Abstract
The martian south polar plateau, Planum Australe, comprises the largest known water-ice surface deposit on the planet. Here, we present evidence for an episode of extensive polar plateau retreat during the Late Amazonian, which affected regions flanking circum-polar terrains located between Cavi Angusti and Sisyphi Montes.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 407-411 |
| Number of pages | 5 |
| Journal | Icarus |
| Volume | 248 |
| DOIs | |
| State | Published - Mar 1 2015 |
Keywords
- Ices
- Mars
- Polar caps
- Polar geology
ASJC Scopus subject areas
- Astronomy and Astrophysics
- Space and Planetary Science