have gone through frozen ground and then eruped as easily eroded ash, instead of lava flows. [2] [3] |
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| 2009 |
6418 characters 1 sections 3 paragraphs 3 images 7 internal links 1 external links |
tyrrhena 0.499 patera 0.409 chains 0.252 tyrrhenum 0.218 voids 0.209 volcano 0.189 ehsan 0.159 sanaei 0.159 yazd 0.159 concentric 0.157 pit 0.156 mare 0.130 club 0.122 253 0.117 iran 0.115 |
Tyrrhena Patera is the central depression of a large volcano in the Mare Tyrrhenum quadrangle of Mars, located at 21.36° south latitude and 253.47° west longitude. It was named after a classical albedo feature name. [1] Pit chains are found at the summit of Tyrrhena Patera. They are formed by collapse of material into underground voids. Since they form chains and concentric fractures that are aligned, they are probably caused by extension of the surface. Volcanic processes made the crust pull apart. Voids were formed, then material fell into them, leaving holes. It is one of the oldest volcanoes on Mars. As a consequence of its old age, Tyrrhena Patera has many radiating gullies on its slope. When it was formed, magma may have gone through frozen ground and then eruped as easily eroded ash, instead of lava flows. [2] |