Volcanic Evolution and Erosion at Tyrrhena and Hadriaca Paterae, Mars

Physics

Scientific paper

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Scientific paper

Tyrrhena 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.

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