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Restio vallis-simius

Known as: Restio vallis simius 
 
National Institutes of Health

Papers overview

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2019
2019
Several interpretations of recurring slope lineae (RSL) have related RSL to the potential presence of transient liquid water on… Expand
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2013
2013
Abstract Phyllosilicate deposits on Mars provide an opportunity to evaluate aqueous activity and the possibility that habitable… Expand
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2013
2013
Outflow channels on Mars are interpreted as the product of gigantic floods due to the catastrophic eruption of groundwater that… Expand
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2008
2008
[1] Abundant wind-related features occur along Spirit's traverse into the Columbia Hills over the basaltic plains of Gusev Crater… Expand
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2007
2007
Introduction: Marwth Vallis and the phyllosilicaterich deposits in and near its lower terminus constitute one of the most… Expand
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2005
2005
[1] Fluvial erosion on early Mars was dominated by valley networks created through a combination of groundwater processes and… Expand
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2004
2004
[1] Ma'adim Vallis, one of the largest valleys in the Martian highlands, appears to have originated by catastrophic overflow of a… Expand
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2004
2004
HESPERIAN BOUNDARY PALEOFLOOD. R. P. Irwin III, A. D. Howard, and T. A. Maxwell, Center for Earth and Planetary Studies, National… Expand
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2003
2003
Introduction: Athabasca Vallis (Fig. 1) is the youngest known outflow channel on Mars, dated by crater counting at 2-8 Ma [1,2… Expand
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