Mount St. Helens: the influence of water on volcanic eruptions

Under what conditions will a volcano erupt? Can we predict the eruption behavior of a volcano by studying rocks from its previous eruptions? Definitive answers to these questions still elude geoscientists. It is known that water greatly influences the properties of magmas, including magma viscosity, degree of crystallization of the melt, and whether a volcano erupts explosively or quietly extrudes magma flows.

This work explores the possibility that crystals formed from magmas in Mount St. Helens are "time capsules" of magmatic water content- more specifically, that the concentration of structural hydroxyl groups in the feldspar phenocrysts from each eruption is a proxy for the water content of the magma that it grew from. For more information about this research, and to find other web sites about Mount St. Helens, click on the links below.

Research on Mount St. Helens

Links to other Mount St. Helens web sites

Postcard picture of Mount St. Helens before the May 18, 1980 eruption.

Back to Liz Johnson's home page or the ESS web page

This material is based upon work supported by the National Science Foundation under Grant no. EAR-0409883. Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author and do not necessarily reflect the views of the National Science Foundation.