Paper No. 241-3
Presentation Time: 10:35 AM
THE VOLCANIC EXPLOSIVE-EFFUSIVE TRANSITION EXPLAINED BY COMPETING OUTGASSING MECHANISMS
Lava dome-forming volcanoes commonly switch between effusive and explosive styles of eruption. Eruptions are driven by gas overpressure, which can be released through development of permeability, yet the least permeable magmas often erupt effusively. We studied gas exsolution and outgassing through experimental vesiculation of hydrous dacite glass samples containing crystal fractions between 0 and 0.8. Outgassing occurs rapidly via fracturing at crystal fractions ≥ 0.7, implying that crystal-rich effusive lavas are likely healed remains of fractured, initially more hydrous magmas. Fracturing and bubble coalescence are both inefficient at crystal fractions of 0.5–0.6, implying eruptive behavior of lava domes can fluctuate in response to minor changes in crystallinity or ascent rate. We delineate a critical permeability-porosity threshold separating effusive magmas from those with explosive potential.