Earth scientists have devised a new method that simulates large explosive volcanic eruptions, paving the way for a better understanding of their impact.
The architecture of Bronze Age deposits left behind from undersea volcanic eruptions sheds light on its parent eruption.
Dr. Johan Gilchrist and Dr. Mark Jellinek examined the concentric terraces that surround the Santorini caldera—historically referred to as the Minoan eruption. Dr. Gilchrist suspected that sedimentation waves collapsing periodically around the volcanic jet spread where they touched the ocean surface during shallow subsurface eruptions.
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