Dark halo craters and the thickness of grooved terrain on Ganymede

Mathematics – Logic

Scientific paper

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Craters, Ganymede, Planetary Geology, Satellite Surfaces, Halos, Histograms, Satellite Imagery, Voyager 2 Spacecraft, Jupiter, Satellites, Ganymede, Craters, Halos, Surface, Features, Grooves, Terrain, Thickness, Radius, Ejecta, Albedo, Formation, Uruk Sulcus, Size, Diameter, Stratigraphy, Depth, Models

Scientific paper

On the basis of a morphological analysis of recent Voyager images of the dark halo craters and grooved terrain in the Uruk Sulcus region on Ganymede, it is proposed that dark halos result from the incorporation of cratered terrain material into crater ejecta. In Uruk Sulcus, only craters greater than about 12 km in diameter have halos, indicating that the cratered material there forms a stratigraphic horizon buried in the grooved terrain. A depth of excavation of cratered terrains of 1.0 to 1.6 km is calculated. It is shown that the estimated depth is consistent with current theoretical models of grooved terrain, where relatively clean ice is emplaced over downdropped blocks of cratered terrain. Several Voyager 2 images of the Uruk Sulcus region on Ganymede are provided.

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