Abstract:Since the high temperatures on the surface of Venus prohibit fluvial processes, the dominant mechanism of sediment production is impact cratering. Sediment produced during impact events is deposited in extensive ejecta blankets and eventually redistributed across Venus' surface by surface winds. Despite the apparent importance of aeolian processes for sediment transport, however, aeolian deposits such as dunes are rare. There is a disconnect between our knowledge of sediment production and the fate of venusian… Show more
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