Enipeus Vallis is a valley in the northern hemisphere of the planet Mars . It is centered at lat. 37°N, long. 267°E in the Arcadia quadrangle (MC-3) between the large volcano Alba Mons and the Tempe Terra plateau. The valley follows a gently sinuous , north-south path for a distance of about 357 km (222 mi). [2] It is likely an ancient watercourse that formed during the early Hesperian (or late Noachian ) period, [3] around 3.7 billion years ago. [4]
Year | Metadata | Sections | Top Words | First Paragraph |
2018 |
98114 characters 6 sections 14 paragraphs 6 images 675 internal links 13 external links |
enipeus 0.629 valley 0.354 tempe 0.225 vallis 0.219 fluvial 0.174 bedforms 0.126 lat 0.118 channels 0.117 stream 0.110 levee 0.108 segment 0.102 267 0.099 vis 0.096 plateau 0.086 alba 0.084 |
Enipeus Vallis is a valley in the northern hemisphere of the planet Mars . It is centered at lat. 37°N, long. 267°E in the Arcadia quadrangle (MC-3) between the large volcano Alba Mons and the Tempe Terra plateau. The valley follows a gently sinuous , north-south path for a distance of about 357 km (222 mi). [2] It is likely an ancient watercourse that formed during the early Hesperian (or late Noachian ) period, [3] around 3.7 billion years ago. [4] |
|
2017 |
56727 characters 6 sections 14 paragraphs 9 images 187 internal links 13 external links |
enipeus 0.629 valley 0.354 tempe 0.225 vallis 0.219 fluvial 0.174 bedforms 0.126 lat 0.118 channels 0.117 stream 0.110 levee 0.108 segment 0.102 267 0.099 vis 0.096 plateau 0.086 alba 0.084 |
Enipeus Vallis is a valley in the northern hemisphere of the planet Mars . It is centered at lat. 37°N, long. 267°E in the Arcadia quadrangle (MC-3) between the large volcano Alba Mons and the Tempe Terra plateau. The valley follows a gently sinuous , north-south path for a distance of about 357 km (222 mi). [2] It is likely an ancient watercourse that formed during the early Hesperian (or late Noachian ) period, [3] around 3.7 billion years ago. [4] |
|
2013 |
51894 characters 5 sections 14 paragraphs 9 images 184 internal links 12 external links |
enipeus 0.629 valley 0.354 tempe 0.225 vallis 0.219 fluvial 0.174 bedforms 0.126 lat 0.118 channels 0.117 stream 0.110 levee 0.108 segment 0.102 267 0.099 vis 0.096 plateau 0.086 alba 0.084 |
Enipeus Vallis is a valley in the northern hemisphere of the planet Mars . It is centered at lat. 37°N, long. 267°E in the Arcadia quadrangle (MC-3) between the large volcano Alba Mons and the Tempe Terra plateau. The valley follows a gently sinuous , north-south path for a distance of about 357 km (222 mi). [2] It is likely an ancient watercourse that formed during the early Hesperian (or late Noachian ) period, [3] around 3.7 billion years ago. [4] |
|
2012 |
30591 characters 5 sections 14 paragraphs 5 images 45 internal links 12 external links |
enipeus 0.629 valley 0.354 tempe 0.225 vallis 0.219 fluvial 0.174 bedforms 0.126 lat 0.118 channels 0.117 stream 0.110 levee 0.108 segment 0.102 267 0.099 vis 0.096 plateau 0.086 alba 0.084 |
Enipeus Vallis is a valley in the northern hemisphere of the planet Mars . It is centered at lat. 37°N, long. 267°E in the Arcadia quadrangle (MC-3) between the large volcano Alba Mons and the Tempe Terra plateau. The valley follows a gently sinuous , north-south path for a distance of about 357 km (222 mi). [2] It is likely an ancient watercourse that formed during the early Hesperian (or late Noachian ) period, [3] around 3.7 billion years ago. [4] |
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2011 |
29594 characters 5 sections 14 paragraphs 5 images 44 internal links 8 external links |
enipeus 0.629 valley 0.354 tempe 0.225 vallis 0.219 fluvial 0.174 bedforms 0.126 lat 0.118 channels 0.117 stream 0.110 levee 0.108 segment 0.102 267 0.099 vis 0.096 plateau 0.086 alba 0.084 |
Enipeus Vallis is a valley in the northern hemisphere of the planet Mars . It is centered at lat. 37°N, long. 267°E in the Arcadia quadrangle (MC-3) between the large volcano Alba Mons and the Tempe Terra plateau. The valley follows a gently sinuous , north-south path for a distance of about 357 km (222 mi). [2] It is likely an ancient watercourse that formed during the early Hesperian (or late Noachian ) period, [3] around 3.7 billion years ago. [4] |
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2010 |
4296 characters 1 sections 2 paragraphs 2 images 5 internal links 1 external links |
enipeus 0.715 377 0.299 357 0.292 vallis 0.234 arcadia 0.234 93 0.165 bar 0.149 centered 0.144 classical 0.135 river 0.130 valley 0.111 17 0.103 long 0.103 scale 0.100 meters 0.093 |
Enipeus Vallis is a valley in the Arcadia quadrangle on Mars. Its location is centered at 377° north latitude and 93.17° west longitude. It is 357 km long and was named after a classical river. [1] |
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2009 |
4334 characters 1 sections 2 paragraphs 2 images 5 internal links 1 external links |
enipeus 0.724 357 0.296 vallis 0.237 arcadia 0.236 degrees 0.225 93 0.167 37 0.159 bar 0.150 centered 0.146 classical 0.137 river 0.131 valley 0.112 long 0.104 scale 0.101 meters 0.094 |
Enipeus Vallis is a valley in the Arcadia quadrangle on Mars. Its location is centered at 37 degrees north latitude and 93.1 degrees west longitude. It is 357 km long and was named after a classical river. [1] |