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Abstract Caldera-forming eruptions are among the most hazardous volcanic processes, particularly submarine ones. Yet, the dynamics of submarine caldera-forming eruptions and, thus, the hazards they pose are not well understood, owing to the relative inaccessibility of the resulting calderas and eruption products. Here we show the changes in geomorphology of Hunga volcano (Tonga) after the 15 January 2022 eruption.
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