T290 Impact Cratering on Earth and throughout the Solar System
Wednesday, 28 September 2016
8:00 AM - 12:00 PM
Room 201
THE RELATIONSHIP BETWEEN SURFACE ROUGHNESS AND SURFACE AGE ON MERCURY
Paper number: T290-7
Program: Technical Sessions
Time: 9:30 AM – 9:45 AM
Authors
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Olivier S. BarnouinJohns Hopkins University Applied Physics Laboratory, Laurel, MD
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Carolyn M. ErnstJohns Hopkins University Applied Physics Laboratory, Laurel, MD
Abstract
In this study, we investigate the relationship between surface age and surface roughness through simulation. We make use of observed surface roughness around one crater at a given scale, and then co-add those results other observed roughness measurements of roughness seen at craters of other scales. In this way, we can simulate how the measured roughness on Mercury evolves as crater density increases with the increasing passage of time. We limit our simulations to the observed surface roughness measured around craters with diameters ranging from 10 to 100 km.
Preliminary results show that for surface roughness at the 1 km scale, the total number of craters in a region does not control the surface roughness, but instead the surface roughness is dominated by the formation and presence of a few large impact craters. This is supported by our observations that a few large impact craters dominate the surface roughness at the 1 km baseline in the volcanic plains of Mercury. For Mercury, the relationship between surface roughness and surface is not directly related and instead the more complex topography around large craters obscures any affect crater density has on surface age
Geological Society of America Abstracts with Programs. Vol. 48, No. 7
doi: 10.1130/abs/2016AM-283064
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