Simulation of Lava Flow Inundation on Martian Cratered Terrain

Details Simulation of Lava Flow Inundation on Martian Cratered Terrain Simulation of Lava Flow Inundation on Martian Cratered Terrain

Mar 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999lpi....30.1112h&link_type=abstract

30th Annual Lunar and Planetary Science Conference, March 15-29, 1999, Houston, TX, abstract no. 1112

Physics

Scientific paper

Lava inundation of a cratered surface is simulated by spreading from a
few sources. Unlike equipotential flooding, lava covers intercrater
plains but high-rimmed craters escape flooding or are partially filled,
as on ridged plains and subdued cratered units.

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