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Atypical planetary lavas: rheological evolution of cooling and crystallizing flows from lunar impact melts and cryovolcanic processes
(University of Missouri--Columbia, 2021)
explain why more highland impact melt sheets are observed, because the thinner impact melts in the mare are more readily erased by impact gardening resulting in a preservation bias in the rock record. I also synthesized a wide range of aqueous solutions...
Rheological and morphological evolution of basaltic lava flows
(University of Missouri--Columbia, 2018)
Over 500 million people live in proximity of an active volcano globally. Although lava flows rarely endanger human life, they often destroy critical infrastructure. Advancing our understanding of lava flow dynamics is ...