Santorini is an example of a multi-cyclic caldera (a large depression formed when a volcano erupts and collapses) and its cycles are characterized by extended periods of effusive to mildly explosive volcanic activity between major caldera-forming events. To explore the submarine architecture of the caldera and its volcanic history, Jonas Preine and colleagues analysed sediments obtained from four deep coring sites from Kameni alongside seismic reflection data. Their findings suggest the caldera
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