Volcanic or Fluvial: Comparison of an Ascraeus Mons, Mars, Braided and Sinuous Channel with Features of the 1859 Mauna Loa Flow and Mare Imbrium Flows

Details Volcanic or Fluvial: Comparison of an Ascraeus Mons, Mars, Braided and Sinuous Channel with Features of the 1859 Mauna Loa Flow and Mare Imbrium Flows Volcanic or Fluvial: Comparison of an Ascraeus Mons, Mars, Braided and Sinuous Channel with Features of the 1859 Mauna Loa Flow and Mare Imbrium Flows

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1612b&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1612

Physics

2

Scientific paper

A channel on Ascraeus Mons, previously suggested to indicate fluvial
activity, is shown in its entirety. Distal portions indicate that this
feature is of a volcanic origin despite similarities in the proximal
sections to fluvial features.

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