5:15 PM - 7:15 PM
[MIS23-P03] Tsunami inundation events postdating the 18th century along the Pacific coast of eastern Hokkaido, inferred from non-destructive analyses
Keywords:XRF core scanner, CT images, Tsunami, Kuril trench
This study focuses on identifying event deposits formed after the 18th century, generated by tsunamis and storms, using non-destructive analyses along the Pacific coast of eastern Hokkaido.
Sediment samples postdating the 18th century were collected from the coasts of Nemuro, Hamanaka, and Taiki by excavating pits and using a handy geoslicer. We carried out non-destructive analyses (CT scanning and XRF analysis) on the samples in the laboratory. As a result, for example, high-density layers within the organic deposits/peat of the samples from Taiki were identified using X-ray computed tomography (CT) images. The XRF core scanner (ITRAX) detected clear peaks of Ca, Br, and Sr within these high-density layers. Based on chronology using Pb-210 and Cs-137, one of the high-density layers was found to correspond to the 1894 Nemuro earthquake.
[Acknowledgements] This study was performed under the cooperative research program of Marine Core Research Institute (MaCRI), Kochi University (22A002, 24A004, 24B004).
Sediment samples postdating the 18th century were collected from the coasts of Nemuro, Hamanaka, and Taiki by excavating pits and using a handy geoslicer. We carried out non-destructive analyses (CT scanning and XRF analysis) on the samples in the laboratory. As a result, for example, high-density layers within the organic deposits/peat of the samples from Taiki were identified using X-ray computed tomography (CT) images. The XRF core scanner (ITRAX) detected clear peaks of Ca, Br, and Sr within these high-density layers. Based on chronology using Pb-210 and Cs-137, one of the high-density layers was found to correspond to the 1894 Nemuro earthquake.
[Acknowledgements] This study was performed under the cooperative research program of Marine Core Research Institute (MaCRI), Kochi University (22A002, 24A004, 24B004).