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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, and the Dallol crater, formed in 1926, was the result of a phreatic eruption. pools best explained by a number of active maar craters. evaporite succession and frequent marine invasions of the salt plain during the Holocene. Evaporites and Geothermal reservoir.