Project Information
Orbital Spectral Mapping of Surface Compositions in the Antarctic Dry Valleys: Regional Distributions of Secondary Mineral-Phases as Climate Indicators

This project uses Aster and Hyperion remote sensing data combined with field observations and laboratory analysis to map soils in the McMurdo Dry Valleys of Antarctica. The goal is to use mineral abundances, compositions, and spatial heterogeneities to investigate the connections between microclimate and surface characteristics. The valleys are one of the most unique landscapes on earth. The outcomes will be relevant to understanding their geologic, biologic, and climactic history, and offer insight into the Martian landscape. The main broader impacts are graduate education and curriculum development involving K12 teachers.
Person Role
Wyatt, Michael Investigator
Antarctic Earth Sciences Award # 0739702
AMD - DIF Record(s)
Data Management Plan
None in the Database
Product Level:
Not provided
  1. Salvatore, M. R., Mustard, J. F., Head, J. W., Rogers, A. D., & Cooper, R. F. (2014). The dominance of cold and dry alteration processes on recent Mars, as revealed through pan-spectral orbital analyses. Earth and Planetary Science Letters, 404, 261–272. (doi:10.1016/j.epsl.2014.08.006)
  2. Gough, R. V., Wong, J., Dickson, J. L., Levy, J. S., Head, J. W., Marchant, D. R., & Tolbert, M. A. (2017). Brine formation via deliquescence by salts found near Don Juan Pond, Antarctica: Laboratory experiments and field observational results. Earth and Planetary Science Letters, 476, 189–198. (doi:10.1016/j.epsl.2017.08.003)
Platforms and Instruments

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