Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Background: Promethei Lingula, a part of Mars ’ south polar plateau, Planum Australe, is made up of south polar layered deposits (SPLD) and includes three broad, deep canyons trending perpendicular to the plateau margin and several spiral troughs concentric to the plateau. Two of the canyons, Promethei and Ultimum Chasmata, expose substrate beneath SPLD, and the other canyon displays a variety of erosional landforms within SPLD, including curvilinear, longitudinal grooves (Australe Sulci). Method: Recent Mars Global Surveyor and Mars Odyssey data sets permit us to map, characterize, and eva...
International audienceAn extensive layered formation covers the high plateaus around Valles Marineri...
Planum Boreum (PB) is a dome of layered icy material rising ~3 km above the surrounding plains in th...
The Medusae Fossae Formation (MFF) is an extensive deposit (2.2×106km2, Bradley, B.A., Sakimoto, S.E...
Mars’ polar regions are covered with ice-rich layered deposits that potentially contain a record of ...
The Mars South Polar Layered Deposits (SPLD) are the result of depositional and erosional events, wh...
We have examined the local base of the south polar layered deposits (SPLD) exposed in the bounding s...
Mars’ polar regions are covered with ice-rich layered deposits that potentially contain a record of ...
Data from the Mars Orbiter Laser Altimeter (MOLA) and Mars Orbiter Camera (MOC) aboard the Mars Glob...
International audienceThe Mars South Polar Layered Deposits (SPLD) are the result of depositional an...
Background: Planum Boreum, the north polar plateau of Mars, displays four extensive low-albedo regio...
We have examined the local base of the south polar layered de-posits (SPLD) exposed in the bounding ...
Sharply delineated closed depressions, one-half to tens of kilometers across, with 400 meters estima...
One of the many questions of Martian exploration is to uncover the history of Mars, through analysis...
International audienceAn extensive layered formation covers the high plateaus around Valles Marineri...
Planum Boreum (PB) is a dome of layered icy material rising ~3 km above the surrounding plains in th...
The Medusae Fossae Formation (MFF) is an extensive deposit (2.2×106km2, Bradley, B.A., Sakimoto, S.E...
Mars’ polar regions are covered with ice-rich layered deposits that potentially contain a record of ...
The Mars South Polar Layered Deposits (SPLD) are the result of depositional and erosional events, wh...
We have examined the local base of the south polar layered deposits (SPLD) exposed in the bounding s...
Mars’ polar regions are covered with ice-rich layered deposits that potentially contain a record of ...
Data from the Mars Orbiter Laser Altimeter (MOLA) and Mars Orbiter Camera (MOC) aboard the Mars Glob...
International audienceThe Mars South Polar Layered Deposits (SPLD) are the result of depositional an...
Background: Planum Boreum, the north polar plateau of Mars, displays four extensive low-albedo regio...
We have examined the local base of the south polar layered de-posits (SPLD) exposed in the bounding ...
Sharply delineated closed depressions, one-half to tens of kilometers across, with 400 meters estima...
One of the many questions of Martian exploration is to uncover the history of Mars, through analysis...
International audienceAn extensive layered formation covers the high plateaus around Valles Marineri...
Planum Boreum (PB) is a dome of layered icy material rising ~3 km above the surrounding plains in th...
The Medusae Fossae Formation (MFF) is an extensive deposit (2.2×106km2, Bradley, B.A., Sakimoto, S.E...