Hydrothermal Eruptions - John Seach

Hydrothermal eruptions are caused by catastrophic discharges of water close to the boiling point.
It is a phreatic eruption. No ash, incandesence, or clasts are erupted. Hydrothermal eruptions
may be caused by a reduction in the overlying pressure.

Examples of hydrothermal eruptions
Waiotapu (New Zealand)
Rotarua (New Zealand)
Kawah Komojang Field (Java, Indonesia)
Yangbajing (Tibet) Drilling induced
 

Hydrothermal Eruptions
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