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- W2007782885 abstract "In eastern Hokkaido, 60 to 80 kilometers above a subducting oceanic plate, tidal mudflats changed into freshwater forests during the first decades after a 17th-century tsunami. The mudflats gradually rose by a meter, as judged from fossil diatom assemblages. Both the tsunami and the ensuing uplift exceeded any in the region's 200 years of written history, and both resulted from a shallow plate-boundary earthquake of unusually large size along the Kuril subduction zone. This earthquake probably induced more creep farther down the plate boundary than did any of the region's historical events." @default.
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- W2007782885 date "2004-12-10" @default.
- W2007782885 modified "2023-10-16" @default.
- W2007782885 title "Transient Uplift After a 17th-Century Earthquake Along the Kuril Subduction Zone" @default.
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- W2007782885 doi "https://doi.org/10.1126/science.1104895" @default.
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