Rootless Cone? Pingo? or Mud Volcano? in Central Elysium Planitia, Mars

Details Rootless Cone? Pingo? or Mud Volcano? in Central Elysium Planitia, Mars Rootless Cone? Pingo? or Mud Volcano? in Central Elysium Planitia, Mars

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.1683n&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.1683

Physics

Scientific paper

It is possible that Mars has experienced recent (~100 Ma) magmatism. In
central Elysium Planitia, the identification of cone-like landforms are
discussed: rootless cones, pingos, or mud volcanos. From their
morphology, the landforms are thought to be rootless cones.

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