Eddie Brooks March 11, 2014 Earth 438 Rampart Craters: A Case for Water on Mars
Outline What What is a Rampart Crater? Cratering Mechanics and Types Why Rampart Crater Formation Theory Where Rampart Craters on Mars Location Implications How Resolving multiple theories
What is a Rampart Crater? Fluidized ejecta Can have multiple ejecta blankets Very lobate Not found on all planetary bodies Most common of Martian crater morphologies
Rampart Cratering Mechanics Impactor strikes ground Kicks up cloud of ejecta Either: Atmosphere causes ejecta to fall in layers Fluidized ejecta flows out in groups Layered, lobate crater is formed
Formation Theories Make Rampart Craters Intriguing The existence of these craters may suggest the presence of large quantities of subsurface volatiles, including water.
Rampart Crater Types Three types of Rampart Craters: Single Layer Ejecta Double Layer Ejecta Multiple Layer Ejecta
Theories on Formation Subsurface Volatiles: Frozen materials heated upon impact Volatiles melt and mix with surrounding terrain Fluidized ejecta flows like mud Theory supported by absence of rampart craters on dry Moon and Mercury Atmospheric Conditions: Atmosphere allows for generation of vortex ring Staggers deposition of ejecta Confirmed mechanics in laboratory setting Theory supported by absence of craters on atmosphere-less Moon and Mercury
Where do the Craters Form?
Black – Rampart Craters Confirmed | White – Insufficient Data
Single Layer Ejecta
Double Layer Ejecta
Multiple Layer Ejecta
Implications of Locations Rampart craters are not location dependent Widespread across Mars Exception: Tharsis Region – geologically young Crater type is location dependent Subsurface volatile theory suggests correlation between frozen/liquid volatile and crater type Atmospheric hypothesis alone lacks mechanism to explain location dependence
Reconciling Multiple Theories Recent variations on atmospheric hypothesis incorporate volatiles to explain different crater types Volatiles, when thrown into the air, may control descent into lobes Raises the question: To what extent does the atmosphere play a role? Enter: Ganymede and Europa
Ganymede and Europa Planets without atmospheres Water and other volatiles present Rampart craters still form Eliminates necessity of atmosphere for formation, emphasizes volatiles Ganymede
Conclusions and Further Work Rampart craters are most likely the product of subsurface volatiles Water is the most likely candidate, based on where craters are found Further work can be performed to find out the exact influence an atmosphere may have on formation Personal Project: Crater Catalogue