Geologic mapping and stratigraphic analyses of MTM -30247, -35247, and -40247 quadrangles are being used to characterize the Reull Vallis (RV) system and to determine the history of the eastern Hellas region of Mars. Studies of RV examine the roles and timing of volatile-driven erosional and depositional processes and provide constraints on potential associated climatic changes. This study complements earlier investigations of the eastern Hellas region, including regional analyses [1-6], mapping studies of circum-Hellas canyons [7-10], and volcanic studies of Hadriaca and Tyrrhena Paterae [11-13]. Key scientific objectives for these quadrangles include 1) characterization of RV in its "fluvial zone," 2) analysis of channels in the surroundi...
The Mars Exploration Rover Opportunity observed an upper layer of a more than 600-m-thick sequence o...
The study of the Chryse Planitia region of Mars is based on geologic mapping on a 1:5,000,000 scale ...
Lunae Planum is an elevated region east of the Tharsis rise, and ridged plains containing numerous S...
Geologic mapping of MTM -30247, -35247, and -40247 quadrangles is being used to characterize Reull V...
Mawrth Vallis is a 15-25 km wide, 500 km long sinuous channel that winds through the highlands of Ar...
The Hellas impact basin, spanning 2000+ km in the cratered highlands, is the largest well-preserved ...
The Hellas basin is a dominant feature in the ancient, southern cratered highlands of Mars. The east...
Hellas basin is the largest (2000+ km across) well-preserved impact structure on Mars and its deepes...
Geologic mapping at 1:500,000 scale of the Mars transverse Mercator (MTM) quads 40292 and 40297 is b...
Virtually the entire map area is mantled by an irregular deposit of material that is apparently fine...
As part of a continuing study to understand the relationship between valleys and highland resurfacin...
Geologic mapping studies at the 1:1M-scale are being used to assess geologic materials and processes...
The highland-lowland boundary (HLB) of Mars is interpreted to be a complex tectonic and erosional tr...
Hesperia Planum, characterized by a high concentration of mare-type wrinkle ridges and ridge rings, ...
The Mars Geologic Mapping (MGM) Program was introduced by NASA in 1987 as a new initiative in the Pl...
The Mars Exploration Rover Opportunity observed an upper layer of a more than 600-m-thick sequence o...
The study of the Chryse Planitia region of Mars is based on geologic mapping on a 1:5,000,000 scale ...
Lunae Planum is an elevated region east of the Tharsis rise, and ridged plains containing numerous S...
Geologic mapping of MTM -30247, -35247, and -40247 quadrangles is being used to characterize Reull V...
Mawrth Vallis is a 15-25 km wide, 500 km long sinuous channel that winds through the highlands of Ar...
The Hellas impact basin, spanning 2000+ km in the cratered highlands, is the largest well-preserved ...
The Hellas basin is a dominant feature in the ancient, southern cratered highlands of Mars. The east...
Hellas basin is the largest (2000+ km across) well-preserved impact structure on Mars and its deepes...
Geologic mapping at 1:500,000 scale of the Mars transverse Mercator (MTM) quads 40292 and 40297 is b...
Virtually the entire map area is mantled by an irregular deposit of material that is apparently fine...
As part of a continuing study to understand the relationship between valleys and highland resurfacin...
Geologic mapping studies at the 1:1M-scale are being used to assess geologic materials and processes...
The highland-lowland boundary (HLB) of Mars is interpreted to be a complex tectonic and erosional tr...
Hesperia Planum, characterized by a high concentration of mare-type wrinkle ridges and ridge rings, ...
The Mars Geologic Mapping (MGM) Program was introduced by NASA in 1987 as a new initiative in the Pl...
The Mars Exploration Rover Opportunity observed an upper layer of a more than 600-m-thick sequence o...
The study of the Chryse Planitia region of Mars is based on geologic mapping on a 1:5,000,000 scale ...
Lunae Planum is an elevated region east of the Tharsis rise, and ridged plains containing numerous S...