Amenthes Cones, Mars: Hydrovolcanic (Tuff) Cones from Phreatomagmatic Explosive Eruptions?

Details Amenthes Cones, Mars: Hydrovolcanic (Tuff) Cones from Phreatomagmatic Explosive Eruptions? Amenthes Cones, Mars: Hydrovolcanic (Tuff) Cones from Phreatomagmatic Explosive Eruptions?

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.1321b&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.1321

Physics

Scientific paper

Aim of the study is a field of pitted cones located along the dichotomy
boundary in the Amenthes region. We tested the hypothesis of a
hydrovolcanic origin of the cones because the regional context displays
lines of evidence for subsurface water ice.

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