Volcanic Pseudocraters on Mars: Icelandic Analogs

Details Volcanic Pseudocraters on Mars: Icelandic Analogs Volcanic Pseudocraters on Mars: Icelandic Analogs

Mar 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001lpi....32.1871g&link_type=abstract

32nd Annual Lunar and Planetary Science Conference, March 12-16, 2001, Houston, Texas, abstract no.1871

Computer Science

Scientific paper

Pseudocraters are small conical structures which develop on some
basaltic lava flows in Iceland as a result of the interaction of the
active flow with water or marshy ground. These features have been
studied in the field and compared with structures observed on Mars.

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