Uzboi-Landon-Morava
The Uzboi-Landon-Morava (ULM) outflow system is a long series of channels and depressions that may have carried water across a major part of Mars. It starts with channels that drain into the Argyre basin in the Argyre quadrangle . Water ponded in the Argyre basin, then the overflow is believed to have traveled northward through Uzboi Vallis , into Landon basin , through Morava Valles , to the floor of Margaritfier basin . [1] [2] [3] Some of the water may have helped to carve Ares Vallis . [4] [5] [6] [7] [8] Altogether, the total area drained for this watershed may have been about 11 X 10 6 km 2 or about 9% of Mars. [9] [10]
Page Revisions
| Year | Metadata | Sections | Top Words | First Paragraph |
| 2018 |
71607 characters 3 sections 5 paragraphs 3 images 644 internal links 0 external links |
argyre 0.540 basin 0.332 uzboi 0.329 morava 0.261 landon 0.245 vallis 0.187 margaritfier 0.169 traveled 0.140 mola 0.135 ulm 0.130 watershed 0.122 ladon 0.119 overflow 0.110 showing 0.109 ponded 0.108 |
The Uzboi-Landon-Morava (ULM) outflow system is a long series of channels and depressions that may have carried water across a major part of Mars. It starts with channels that drain into the Argyre basin in the Argyre quadrangle . Water ponded in the Argyre basin, then the overflow is believed to have traveled northward through Uzboi Vallis , into Landon basin , through Morava Valles , to the floor of Margaritfier basin . [1] [2] [3] Some of the water may have helped to carve Ares Vallis . [4] [5] [6] [7] [8] Altogether, the total area drained for this watershed may have been about 11 X 10 6 km 2 or about 9% of Mars. [9] [10] |
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| 2017 |
9395 characters 3 sections 6 paragraphs 3 images 11 internal links 0 external links |
argyre 0.537 basin 0.330 uzboi 0.327 morava 0.259 landon 0.243 vallis 0.185 margaritfier 0.168 traveled 0.139 mola 0.135 ulm 0.130 watershed 0.122 ladon 0.118 gallery 0.116 overflow 0.109 showing 0.108 |
The Uzboi-Landon-Morava (ULM) outflow system is a long series of channels and depressions that may have carried water across a major part of Mars. It starts with channels that drain into the Argyre basin in the Argyre quadrangle . Water ponded in the Argyre basin, then the overflow is believed to have traveled northward through Uzboi Vallis , into Landon basin , through Morava Valles , to the floor of Margaritfier basin . [1] [2] [3] Some of the water may have helped to carve Ares Vallis . [4] [5] [6] [7] [8] Altogether, the total area drained for this watershed may have been about 11 X 10 6 km 2 or about 9% of Mars. [9] [10] |
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| 2015 |
8657 characters 3 sections 4 paragraphs 2 images 11 internal links 0 external links |
argyre 0.574 basin 0.353 morava 0.277 landon 0.260 uzboi 0.233 margaritfier 0.179 traveled 0.149 mola 0.144 ulm 0.139 watershed 0.130 overflow 0.117 ponded 0.115 drain 0.115 drained 0.109 northward 0.108 |
The Uzboi-Landon-Morava (ULM) outflow system is a long series of channels and depressions that may have carried water across a major part of Mars. It starts with channels that drain into the Argyre basin in the Argyre quadrangle . Water ponded in the Argyre basin, then the overflow is believed to have traveled northward through Uzboi Vallis , into Landon basin , through Morava Valles , to the floor of Margaritfier basin . [1] [2] [3] Some of the water may have helped to carve Ares Vallis . [4] [5] [6] [7] [8] Altogether, the total area drained for this watershed may have been about 11 X 10 6 km 2 or about 9% of Mars. [9] [10] |