Mid-Latitude Dissected Mantle Terrain as Viewed from HiRISE
Abstract
Using HiRISE, we examine the morphology of the mid-latitude dissected mantle terrain to test the plausibility of the hypothesis that this global terrain results from desiccation of an ice-rich mantle deposited at times of high obliquity.
- Publication:
-
Seventh International Conference on Mars
- Pub Date:
- July 2007
- Bibcode:
- 2007LPICo1353.3351S