high-resolution structural mapping in southwest candor chasma · high-resolution topography •...
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High-resolution structural mapping in
Southwest Candor Chasma
Chris Okubo, Alfred McEwen, HiRISE TeamLunar and Planetary Laboratory, University of Arizona
Kevin LewisDivision of Geological and Planetary SciencesCalifornia Institute of Technology
Randy KirkU.S. Geological Survey, Astrogeology Team
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Southwest Candor Chasma, Valles Marineris
Candor ChasmaCandor Chasma
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Layers contain abundant evidence of past
groundwater
Study areaStudy area
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Ground level view
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Low altitude view
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History recorded in the rocks
• Candor Chasma was a sedimentary basin
– Paradox basin, SE Utah analog
• Preserves geologic history since 3.7 Gya
– Chemistry may record global climate change
– Transition to acidic groundwater
– Iron cycling in acidic environment
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High-resolution topography
• Uses two HiRISE images of the same target– Same target
– Different look directions
– Parallax yields topography
• Each image– 27 cm per pixel sampling of surface brightness
– Detect features ~27 cm across
– Resolve 2D shape of features ~1 m across
• Both images combined– 1 m per pixel sampling of topography
– Detect changes in elevation ~1 m across
– Resolve 3D shape of features 3-5 m across
• Unprecedented resolution of geomorphology from orbit