What controls eruption style?

"Probabilistic assessment of future vent locations and eruption styles for the Auckland Volcanic Field, New Zealand".

The eruption also lent its name to the "Peléan eruption style".

The more typical eruption style is a steady lava flow from a central vent, which can produce wide lava lakes, ponds of lava forming in craters or other depressions.

The eruption styles within the belt range from effusive to explosive, with compositions from basalt to rhyolite.

In the summer of 1997, it erupted in an event now defined as "Pillanian" eruption style.

His description of the eruption style is now used all over the world for eruptions characterised by a dense cloud of ash-laden gas exploding from the crater and rising high above the peak.

This new online-only publication has chapters covering the tectonic setting, rocks, eruption styles, landforms, community impact, effect on climate, and monitoring of Alaska's volcanoes.

This eruption style can take the form of either lava flows, spreading across the floor of the paterae, or lava lakes.

Explosion-dominated eruptions are the most pronounced of Io's eruption styles.