Morphology and Emplacement Processes at the Distal End of the Carrizozo Lava Flow, New Mexico: Implications for Martian Sheet Flows

Details Morphology and Emplacement Processes at the Distal End of the Carrizozo Lava Flow, New Mexico: Implications for Martian Sheet Flows Morphology and Emplacement Processes at the Distal End of the Carrizozo Lava Flow, New Mexico: Implications for Martian Sheet Flows

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpi....39.1734g&link_type=abstract

39th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXIX), held March 10-14, 2008 in League City, Texas.

Physics

1

Scientific paper

The morphology at the distal end of the Carrizozo lava flow in New
Mexico provides insight for the emplacement of sheet flows on Mars.
Observations suggest that significant inflation has occurred to form
flat platform surfaces and terraced margins.

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