Morphologic variation of an evolving dome controlled by the extrusion of finite yield strength magma

Degassing-induced crystallization in volatile rich intermediate composition magmas results in material stiffening and strengthening that prior to solidification is reflected in non-Newtonian rheology. We explore the effects of a spectrum of such rheological regimes on eruptive style and morphologic...

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Bibliographic Details
Published in:Journal of volcanology and geothermal research Vol. 370; pp. 51 - 64
Main Authors: Husain, Taha, Elsworth, Derek, Voight, Barry, Mattioli, Glen, Jansma, Pamela
Format: Journal Article
Language:English
Published: Elsevier B.V 15-01-2019
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Summary:Degassing-induced crystallization in volatile rich intermediate composition magmas results in material stiffening and strengthening that prior to solidification is reflected in non-Newtonian rheology. We explore the effects of a spectrum of such rheological regimes on eruptive style and morphologic evolution of lava domes, using a two-dimensional (2D) particle-dynamics model for a spreading viscoplastic (Bingham) fluid. We assume that the ductile magma core of a 2D synthetic lava dome develops finite yield strength, and that deformable frictional talus evolves from a carapace that caps the magma core. Our new model is calibrated against an existing analytical model for a spreading viscoplastic lava dome and is further compared against observational data of lava dome growth. Results indicate that a degassing-induced increase in strength of the injected magma causes a transition in the lava dome morphology from a dome with low surface relief evolving endogenously (with apparent bulk yield strength - 104 < τ0a < 106 Pa), to a Pelean lava dome with spines (τ0a > 105 – 106 Pa) extruded through the dome carapace. The virtual lava dome with τ0a = 0.6 MPa shows good agreement with the observed dome heights observed at the Soufriere Hills Volcano, Montserrat during a period of endogenous growth. The calculated apparent flow viscosity (1.36 × 1011 Pa·s for τ0a = 0.6 MPa) is in the range of estimated viscosities (109 to 1012 Pa·s) for andesitic-dacitic crystal-rich lavas. Our model results indicate a strong correlation between apparent yield strength and dome morphology, with both controlled by degassing-induced crystallization and extrusion rate.
ISSN:0377-0273
1872-6097
DOI:10.1016/j.jvolgeores.2019.01.010