Terraced Margins on the Inflated McCartys Basalt Lava Flow, New Mexico: Constraints on Emplacement Mechanisms

Details Terraced Margins on the Inflated McCartys Basalt Lava Flow, New Mexico: Constraints on Emplacement Mechanisms Terraced Margins on the Inflated McCartys Basalt Lava Flow, New Mexico: Constraints on Emplacement Mechanisms

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.1831z&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.1831

Physics

Scientific paper

Terraces along the margin of the McCartys lava flow have distinct
topographic characteristics that indicate the features are one
manifestation of the lava flow inflation process.

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