Restio vallis-simius

Several interpretations of recurring slope lineae (RSL) have related RSL to the potential presence of transient liquid water on… Expand

Abstract Phyllosilicate deposits on Mars provide an opportunity to evaluate aqueous activity and the possibility that habitable… Expand

Outflow channels on Mars are interpreted as the product of gigantic floods due to the catastrophic eruption of groundwater that… Expand

[1] Abundant wind-related features occur along Spirit's traverse into the Columbia Hills over the basaltic plains of Gusev Crater… Expand

Introduction: Marwth Vallis and the phyllosilicaterich deposits in and near its lower terminus constitute one of the most… Expand

[1] Fluvial erosion on early Mars was dominated by valley networks created through a combination of groundwater processes and… Expand

[1] Ma'adim Vallis, one of the largest valleys in the Martian highlands, appears to have originated by catastrophic overflow of a… Expand

HESPERIAN BOUNDARY PALEOFLOOD. R. P. Irwin III, A. D. Howard, and T. A. Maxwell, Center for Earth and Planetary Studies, National… Expand

Introduction: Athabasca Vallis (Fig. 1) is the youngest known outflow channel on Mars, dated by crater counting at 2-8 Ma [1,2… Expand