Libya Montes
The Libya Montes are a highland terrain on Mars up-lifted by the giant impact that created the Isidis basin to the north.
Page Revisions
| Year | Metadata | Sections | Top Words | First Paragraph |
| 2017 |
33697 characters 3 sections 6 paragraphs 9 images 156 internal links 10 external links |
libya 0.462 isidis 0.334 montes 0.280 esp 0.231 1830 0.199 basin 0.179 fluvial 0.147 018223 0.137 018368 0.137 03051 0.137 m02 0.137 msss 0.137 angles 0.131 hesperian 0.124 valleys 0.120 |
The Libya Montes are a highland terrain on Mars up-lifted by the giant impact that created the Isidis basin to the north. |
|
| 2016 |
31804 characters 3 sections 6 paragraphs 9 images 155 internal links 9 external links |
libya 0.462 isidis 0.334 montes 0.280 esp 0.231 1830 0.199 basin 0.179 fluvial 0.147 018223 0.137 018368 0.137 03051 0.137 m02 0.137 msss 0.137 angles 0.131 hesperian 0.124 valleys 0.120 |
The Libya Montes are a highland terrain on Mars up-lifted by the giant impact that created the Isidis basin to the north. |
|
| 2015 |
31536 characters 3 sections 6 paragraphs 9 images 154 internal links 9 external links |
libya 0.462 isidis 0.334 montes 0.280 esp 0.231 1830 0.199 basin 0.179 fluvial 0.147 018223 0.137 018368 0.137 03051 0.137 m02 0.137 msss 0.137 angles 0.131 hesperian 0.124 valleys 0.120 |
The Libya Montes are a highland terrain on Mars up-lifted by the giant impact that created the Isidis basin to the north. |
|
| 2013 |
30970 characters 3 sections 6 paragraphs 9 images 154 internal links 9 external links |
libya 0.462 isidis 0.334 montes 0.280 esp 0.231 1830 0.199 basin 0.179 fluvial 0.147 018223 0.137 018368 0.137 03051 0.137 m02 0.137 msss 0.137 angles 0.131 hesperian 0.124 valleys 0.120 |
The Libya Montes are a highland terrain on Mars up-lifted by the giant impact that created the Isidis basin to the north. |
|
| 2012 |
9666 characters 3 sections 6 paragraphs 5 images 10 internal links 9 external links |
libya 0.430 pareidolia 0.322 isidis 0.310 montes 0.261 esp 0.215 1830 0.185 basin 0.167 fluvial 0.136 018223 0.127 018368 0.127 03051 0.127 m02 0.127 msss 0.127 angles 0.122 hesperian 0.115 |
The Libya Montes are a highland terrain on Mars up-lifted by the giant impact that created the Isidis basin to the north. |
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| 2011 |
8051 characters 2 sections 3 paragraphs 5 images 11 internal links 6 external links |
libya 0.554 montes 0.252 isidis 0.250 mountains 0.236 03051 0.205 m02 0.205 msss 0.205 facial 0.185 pareidolia 0.173 cydonia 0.165 basin 0.134 crop 0.133 giant 0.123 iapygia 0.122 trigger 0.122 |
The Libya Montes are a ring of mountains on Mars up-lifted by the giant impact that created the Isidis basin to the north. During 1999, this region became one of the top two that were being considered for the now-canceled Mars Surveyor 2001 Lander . The Isidis basin is very, very ancient. Thus, the mountains that form its rims would contain some of the oldest rocks available at the Martian surface, and a landing in this region might potentially provide information about conditions on early Mars. After they formed by giant impact, the Libya Mountains and valleys were subsequently modified and eroded by other processes, including wind, impact cratering, and flow of liquid water to make the many small valleys. [2] |
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| 2010 |
5796 characters 1 sections 3 paragraphs 3 images 8 internal links 2 external links |
libya 0.574 isidis 0.345 mountains 0.326 montes 0.232 basin 0.186 giant 0.169 iapygia 0.168 valleys 0.165 cratering 0.145 lifted 0.139 rims 0.136 canceled 0.132 oldest 0.118 modified 0.114 networks 0.108 |
The Libya Montes are a ring of mountains on Mars up-lifted by the giant impact that created the Isidis basin to the north. During 1999, this region became one of the top two that were being considered for the now-canceled Mars Surveyor 2001 Lander . The Isidis basin is very, very ancient. Thus, the mountains that form its rims would contain some of the oldest rocks available at the Martian surface, and a landing in this region might potentially provide information about conditions on early Mars. After they formed by giant impact, the Libya Mountains and valleys were subsequently modified and eroded by other processes, including wind, impact cratering, and flow of liquid water to make the many small valleys. [2] |
|
| 2009 |
5426 characters 1 sections 3 paragraphs 3 images 8 internal links 1 external links |
libya 0.574 isidis 0.345 mountains 0.326 montes 0.232 basin 0.186 giant 0.169 iapygia 0.168 valleys 0.165 cratering 0.145 lifted 0.139 rims 0.136 canceled 0.132 oldest 0.118 modified 0.114 networks 0.108 |
The Libya Montes are a ring of mountains on Mars up-lifted by the giant impact that created the Isidis basin to the north. During 1999, this region became one of the top two that were being considered for the now-canceled Mars Surveyor 2001 Lander . The Isidis basin is very, very ancient. Thus, the mountains that form its rims would contain some of the oldest rocks available at the Martian surface, and a landing in this region might potentially provide information about conditions on early Mars. After they formed by giant impact, the Libya Mountains and valleys were subsequently modified and eroded by other processes, including wind, impact cratering, and flow of liquid water to make the many small valleys. [1] |
|
| 2008 |
5013 characters 1 sections 1 paragraphs 2 images 6 internal links 1 external links |
libya 0.450 isidis 0.406 mountains 0.384 basin 0.218 giant 0.199 valleys 0.194 cratering 0.170 lifted 0.164 rims 0.160 canceled 0.156 oldest 0.139 montes 0.136 modified 0.134 subsequently 0.127 1999 0.119 |
The Libya Montes are a ring of mountains on Mars up-lifted by the giant impact that created the Isidis basin to the north. During 1999, this region became one of the top two that were being considered for the now-canceled Mars Surveyor 2001 Lander . The Isidis basin is very, very ancient. Thus, the mountains that form its rims would contain some of the oldest rocks available at the Martian surface, and a landing in this region might potentially provide information about conditions on early Mars. After they formed by giant impact, the Libya Mountains and valleys were subsequently modified and eroded by other processes, including wind, impact cratering, and flow of liquid water to make the many small valleys. [1] |