A Sagging-Spreading Continuum for the Structure of Large Volcanoes on Terrestrial Planets

Details A Sagging-Spreading Continuum for the Structure of Large Volcanoes on Terrestrial Planets A Sagging-Spreading Continuum for the Structure of Large Volcanoes on Terrestrial Planets

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.2791b&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.2791

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Scientific paper

We use a series of scaled analog models to develop a sagging-spreading
continuum for large volcanoes, into which we place natural examples from
Earth and other planets based on their surface structures.

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