Most models for volcanic tremor rely on specific properties of the geometry, structure and constitution of volcanic conduits as well as the gas content of the erupting magma. Here, a model is used of a silicic magma rising in a conduit as a columnar plug to demonstrate that, for most geologically relevant conditions, the magma column will oscillate or 'wag' against the restoring force of a highly vesicular annulus of sheared bubbles at observed tremor frequencies. The frequencies produced are relatively insensitive to the conduit structure and geometry.
- A. Mark Jellinek
- David Bercovici
