Cryovolcanic History of Ceres from Topography
Abstract
We use image analysis and flow modeling of domes on Ceres to argue that they are cryovolcanic in origin. Results imply an average cryovolcanic rate of 10000 m^3/yr, orders of magnitude lower than rates of basaltic volcanism on terrestrial planets.
- Publication:
-
Cryovolcanism in the Solar System Workshop,
- Pub Date:
- June 2018
- Bibcode:
- 2018LPICo2045.2007S