Lee, Pascal; Cockell, Charles S.; Marinova, Margarita M.; McKay, Christopher P. and Rice Jr., James W.
PDF (Not Set)
- Requires a PDF viewer such as GSview, Xpdf or Adobe Acrobat Reader
|Google Scholar:||Look up in Google Scholar|
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:||Science > Physical Sciences
|Interdisciplinary Research Centre:||Centre for Earth, Planetary, Space and Astronomical Research (CEPSAR)|
|Depositing User:||Kyra Proctor|
|Date Deposited:||27 Jun 2007|
|Last Modified:||15 Jan 2016 13:57|
|Share this page:|