Recent analysis of the composition of tiny crystals inside ash deposits from prehistoric eruptions is overturning old beliefs about supervolcano behavior--and revealing new surprises about the aftermath.
The inner workings of the magma chambers that fuel supervolcanoes can evolve in ways that strongly influence the style of future eruptions.
The volcanic winter that grips the planet in the wake of a supereruption is probably shorter than once suspected, although chemical reactions in the atmosphere may be much more dangerous.