Physics
Scientist
Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian Institution, Washington, D. C., USA
Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian Institution, Independence Avenue at 6th Street SW, Washington, DC 20013-7012, USA
Department of Environmental Sciences, University of Virginia, Charlottesville, Virginia, USA
Planetary Science Institute, Tucson, Arizona, USA
Center for Earth and Planetary Studies, National Air and Space Museum MRC 315, Smithsonian Institution, Washington, DC 20013-7012, USA
Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian Institution, Washington, DC 20560, USA; Department of Environmental Sciences, University of Virginia, Charlottesville, VA 22904, USA
Smithsonian Institution, National Air and Space Museum CEPS, MRC 315 6th St at Independence Ave SW, Washington, DC 20013-7012, USA
Smithsonian Institution, Center for Earth and Planetary Studies, National Air and Space Museum, Washington, DC 20560, USA
Planetary Science Institute, 1700 E. Ft. Lowell Rd., Suite 106, Tucson, AZ 85719, USA
Planetary Science Institute, Tucson, AZ, USA; Sciences Institute, Tucson, AZ, USA; Institution, Center for Earth and Planetary Studies National Air and Space Museum, Washington, DC 20560, USA
Smithsonian Institution, Center for Earth and Planetary Studies, National Air and Space Museum, MRC 315, 6th St. at Independence Ave SW, Washington, DC 20013-7012, USA
Smithsonian Institution, MRC 315, 6th St. at Independence Ave. SW, Washington, DC 20013-7012, USA
Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian Institution, 6th at Independence SW, Washington, DC 20560, USA
Planetary Science Institute, Tucson, AZ, USA / NASM,
A Lake in Uzboi Vallis and Implications for Late Noachian Climate on Mars
A lake in Uzboi Vallis and implications for Late Noachian-Early Hesperian climate on Mars
A Large Paleolake Basin at the Head of Ma'adim Vallis, Mars
An intense terminal epoch of widespread fluvial activity on early Mars: 1. Valley network incision and associated deposits
An intense terminal epoch of widespread fluvial activity on early Mars: 2. Increased runoff and paleolake development
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