Explosive volcanism may not be an inevitable consequence of magma fragmentation

Abstract

The fragmentation of magma, containing abundant gas bubbles, is thought to be the defining characteristic of explosive eruptions1,2,3. When viscous stresses associated with the growth of bubbles and the flow of the ascending magma exceed the strength of the melt2,4,5,6, the magma breaks into disconnected fragments suspended within an expanding gas phase. Although repeated effusive and explosive eruptions for individual volcanoes are common7,8, the dynamics governing the transition between explosive and effusive eruptions remain unclear. Magmas for both types of eruptions originate from sources with similar volatile content, yet effusive lavas erupt considerably more degassed than their explosive counterparts7,8. One mechanism for degassing during magma ascent, consistent with observations, is the generation of intermittent permeable fracture networks generated by non-explosive fragmentation near the conduit walls9,10,11. Here we show that such fragmentation can occur by viscous shear in both effusive and explosive eruptions. Moreover, we suggest that such fragmentation may be important for magma degassing and the inhibition of explosive behaviour. This implies that, contrary to conventional views, explosive volcanism is not an inevitable consequence of magma fragmentation.

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Figure 1: Deformation textures of annealed fragments in obsidian from Big Glass Mountain, California.
Figure 2: Evolution of a typical model simulation.
Figure 3: Model results and predicted occurrence of shear-induced fragmentation.

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Acknowledgements

We thank P. Papale and D. L. Sahagian for comments on the previous versions of the manuscript, and K. V. Cashman, A. Rust, and A. M. Jellinek for comments on earlier versions. This work was supported by the National Science Foundation and the Sloan Foundation.

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Correspondence to Helge M. Gonnermann.

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Gonnermann, H., Manga, M. Explosive volcanism may not be an inevitable consequence of magma fragmentation. Nature 426, 432–435 (2003). https://doi.org/10.1038/nature02138

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