The morphology and setting of a groove in Gusev strongly supports the hypothesis of a lateral channel generated by meltwater flowing against an ice covered lake margin. The size of the groove and the slope of the bed independent of the topography of the crater are consistent with modest discharges. Additional information is contained in the original extended abstract.
New Evidence Supporting an Ice-covered Lake in Gusev Crater
2002-04-01
Conference paper
No indication
English
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