Two-step movement of tsunami boulders unveiled by modified viscous remanent magnetization and radiocarbon dating
Massive boulders in landslide and tsunami deposits are prominent geomorphic features in various landscapes. Tracking their movement history is important for reconstructing past geologic dynamics; however, the reworking movements of massive boulders remain unresolved. The boulder field on the Ishigak...
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| Published in | Scientific reports Vol. 12; no. 1; pp. 13011 - 12 |
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| Main Authors | , , , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
London
Nature Publishing Group UK
29.07.2022
Nature Publishing Group Nature Portfolio |
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| Abstract | Massive boulders in landslide and tsunami deposits are prominent geomorphic features in various landscapes. Tracking their movement history is important for reconstructing past geologic dynamics; however, the reworking movements of massive boulders remain unresolved. The boulder field on the Ishigaki Island was formed by repeated tsunamis. Although the individual movement histories of boulders contribute to retrodict the history of different magnitude tsunamis, their radiocarbon ages only correspond to the tsunamis that detached boulders from the reef. Viscous remanent magnetization dating methods have been applied in reworking movements. These methods reveal signals associated with remanent magnetization that gradually grew since the reworking event, which helps to determine the passage of time. The methods were verified by comparison to the radiocarbon ages of un-reworked boulders detached by the recent Meiwa tsunami, while the estimated ages of such two boulders based on the classical relaxation theory contradicted the radiocarbon ages. Here, we show that a method based on the stretched exponential function addressed this contradiction. The reworking movement was estimated using an additional boulder, whose, using our method, radiocarbon age indicated that an older tsunami moved it, whereas the remanent magnetization age unveiled a reworking of the boulder attributed to the Meiwa tsunami. |
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| AbstractList | Massive boulders in landslide and tsunami deposits are prominent geomorphic features in various landscapes. Tracking their movement history is important for reconstructing past geologic dynamics; however, the reworking movements of massive boulders remain unresolved. The boulder field on the Ishigaki Island was formed by repeated tsunamis. Although the individual movement histories of boulders contribute to retrodict the history of different magnitude tsunamis, their radiocarbon ages only correspond to the tsunamis that detached boulders from the reef. Viscous remanent magnetization dating methods have been applied in reworking movements. These methods reveal signals associated with remanent magnetization that gradually grew since the reworking event, which helps to determine the passage of time. The methods were verified by comparison to the radiocarbon ages of un-reworked boulders detached by the recent Meiwa tsunami, while the estimated ages of such two boulders based on the classical relaxation theory contradicted the radiocarbon ages. Here, we show that a method based on the stretched exponential function addressed this contradiction. The reworking movement was estimated using an additional boulder, whose, using our method, radiocarbon age indicated that an older tsunami moved it, whereas the remanent magnetization age unveiled a reworking of the boulder attributed to the Meiwa tsunami. Abstract Massive boulders in landslide and tsunami deposits are prominent geomorphic features in various landscapes. Tracking their movement history is important for reconstructing past geologic dynamics; however, the reworking movements of massive boulders remain unresolved. The boulder field on the Ishigaki Island was formed by repeated tsunamis. Although the individual movement histories of boulders contribute to retrodict the history of different magnitude tsunamis, their radiocarbon ages only correspond to the tsunamis that detached boulders from the reef. Viscous remanent magnetization dating methods have been applied in reworking movements. These methods reveal signals associated with remanent magnetization that gradually grew since the reworking event, which helps to determine the passage of time. The methods were verified by comparison to the radiocarbon ages of un-reworked boulders detached by the recent Meiwa tsunami, while the estimated ages of such two boulders based on the classical relaxation theory contradicted the radiocarbon ages. Here, we show that a method based on the stretched exponential function addressed this contradiction. The reworking movement was estimated using an additional boulder, whose, using our method, radiocarbon age indicated that an older tsunami moved it, whereas the remanent magnetization age unveiled a reworking of the boulder attributed to the Meiwa tsunami. Massive boulders in landslide and tsunami deposits are prominent geomorphic features in various landscapes. Tracking their movement history is important for reconstructing past geologic dynamics; however, the reworking movements of massive boulders remain unresolved. The boulder field on the Ishigaki Island was formed by repeated tsunamis. Although the individual movement histories of boulders contribute to retrodict the history of different magnitude tsunamis, their radiocarbon ages only correspond to the tsunamis that detached boulders from the reef. Viscous remanent magnetization dating methods have been applied in reworking movements. These methods reveal signals associated with remanent magnetization that gradually grew since the reworking event, which helps to determine the passage of time. The methods were verified by comparison to the radiocarbon ages of un-reworked boulders detached by the recent Meiwa tsunami, while the estimated ages of such two boulders based on the classical relaxation theory contradicted the radiocarbon ages. Here, we show that a method based on the stretched exponential function addressed this contradiction. The reworking movement was estimated using an additional boulder, whose, using our method, radiocarbon age indicated that an older tsunami moved it, whereas the remanent magnetization age unveiled a reworking of the boulder attributed to the Meiwa tsunami.Massive boulders in landslide and tsunami deposits are prominent geomorphic features in various landscapes. Tracking their movement history is important for reconstructing past geologic dynamics; however, the reworking movements of massive boulders remain unresolved. The boulder field on the Ishigaki Island was formed by repeated tsunamis. Although the individual movement histories of boulders contribute to retrodict the history of different magnitude tsunamis, their radiocarbon ages only correspond to the tsunamis that detached boulders from the reef. Viscous remanent magnetization dating methods have been applied in reworking movements. These methods reveal signals associated with remanent magnetization that gradually grew since the reworking event, which helps to determine the passage of time. The methods were verified by comparison to the radiocarbon ages of un-reworked boulders detached by the recent Meiwa tsunami, while the estimated ages of such two boulders based on the classical relaxation theory contradicted the radiocarbon ages. Here, we show that a method based on the stretched exponential function addressed this contradiction. The reworking movement was estimated using an additional boulder, whose, using our method, radiocarbon age indicated that an older tsunami moved it, whereas the remanent magnetization age unveiled a reworking of the boulder attributed to the Meiwa tsunami. |
| ArticleNumber | 13011 |
| Author | Saito, Hirotake Satake, Kenji Nakamura, Norihiro Miyairi, Yosuke Goto, Kazuhisa Sato, Masahiko Yamada, Masaki Yokoyama, Yusuke Sato, Tetsuro |
| Author_xml | – sequence: 1 givenname: Tetsuro surname: Sato fullname: Sato, Tetsuro email: tetsuro.sato@aoni.waseda.jp organization: Department of Earth Science, School of Education, Waseda University, Earthquake Research Institute, The University of Tokyo – sequence: 2 givenname: Masahiko surname: Sato fullname: Sato, Masahiko organization: Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo – sequence: 3 givenname: Masaki surname: Yamada fullname: Yamada, Masaki organization: Department of Geology, Faculty of Science, Shinshu University – sequence: 4 givenname: Hirotake surname: Saito fullname: Saito, Hirotake organization: Department of Geology, Faculty of Science, Shinshu University – sequence: 5 givenname: Kenji surname: Satake fullname: Satake, Kenji organization: Earthquake Research Institute, The University of Tokyo – sequence: 6 givenname: Norihiro surname: Nakamura fullname: Nakamura, Norihiro organization: Institute for Excellence in Higher Education, Tohoku University – sequence: 7 givenname: Kazuhisa surname: Goto fullname: Goto, Kazuhisa organization: Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo – sequence: 8 givenname: Yosuke surname: Miyairi fullname: Miyairi, Yosuke organization: Atmosphere and Ocean Research Institute, The University of Tokyo – sequence: 9 givenname: Yusuke surname: Yokoyama fullname: Yokoyama, Yusuke organization: Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo, Atmosphere and Ocean Research Institute, The University of Tokyo, Graduate Program on Environmental Sciences, Graduate School of Arts and Sciences, The University of Tokyo, Japan Agency for Marine-Earth Science and Technology, Biogeochemistry Research Center, Research School of Physics, The Australian National University |
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| Snippet | Massive boulders in landslide and tsunami deposits are prominent geomorphic features in various landscapes. Tracking their movement history is important for... Abstract Massive boulders in landslide and tsunami deposits are prominent geomorphic features in various landscapes. Tracking their movement history is... |
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| SubjectTerms | 704/2151/213 704/2151/215 704/2151/2809 704/2151/412 704/4111 Dating Humanities and Social Sciences Landslides Magnetism multidisciplinary Radiocarbon dating Science Science (multidisciplinary) Tsunamis |
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| Title | Two-step movement of tsunami boulders unveiled by modified viscous remanent magnetization and radiocarbon dating |
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