Climate Change on Mars from Erosion Rates at the Mars Exploration Rover Landing Sites
Abstract
The gradation history of the Gusev and Meridiani plains argues for a dry and desiccating environment since the Late Hesperian, in contrast to the sedimentary evaporites in Meridiani Planum that document a warmer and wetter environment in the Noachian.
- Publication:
-
Seventh International Conference on Mars
- Pub Date:
- July 2007
- Bibcode:
- 2007LPICo1353.3034G