Skip to main content
Log in

The 2011 Tohoku-oki Earthquake Tsunami: Similarities and Differences to the 869 Jogan Tsunami on the Sendai Plain

  • Published:
Pure and Applied Geophysics Aims and scope Submit manuscript

Abstract

A post-tsunami field survey following the 2011 Tohoku-oki Earthquake Tsunami was carried out to asses inundated area in Sendai Plain, Northeast Japan. The type of inundation was classified into two categories (major and minor) according to the amount of accumulated debris, garbage and sediment. Major and minor inundations were identified up to 4 and 5 km from the coastline, respectively. Many artificial geomorphological features, such as roadway embankments and canals, were believed to have affected the run-up process of the tsunami. The inundation area of the 2011 tsunami on the Sendai Plain is compared with that of the 869 Jogan tsunami, which was reconstructed using numerical modeling based on available historical and geological records. The inundation area of the 2011 Tohoku-oki tsunami is comparable to that of the 869 Jogan tsunami, although a direct comparison is difficult due to differences in geomorphological contexts between the paleo period and the present.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8

Similar content being viewed by others

References

  • Abe, I., Abe, T., Arai, K., Fujima, K., Fujino, S., Gokon, H., Goto, K., Harada, K., Haraguchi, T., Imai, K., Imamura, F., Koshimura, S., Murashima, Y., Naruse, H., Seto, S., Shigihara, Y., Sugawara, D., Takahashi, T., Tsudaka, R., Yamashita, S. (2011), High resolution survey results for the inundation limit and height of the 2011 Tohoku earthquake tsunami, Abstract of the Japan Geoscience Union Meeting 2011, May 22–27, Makuhari, Chiba, Japan, MIS036-P120.

  • Abe, H., Sugeno, Y., and Chigama, A. (1990), Estimation of the height of the Sanriku Jogan 11 Earthquake-tsunami (A.D. 869) in the Sendai Plain, J. Seismol. Soc. Japan (Zishin) 43, 513–525 (in Japanese with English abstract).

  • Geographical Survey Institute (1984), Report of fundamental research of coastal area (Sendai Bay), GSI technical reference, D 3, No. 51, Tsukuba, Japan.

  • Goto, K., Chagué-Goff C., Fujino, S., Goff, J., Jaffe, B., Nishimura, Y., Richmond, B., Sugawara, D., Szczuciński, W., Tappin, D. R., Witter, R. C. and Yulianto, E. (2011), New insights of tsunami hazard from the 2011 Tohoku-oki event, Marine Geology 290, 46–50.

  • Haraguchi, T., Torii, K., Fujiwara, O., Shimazaki, K., and Imaizumi T. (2006), Tsunami deposits from Otsuchi Bay in Sanriku Coast, northeast Japan, Chikyu 28 (8), 539–545 (in Japanese).

  • Hatori, T. (1987), Distributions of Seismic Intensity and Tsunami of the 1793 Miyagi Oki Earthquake, Northeastern Japan, Bull. Earthq. Res. Inst. 62, 297–309 (in Japanese).

  • Ito, A. (2006). Marine Regression During the Historical Time in Sendai Coastal Plain, Northeast Japan, Bulletin of the Faculty of Education, Kagoshima University, Natural science 57, 1–8. (in Japanese).

  • IUGG/IOC TIME PROJECT (1997), IOC Manuals and Guides, No. 35, UNESCO.

  • Lay, T., Ammon, C. J., Kanamori, H., Xue, L., and Kim., M. J. (2011), Possible large near-trench slip during the 2011 Mw 9.0 off the Pacific coast of Tohoku Earthquake, Earth Planets Space 63, 687–692.

  • Lay, T., and Kanamori, H. (2011), Insights from the great 2011 Japan earthquake, Phys. Today 64 (12), 33–39; doi: 10.1063/PT.3.1361.

  • Matsumoto, H. (1985). Beach Ridge Ranges and the Holocene Sea-level Fluctuations on Alluvial Coastal Plains, Northeast Japan, Sci. Rep. Tohoku Univ., 7th series (geography) 35, 15–46.

  • Minoura, K., and Nakaya, S. (1991), Traces of tsunami preserved in inter-tidal lacustrine and marsh deposits: some examples from northeastern Japan, J. Geol. 99, 265.

  • Minoura, K., Imamura, F., Sugawara, D., Kono, Y., and Iwashita, T. (2001), The 869 Jogan tsunami deposit and recurrence interval of large scale tsunami on the Pacific coast of northeastern Japan, J. Natur. Disast. Sci. 23, 83–88.

  • Mori, N., Takahashi, T., Yasuda, T., and Yanagisawa H. (2011), Survey of 2011 Tohoku earthquake tsunami inundation and run-up, Geophysical Research Letters 38, L00G14, doi:10.1029/2011GL049210.

  • Namegaya, Y., Satake, K., and Yamaki, S. (2010), Numerical simulation of the AD 869 Jogan tsunami in Ishinomaki and Sendai plains and Ukedo river-mouth lowland, Annual Report of Active Fault and Paleoearthquake Researches 10, 1–21 (in Japanese with English Abstract).

  • Normile, D. (2011), Scientific Consensus on Great Quake Came Too Late, Science 332, 22–23.

  • Okada, Y. (1985), Surface deformation due to shear and tensile faults in a half-space, Bull. Seismol. Soc. Am. 75, 1135–1154.

  • Ozawa, S., Nishimura, T., Suito, H., Kobayashi, T., Tobita, M., and Imakiire, T. (2011), Coseismic and postseismic slip of the 2011 magnitude-9 Tohoku-Oki earthquake, Nature 475, 373–376.

  • Satake, K., Nanayama, H., and Yamaki, S. (2003), Source models of the unusual tsunami in the 17th century in eastern Hokkaido, Annual Report of Active Fault and Paleoearthquake Researches 3, 315–362 (in Japanese with English Abstract).

  • Satake, K., Namegaya, Y., and Yamaki, S. (2008), Numerical simulation of the AD 869 Jogan tsunami in Ishinomaki and Sendai Plains, Annual Report of Active Fault and Paleoearthquake Research 8, 71–89 (in Japanese with English Abstract).

  • Sato, R. (1979), Theoretical basis on relationships between focal parameters and earthquake magnitude, J. Phys. Earth 27, 353–372.

  • Sawai, Y., Shishikura, M., Okamura, Y., Takada, K., Matsu’ura, T., Aung, T. T., Komatsubara, J., Fujii, Y., Fujiwara, O., Satake, K., Kamataki, T., and Sato, N. (2007), A study of paleotsunami using handy geoslicer in Sendai Plain (Sendai, Natori, Iwanuma, Watari, and Yamamoto), Miyagi, Japan, Annual Report of Active Fault and Paleoearthquake Researches 7, 47–80 (in Japanese with English Abstract).

  • Sawai, Y., Shishikura, M., and Komatsubara, J. (2008), A study of paleotsunami using hand corer in Sendai plain (Sendai City, Natori City, Iwanuma City, Watari Town, Yamamoto Town), Miyagi, Japan, Annual Report of Active Fault and Paleoearthquake Researches 8, 17–70 (in Japanese with English Abstract).

  • Shishikura, M., Sawai, Y., Okamura, Y., Komatsubara, J., Aung, T. T., Ishiyama, T., Fujiwara, O., and Fujino, S. (2007), Age and distribution of tsunami deposit in the Ishinomaki Plain, northeastern Japan, Annual Report of Active Fault and Paleoearthquake Researches 7, 31–46 (in Japanese with English Abstract).

  • Sugawara, D., Imamura, F., Matsumoto, H., Goto, K., and Minoura, K. (2010), Numerical reconstruction of ancient tsunami: field survey of the Jogan tsunami and estimation of paleo-topography, DCRC tsunami engineering 27, 103–132 (in Japanese).

  • Sugawara, D., Imamura, F., Matsumoto, H., Goto, K., and Minoura K. (2011), Reconstruction of the AD 869 Jogan earthquake induced tsunami by using the geological data, J. Japan Soc. Natur. Disast. Sci. 29 (4), 501–516 (in Japanese with English abstract).

  • Sugawara, D., Imamura, F., Goto, K., Matsumoto, H., and Minoura, K. (2011b), Inundation area by the 2011 Tohoku earthquake tsunami in Sendai plain: comparison to the 869 Jogan earthquake tsunami, Abstract of the Japan Geoscience Union Meeting 2011, May 22–27, Makuhari, Chiba, Japan, MIS036-P129.

  • Suzuki, H., Imaizumi, T., Ishiyama, T., Miyauchi, T., Kagohara, K., Haraguchi, T., Murashima, N., and Omachi, T. (2009), Holocene tsunami deposits associated with earthquakes along Pacific coast, northeast Japan, EOS Trans. AGU 90 (52), Fall Meet. Suppl., T33B-1884.

  • Torii K., Haraguchi, T., Imaizumi, T., Miyauchi, T., and Shimazaki, K. (2007), Field survey of tsunami deposit in Sanriku Coast, Northeast Japan, Proc. Japanese Soc. Eng. Geol., pp.23.

  • Watanabe, H. (1985), Comprehensive list of disaster tsunamis in Japan, Press of Tokyo University, Tokyo, Japan, (in Japanese).

  • Watanabe, H. (2001), Is it possible to clarify the real state of past earthquakes and tsunamis on the basis of legends? As an example of the 869 Jogan earthquake and tsunami, Histor. Earthq (Rekishi-jishin) 17, 130–146 (in Japanese).

Download references

Acknowledgments

The post-tsunami field survey following the 2011 earthquake was conducted with support from a special grant under the “Emergency tsunami field survey in the Pacific coast of Tohoku Region” from the Ministry of Education, Culture, Sports, Science and Technology, Japan. The field survey and numerical modeling of the Jogan tsunami was supported by the Tohoku University GCOE program “Global Education and Research Center for Earth and Planetary Dynamics” and by the Grant-in-Aid for Scientific Research (A), 22241042, 2010, from the Ministry of Education, Science, Sports and Culture.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Daisuke Sugawara.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Sugawara, D., Imamura, F., Goto, K. et al. The 2011 Tohoku-oki Earthquake Tsunami: Similarities and Differences to the 869 Jogan Tsunami on the Sendai Plain. Pure Appl. Geophys. 170, 831–843 (2013). https://doi.org/10.1007/s00024-012-0460-1

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00024-012-0460-1

Keywords

Navigation