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Volcanic Evolution and Erosion at Tyrrhena and Hadriaca Paterae, MarsTyrrhena and Hadriaca Paterae are low-relief central-vent volcanoes with shallowly sloping flanks dissected by radial channels. We present results of our investigations of channel formation, the Tyrrhena Patera lava flow field, and the relation between Hesperia Planum and Tyrrhena Patera. Additional information is contained in the original extended abstract.
Document ID
20020046092
Acquisition Source
Goddard Space Flight Center
Document Type
Conference Paper
Authors
Gregg, T. K. P. (Buffalo Univ. NY United States)
Crown, D. A. (Planetary Science Inst. Tucson, AZ United States)
Sakimoto, S. E. H. (NASA Goddard Space Flight Center Greenbelt, MD United States)
Date Acquired
August 20, 2013
Publication Date
April 1, 2002
Publication Information
Publication: Lunar and Planetary Science XXXIII
Subject Category
Lunar And Planetary Science And Exploration
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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