Abalos Undae
Abalos Undae ( Latin for "Abalos Waves") is a dune field on Mars in the periphery of Planum Boreum , the Martian North pole. It is one of the officially named northern circumpolar dune fields, along with Olympia , Hyperboreae , and Siton Undae , and also one of the densest of the region. [1] [2] Its northernmost boundary is located in the southwest channel that separates the Abalos Colles formation from the main polar ice cap, and from there the dune field extends southwest all the way to the lowlands of Vastitas Borealis . [2] [3] [4]
Page Revisions
| Year | Metadata | Sections | Top Words | First Paragraph |
| 2018 |
107217 characters 5 sections 22 paragraphs 18 images 665 internal links 13 external links |
1. Location and formation characteristics |
abalos 0.695 undae 0.528 dunes 0.192 dune 0.138 scarp 0.133 colour 0.118 hyperboreae 0.112 gypsum 0.111 periphery 0.105 olympia 0.098 basal 0.091 siton 0.090 irb 0.087 fields 0.068 tenuis 0.067 |
Abalos Undae ( Latin for "Abalos Waves") is a dune field on Mars in the periphery of Planum Boreum , the Martian North pole. It is one of the officially named northern circumpolar dune fields, along with Olympia , Hyperboreae , and Siton Undae , and also one of the densest of the region. [1] [2] Its northernmost boundary is located in the southwest channel that separates the Abalos Colles formation from the main polar ice cap, and from there the dune field extends southwest all the way to the lowlands of Vastitas Borealis . [2] [3] [4] |
| 2017 |
65095 characters 5 sections 22 paragraphs 21 images 176 internal links 10 external links |
1. Location and formation characteristics |
abalos 0.695 undae 0.528 dunes 0.192 dune 0.138 scarp 0.133 colour 0.118 hyperboreae 0.112 gypsum 0.111 periphery 0.105 olympia 0.098 basal 0.091 siton 0.090 irb 0.087 fields 0.068 tenuis 0.067 |
Abalos Undae ( Latin for "Abalos Waves") is a dune field on Mars in the periphery of Planum Boreum , the Martian North pole. It is one of the officially named northern circumpolar dune fields, along with Olympia , Hyperboreae , and Siton Undae , and also one of the densest of the region. [1] [2] Its northernmost boundary is located in the southwest channel that separates the Abalos Colles formation from the main polar ice cap, and from there the dune field extends southwest all the way to the lowlands of Vastitas Borealis . [2] [3] [4] |