Physics
Scientific paper
Aug 1985
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1985em%26p...33..103t&link_type=abstract
Earth, Moon and Planets, Volume 33, Issue 1, pp.103-104
Physics
Mars, Channels, Ice, Distribution, Climate, Models, Thermal Effects, Cooling, Valleys, Formation, Chronology, Impacts, Bombardment, Hypotheses, Flow, Analogs
Scientific paper
If it is assumed that the Martian outflow channels are result of sporadic melting of ground ice, their planet-wide distribution could imply that a sheet of ice once covered Mars. This ice sheet could have acted, in a similar manner as Hoyle's oceanic meteoric dust suspension layer model as an initiator of a Martian ice age which would be responsible for the decline of valley network formation at the end of the heavy bombardment period.
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