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Project > Geological History of Sites > The Nisyros Hydrothermal Crater Field
The Nisyros Hydrothermal Crater Field
The Nisyros Hydrothermal Crater Field IntroductionHydrothermal craters (Fig. 36) are formed mainly by steam and gas explosions
of a hydrothermal system near the surface within or in the vicinity of a volcanic
caldera, mostly due to steam overpressure and not to a magmatic eruption. Fig. 36 The Nisyros hydrothermal crater field within the
caldera (Ikonos image, 30.4.2000, resolution 1 m), red points: monitored fumaroles.
Swiss Federal Institute of Technology (ETHZ)
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