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The summit craters represent the junction area of the volcanic activity through which breathes the persistent vent of Etna, and in more or less regular intervals, are the site of explosive events of various types as: Strombolian obstruction phreatic activities etc. that continually change the morphology.
Craters of the Moon geothermal area. The Taupo Volcanic Zone is a highly active volcanic V shaped area in the North Island of New Zealand that is spreading east-west at the rate of about 8mm per year. It is named after Lake Taupo, the flooded caldera of the largest volcano in the zone.he Taupo Volcanic Zone is approximately 350 kilometres (217 mi) long by 50 kilometres (31 mi) wide. Mount Ruapehu marks its southwestern end, while the submarine Whakatane volcano (85 kilometres (53 mi) beyond White Island) is considered its northeastern limit.