Item talk:Q59773

From geokb

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     "name": "The dynamics of Hawaiian-style eruptions: A century of study",
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     "abstract": "This chapter, prepared in celebration of the Hawaiian Volcano Observatory\u02bcs centennial, provides a historical lens through which to view modern paradigms of Hawaiian-style eruption dynamics. The models presented here draw heavily from observations, monitoring, and experiments conducted on K\u012blauea Volcano, which, as the site of frequent and accessible eruptions, has attracted scientists from around the globe. Long-lived eruptions in particular\u2014Halema\u2018uma\u2018u 1907\u201324, K\u012blauea Iki 1959, Mauna Ulu 1969\u201374, Pu\u2018u \u2018\u014c\u2018\u014d-Kupaianaha 1983\u2013present, and Halema\u2018uma\u2018u 2008\u2013present\u2014have offered incomparable opportunities to conceptualize and constrain theoretical models with multidisciplinary data and to field-test model results. The central theme in our retrospective is the interplay of magmatic gas and near-liquidus basaltic melt. A century of study has shown that gas exsolution facilitates basaltic dike propagation; volatile solubility and vesiculation kinetics influence magma-rise rates and fragmentation depths; bubble interactions and gas-melt decoupling modulate magma rheology, eruption intensity, and plume dynamics; and pyroclast outgassing controls characteristics of eruption deposits. Looking to the future, we anticipate research leading to a better understanding of how eruptive activity is influenced by volatiles, including the physics of mixed CO2-H2O degassing, gas segregation in nonuniform conduits, and vaporization of external H2O during magma ascent.",
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