HIGHLIGHTS
SUMMARY
The authors use scaled analog experiments and spectral analyses of well-preserved periodic terracing observed at the Sumisu and Santorini CCF eruption deposits to argue there are key quantitative clues to the dynamics governing CCF eruptions and their hazards in the terraced architectures of submarine CCF eruption deposits. The authors show that submarine eruptions in a ‘total collapse` (TC) regime deliver material to the water surface and seabed in periodic annular "sedimentation waves" (SW). SWs descending from powerful "deep water" eruption columns with heights comparable to the water depth, involves minimal interactions with the . . .
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