Lee, Pascal; Cockell, Charles S.; Marinova, Margarita M.; McKay, Christopher P. and Rice Jr., James W.
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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.
|Item Type:||Conference Item|
|Extra Information:||Abstract #1809|
|Academic Unit/Department:||Faculty of Science, Technology, Engineering and Mathematics (STEM) > Physical Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM)
|Interdisciplinary Research Centre:||Centre for Earth, Planetary, Space and Astronomical Research (CEPSAR)|
|Depositing User:||Kyra Proctor|
|Date Deposited:||27 Jun 2007|
|Last Modified:||04 Aug 2016 09:03|
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