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Historical Nankai-Suruga megathrust earthquakes recorded by tsunami and terrestrial mass movement deposits on the Shirasuka coastal lowlands, Shizuoka Prefecture, Japan

Bibliographic Data

ID12265255
AuthorsEd Garrett (0000-0001-9985-0651, Durham University, corresponding author), Osamu Fujiwara (0000-0001-7749-5919, Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology, Japan), Svenja Riedesel (0000-0003-2936-8776, University of Cologne), J Walstra (0000-0001-9721-124X, Institute of Natural Sciences), Koen Deforce (0000-0003-3075-2564, Flanders Heritage Institute, Belgium), Yūsuke Yokoyama (0000-0001-7869-5891, Atmosphere and Ocean Research Institute, The University of Tokyo, Japan), Sabine Schmidt (0000-0002-5985-9747, UMR5805 EPOC, University of Bordeaux, France), Helmut Brückner (0000-0002-2130-5394, University of Cologne), Marc De Batist (0000-0002-1625-2080, Ghent University), Vanessa M A Heyvaert (0000-0001-7382-0120, Institute of Natural Sciences), Vanessa MA Heyvaert (Institute of Natural Sciences), and the QuakeRecNankai Team
Year2018
Volume28
Issue6
Pages968-983
Publication date2018-01-19
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1177/0959683617752844
OpenAlexW2783462251
LanguageEN
Citations received2
References cited79

Geological investigations of coastal sediment sequences play a key role in verifying earthquake and tsunami characteristics inferred from historical records. In this paper, we present a multi-proxy investigation of a coastal lowland site facing the Nankai-Suruga megathrust and appraise evidence for tsunamis and earthquake-triggered terrestrial mass movements occurring over the last 800 years. Combining a high-resolution chronology with X-ray computed tomography and analyses of particle size, diatoms, pollen, non-pollen palynomorphs and aerial photographs, we present the most compelling geological evidence of the 1361 CE Kōan (also known as Shōhei) tsunami reported to date from any site along the megathrust. This finding is consistent with either of two recent hypotheses: a single larger rupture of both the Nankai and Tōnankai regions or two smaller ruptures separated by a few days. Enhancing the site chronology using Bayesian age modelling, we verify evidence for inundation during the 1498 CE Meiō tsunami. While previous investigations identified evidence for historically recorded tsunamis in 1605, 1707 and 1854 CE and a storm surge in 1680 or 1699 CE, we encountered a thick sand layer rather than discrete extreme wave deposits in this interval. The overprinting of evidence highlights the potential for geological records to underestimate the frequency of these events. A terrestrial mass movement also deposited a sand layer at the site; radionuclide dating and aerial photographs provide independent confirmation that this may have been triggered by intense shaking in 1944 CE during the most recent great Nankai-Suruga megathrust earthquake

Chronology · Geologic record · Landslide · Mass movement · Overprinting · Seismology · Subduction · Tectonics · earthquake and tectonic studies · Geology and Paleoclimatology Research · Methane Hydrates and Related Phenomena · Geology · Oceanography · Paleontology

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