The Mars Exploration Rover Opportunity observed an upper layer of a more than 600-m-thick sequence of light toned outcrops that characterize the Meridiani region of Mars. Results from the rover analyses have shown that the bedrock contains mineral and textural characteristics that require the interaction of, and possibly an overall formation by, water-related mechanisms in order to be explained. Additionally, remote sensing studies of the region have suggested that the rocks sampled in places by the MER rover consist of many distinct layers extending over an area of more than 3 X 10(exp 5) square km spanning 20 of longitude
Les processus internes et externes qui ont formé et structuré la croûte de la planète Mars au début ...
International audienceAn extensive layered formation covers the high plateaus around Valles Marineri...
The area of Meridiani Planum on Mars became of particular interest after the detection of coarse-gra...
The Mars Exploration Rover Opportunity observed an upper layer of a more than 600-m-thick sequence o...
The Mars Exploration Rover Opportunity touched down at Meridiani Planum in January 2004 and since th...
Geologic mapping studies at the 1:1M-scale are being used to assess geologic materials and processes...
As part of a continuing study to understand the relationship between valleys and highland resurfacin...
We have used Mars Exploration Rover Opportunity data to investigate the origin and alteration of lit...
Chemical, mineralogic, and lithologic ground truth was acquired for the first time on Mars in terrai...
Mawrth Vallis is a 15-25 km wide, 500 km long sinuous channel that winds through the highlands of Ar...
Virtually the entire map area is mantled by an irregular deposit of material that is apparently fine...
Chemical, mineralogic, and lithologic ground truth was acquired for the first time on Mars in terrai...
Geologic and geomorphic analyses reveal the effects of fluvial processes within Tyrrhena Terra, Prom...
The Microscopic Imager (MI) on the Mars Exploration Rover Opportunity has returned images of Mars wi...
The Mars Exploration Rover Opportunity has spent more than 2 years exploring Meridiani Planum, trave...
Les processus internes et externes qui ont formé et structuré la croûte de la planète Mars au début ...
International audienceAn extensive layered formation covers the high plateaus around Valles Marineri...
The area of Meridiani Planum on Mars became of particular interest after the detection of coarse-gra...
The Mars Exploration Rover Opportunity observed an upper layer of a more than 600-m-thick sequence o...
The Mars Exploration Rover Opportunity touched down at Meridiani Planum in January 2004 and since th...
Geologic mapping studies at the 1:1M-scale are being used to assess geologic materials and processes...
As part of a continuing study to understand the relationship between valleys and highland resurfacin...
We have used Mars Exploration Rover Opportunity data to investigate the origin and alteration of lit...
Chemical, mineralogic, and lithologic ground truth was acquired for the first time on Mars in terrai...
Mawrth Vallis is a 15-25 km wide, 500 km long sinuous channel that winds through the highlands of Ar...
Virtually the entire map area is mantled by an irregular deposit of material that is apparently fine...
Chemical, mineralogic, and lithologic ground truth was acquired for the first time on Mars in terrai...
Geologic and geomorphic analyses reveal the effects of fluvial processes within Tyrrhena Terra, Prom...
The Microscopic Imager (MI) on the Mars Exploration Rover Opportunity has returned images of Mars wi...
The Mars Exploration Rover Opportunity has spent more than 2 years exploring Meridiani Planum, trave...
Les processus internes et externes qui ont formé et structuré la croûte de la planète Mars au début ...
International audienceAn extensive layered formation covers the high plateaus around Valles Marineri...
The area of Meridiani Planum on Mars became of particular interest after the detection of coarse-gra...