Abstract
Galileo images of Gaspra reveal it to be an irregularly shaped object
(19 by 12 by 11 kilometers) that appears to have been created by
a catastrophic collisional disruption of a precursor parent body.
The cratering age of the surface is about 200 million years. Subtle
albedo and color variations appear to correlate with morphological
features: Brighter materials are associated with craters especially
along the crests of ridges, have a stronger 1-micrometer absorption,
and may represent freshly excavated mafic materials; darker materials
exhibiting a significantly weaker 1-micrometer absorption appear
concentrated in interridge areas. One explanation of these patterns
is that Gaspra is covered with a thin regolith and that some of this
material has migrated downslope in some areas.
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