Geomorphology of debris aprons in the eastern Hellas region of Mars

Details Geomorphology of debris aprons in the eastern Hellas region of Mars Geomorphology of debris aprons in the eastern Hellas region of Mars

Mar 1997

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997lpi....28.1377s&link_type=abstract

Conference Paper, 28th Annual Lunar and Planetary Science Conference, p. 377.

Mathematics

Logic

8

Mars Surface, Geomorphology, Space Debris, Planetary Geology, Volcanoes, Satellite Imagery, Planetary Mapping, Viking Orbiter Spacecraft, Surface Properties

Scientific paper

Recent geologic mapping and geomorphic analyses have documented the geologic history of the eastern Hellas region of Mars in terms of the styles, timing, and evolution of volcanic activity associated with eruptive centers at Hadriaca and Tyrrhena Paterae. As a result of the geologic relationships between regional volcanic units and the Dao, Harmakhis, and Reull Valles outflow channel systems, constraints have been established for the timing and nature of erosional and depositional processes occurring in the region. The present study examines late-stage (Amazonian) degradation processes recorded in a series of debris aprons and debris flows located predominantly around massifs in the eroded southern highlands along the Reull and Harmakhis Valles outflow systems.

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