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Lee, Pascal; Cockell, Charles S.; Marinova, Margarita M.; McKay, Christopher P. and Rice Jr., James W.
(2001).
URL: http://www.lpi.usra.edu/meetings/lpsc2001/pdf/1809...
Abstract
Based on morphologic and contextual analogs from Devon Island, Arctic Canada, the recent martian slope flow features reported by Malin and Edgett are reinterpreted as being due not necessarily to groundwater seepage but possibly to snow or ice melt.