As part of a continuing study to understand the relationship between valleys and highland resurfacing through geologic mapping, the authors are continuing to map seven 1:500,000-scale MTM quads in portions of the Margaritifer, Arabia, and Noachis Terrae. Results from this mapping will also help constrain the role and extent of past water in the region. The MTMs are grouped in two different areas within the region and compliment previous mapping in adjacent areas. Three western quads focus on Jones crater and the Himera, Samara, and Loire Valles systems. This abstract focuses on the four eastern quads wherein a large, ancient impact structure, Noachis basin, is flanked on its south and east by a series of valley networks. A solitary valley d...
Geologic mapping studies at the 1:1M-scale are being used to assess geologic materials and processes...
Terrain studies of candidate landing sites for a future rover/sample-return mission to Mars are bein...
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...
Geologic mapping at 1:500,000 scale of the Mars transverse Mercator (MTM) quads 40292 and 40297 is b...
Geologic and geomorphic analyses reveal the effects of fluvial processes within Tyrrhena Terra, Prom...
Mawrth Vallis is a 15-25 km wide, 500 km long sinuous channel that winds through the highlands of Ar...
The Mars Exploration Rover Opportunity observed an upper layer of a more than 600-m-thick sequence o...
Geomorphic mapping at 1:500,000 scale within three quadrangles in Margaritifer Terra, Mars, is neari...
The Mars Geologic Mapping (MGM) Program was introduced by NASA in 1987 as a new initiative in the Pl...
[1] Martian valley networks have been identified mainly in the Noachian heavily cratered uplands. Th...
International audienceMartian valley networks have been identified mainly in the Noachian heavily cr...
We are approaching the end of the third year of mapping the Athabasca Valles region of Mars. The lin...
Hellas basin is the largest (2000+ km across) well-preserved impact structure on Mars and its deepes...
Geologic mapping studies at the 1:1M-scale are being used to assess geologic materials and processes...
Terrain studies of candidate landing sites for a future rover/sample-return mission to Mars are bein...
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...
Geologic mapping at 1:500,000 scale of the Mars transverse Mercator (MTM) quads 40292 and 40297 is b...
Geologic and geomorphic analyses reveal the effects of fluvial processes within Tyrrhena Terra, Prom...
Mawrth Vallis is a 15-25 km wide, 500 km long sinuous channel that winds through the highlands of Ar...
The Mars Exploration Rover Opportunity observed an upper layer of a more than 600-m-thick sequence o...
Geomorphic mapping at 1:500,000 scale within three quadrangles in Margaritifer Terra, Mars, is neari...
The Mars Geologic Mapping (MGM) Program was introduced by NASA in 1987 as a new initiative in the Pl...
[1] Martian valley networks have been identified mainly in the Noachian heavily cratered uplands. Th...
International audienceMartian valley networks have been identified mainly in the Noachian heavily cr...
We are approaching the end of the third year of mapping the Athabasca Valles region of Mars. The lin...
Hellas basin is the largest (2000+ km across) well-preserved impact structure on Mars and its deepes...
Geologic mapping studies at the 1:1M-scale are being used to assess geologic materials and processes...
Terrain studies of candidate landing sites for a future rover/sample-return mission to Mars are bein...
Virtually the entire map area is mantled by an irregular deposit of material that is apparently fine...