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Paleotsunamis from the central Kuril Islands segment of the Japan-Kuril-Kamchatka subduction zone

Published online by Cambridge University Press:  20 January 2017

Breanyn MacInnes ,
Ekaterina Kravchunovskaya ,
Tatiana Pinegina  and
Joanne Bourgeois
Breanyn MacInnes*
Affiliation:
Department of Geological Sciences, Central Washington University, 400 E University Way, Ellensburg, WA 98926-7418, USA
Tatiana Pinegina
Affiliation:
Institute of Volcanology and Seismology, Far Eastern Branch, Russian Academy of Sciences, Petropavlovsk-Kamchatskiy, 683006, Russia
Joanne Bourgeois
Affiliation:
Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195, USA
*
*[email protected] (B. MacInnes)
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Abstract

Paleotsunami records from the central Kuril Island segment of the Japan-Kuril-Kamchatka subduction zone indicate that the region has been frequently inundated by tsunamis. As many as 20e22 tsunami deposits are recognized on Matua Island for the past 3300 yr with an average tsunami recurrence interval of ~150 yr, and 34e36 tsunami deposits are evident on Simushir Island for the past 2350 yr with an average recurrence of ~65 yr. These intervals are short, but comparable to other segments of the Japan-Kuril-Kamchatka subduction zone. Results from all survey locations reveal shortening recurrence intervals toward the present, especially for the last 600 yr, indicating a possible preservation bias. On Simushir, tsunamis at least 11 m higher than the modern tsunamis in 2006 and 2007 occurred every ~300 yr on average. On Matua, tsunamis with slightly farther inundation than the 2006 and 2007 tsunamis occurred every ~215 yr while those with at least 100 m farther inland inundation occur every ~750 yr. Our paleotsunami record almost certainly includes tsunamis that are not from great subduction zone earthquakes in the central Kuril segment: we expect the Matua record includes volcanic tsunamis and the Simushir record includes tsunamis from the southern Kuril segment.

Keywords

TsunamiPaleotsunamiKuril Islands
Type
Research Article
Information
Quaternary Research , Volume 86 , Issue 1 , July 2016 , pp. 54 - 66
Copyright
Copyright © American Quaternary Association 2016 

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References

Ammon, C.J., Kanamori, H., Lay, T., 2008. A great earthquake doublet and seismic stress transfer cycle in the central Kuril islands. Nature 451, 561–566.Google Scholar
Apel, E.V., Bürgmann, R., Steblov, G., Vailenko, N., King, R., Prytkov, A., 2006. Independent active microplate tectonics of northeast Asia from GPS velocities and block modeling. Geophysical Research Letters 33, L11303. http://dx.doi.org/ 10.1029/2006GL026077.Google Scholar
Beck, S.L., Ruff, L.J., 1987. Rupture process of the great 1963 Kurile Islands earthquake sequence: asperity interaction and multiple event rupture. Journal of Geophysical Research 92, 14, 123–14,138. http://dx.doi.org/10.1029/JB092iB13p14123.Google Scholar
Bird, P., 2003. An updated digital model of plate boundaries. Geochemistry, Geophysics, Geosystems 4 (3). http://dx.doi.org/10.1029/2001GC000252.Google Scholar
Bourgeois, J., Pinegina, T.K., Ponomareva, V.V., Zaretskaia, N.E., 2006. Holocene tsunamis in the southwestern Bering Sea, Russian Far East, and their tectonic implications. Geological Society of America Bulletin 118, 449–463. http://dx.doi.org/10.1130/B25726.1.Google Scholar
Bronk Ramsey, C., 2009. Bayesian analysis of radiocarbon dates. Radiocarbon 51 (1), 337–360.Google Scholar
Clague, J.J., Bobrowsky, P.T., Hutchinson, I., 2000. A review of geological records of large tsunamis at Vancouver Island, British Columbia, and implications for hazard. Quaternary Science Reviews 19 (9), 849–863.Google Scholar
Dengler, L., Uslu, B., Barberopoulou, A., Yim, S.C., Kelly, A., 2009. The November 15, 2006 Kuril Islands-generated tsunami in Crescent City, California. Pure and Applied Geophysics 166, 37–53.Google Scholar
Dura, T., Cisternas, M., Horton, B.P., Ely, L.L., Nelson, A.R., Wesson, R.L., Pilarczyk, J.E., 2015. Coastal evidence for Holocene subduction-zone earthquakes and tsunamis in central Chile. Quaternary Science Reviews 113, 93–111.Google Scholar
Ely, L.L., Cisternas, M., Wesson, R.L., Dura, T., 2014. Five centuries of tsunamis and land-level changes in the overlapping rupture area of the 1960 and 2010 Chilean earthquakes. Geology 42 (11), 995–998.Google Scholar
Fedotov, S.A., 1965. Regularities of the distribution of large earthquakes of Kamchatka, the Kuril Islands and north-eastern Japan. Akademii Nauk SSSR Institute Fiziki Zemli Trudy 36 (203), 66–93 ([in Russian]).Google Scholar
Fedotov, S.A., 1968. On the seismic cycle, possibilities of quantitative seismic zonation, and long-term earthquake prediction. In: Seismicheskoe raionirovanie SSSR (Seismic Zonation of the USSR). Nauka, Moscow, pp. 121–150.Google Scholar
Fedotov, S.A., Chernyshev, S.D., Chernysheva, G.V., 1982. The improved determination of the source boundaries for earthquakes of M>7.75, of the properties of the seismic cycle, and of long-term seismic prediction for the Kurile-Kamchatka Arc. Earthquake Prediction Research 1, 153–171.7.75,+of+the+properties+of+the+seismic+cycle,+and+of+long-term+seismic+prediction+for+the+Kurile-Kamchatka+Arc.+Earthquake+Prediction+Research+1,+153–171.>Google Scholar
Fitzhugh, B., Shubin, V.O., Tezuka, K., Ishizuka, Y., Mandryk, C.A., 2002. Archaeology in the Kuril Islands: advances in the study of human paleobiogeography and Northwest Pacific prehistory. Arctic Anthropology 69–94.Google Scholar
Fitzhugh, B., 2012. Chapter 1. Hazards, impacts, and resilience among hunter-gatherers of the Kuril Islands. In: Cooper, J., Sheets, P. (Eds.), Surviving Sudden Environmental Change: Answers from Archaeology. U. Colorado Press, Boulder, CO, pp. 19–42.Google Scholar
Fitzhugh, B., Gjesfjeld, E., Brown, W., Hudson, M.J., Shaw, J.D., 2016. Resilience and the population history of the Kuril Islands, Northwest Pacific: a study in complex human ecodynamics. Quaternary International. http://dx.doi.org/10.1016/j.quaint.2016.02.003.Google Scholar
Ganzey, L.A., Razjigaeva, N.G., Grebennikova, T.A., Lyashevskaya, M.S., Il’ev, A.Y., Kaistrenko, V.M., Kharlamov, A.A., 2011. Influence of natural catastrophes on the development of Southern Kuril Island landscapes in the Holocene. Quaternary International 237 (1), 15–23.Google Scholar
Geller, R.J., Kanamori, H., 1977. Magnitudes of great shallow earthquakes from 1904 to 1952. Bulletin of the Seismological Society of America 67, 587–598.Google Scholar
Golder, F., 1914. Russian Expansion on the Pacific, 1641–1850: an Account of the Earliest and Later Expeditions Made by the Russians along the Pacific Coast of Asia and North America; Including Some Related Expeditions to the Arctic Regions. The Arthur H. Clark co.Google Scholar
Gorshkov, G.S., 1958. Catalog of the Active Volcanoes of the World Including Solfatara Fields. P. VII. Kurile Islands. Inter. Volcanological Assoc, Napoli, Italy, p. 99.Google Scholar
Gorshkov, G.S., 1967. Volcanism of Kurile Island Arc. M.: Nauka, 287 p. (in Russian).Google Scholar
Goto, K., Chagué-Goff, C., Fujino, S., Goff, J., Jaffe, B., Nishimura, Y., Richmond, B., Sugawara, D., Szczuciński, W., Tappin, D., Witter, R.C., Yulianto, E., 2011. New insights of tsunami hazard from the 2011 Tohoku-oki event. Marine Geology 290, 46–50. http://dx.doi.org/10.1016/j.margeo.2011.10.004.Google Scholar
Hatori, T., 1971. Tsunami sources in Hokkaido and southern Kurile regions. Bulletin of the Earthquake Research Institute 49, 63–75.Google Scholar
Ide, S., Baltay, A., Beroza, G.C., 2011. Shallow dynamic overshoot and energetic deep rupture in the 2011 Mw 9.0 Tohoku-Oki earthquake. Science 332 (6036), 1422–1429. http://dx.doi.org/10.1126/science.1207020.Google Scholar
Iliev, A.Y., Kaistrenko, V.M., Gretskaya, E.V., Tikhonchuk, E.A., Razjigaeva, N.G., Grebennikova, T.A., Ganzey, L.A., Kharlamov, A.A., 2005. Holocene tsunami traces on Kunashir Island, Kurile subduction zone. In: Satake, K. (Ed.), Tsunamis: Case Studies and Recent Developments; Advances in Natural and Technological Hazards Research. Springer, Netherlands, pp. 171–192.Google Scholar
Kelsey, H.M., Nelson, A.R., Hemphill-Haley, E., Witter, R.C., 2005. Tsunami history of an Oregon coastal lake reveals a 4650 yr record of great earthquakes on the Cascadia subduction zone. Geological Society of America Bulletin 117, 7–8, 1009-1032.Google Scholar
Krasheninnikov, S.P., 1972. Explorations of Kamchatka, North Pacific Scimitar; Report of a Journey Made to Explore Eastern Siberia in 1735-1741, by Order of the Russian Imperial Government. Oregon Historical Society, Portland.Google Scholar
Laverov, N.P., Dobrezov, N.L., Bogatikov, O.A., Bondur, V.G., Gurbaniv, A.G., Karamurzov, B.S., Kovalenko, V.I., 2005. Modern and Holocene Volcanism in Russia. Nauka, Moscow, 604 pp. [in Russian].Google Scholar
Laverov, N.P., Lappo, S.S., Lobkovsky, L.I., Baranov, B.V., Kulinich, R.G., Karp, B.Y., 2006. The central Kuril “gap”: structure and seismic potential. Doklady Earth Science 409, 787–790. http://dx.doi.org/10.1134/S1028334X06050254.Google Scholar
Lay, T., Kanamori, H., Ammon, C.J., Hutko, A.R., Furlong, K., Rivera, L., 2009. The 2006–2007 Kuril Islands great earthquake sequence. Journal of Geophysical Research 114, B11308. http://dx.doi.org/10.1029/2008JB006280.Google Scholar
Lensen, G.A., 1959. The Russian Push toward Japan; Russo-Japanese Relations, 1697–1875. Princeton University Press, Princeton, N.J.Google Scholar
MacInnes, B.T., 2010. Bridging Seismology and Geomorphology: Investigations of the 2006 and 2007 Kuril Island Tsunamis. Ph.D. dissertation. University of Washington, Seattle, 177 pp.Google Scholar
MacInnes, B.T., Weiss, R., Bourgeois, J., Pinegina, T.K., 2010. Slip distribution of the 1952 Kamchatka great earthquake based on near-field tsunami deposits and historical records. Bulletin of the Seismological Society of America. http://dx.doi.org/10.1785/0120090376.Google Scholar
MacInnes, B.T., Pinegina, T.K., Bourgeois, J., Razhegaeva, N.G., Kaistrenko, V.M., Kravchunovskaya, E.A., 2009a. Field survey and geological effects of the 15 November 2006 Kuril tsunami in the middle Kuril Islands. Pure and Applied Geophysics 166. http://dx.doi.org/10.1007/s00024-008-0428-3.Google Scholar
MacInnes, B.T., Bourgeois, J., Pinegina, T.K., Kravchunovskaya, E., 2009b. Tsunami geomorphology: erosion and deposition from the 15 November 2006 Kuril Island tsunami. Geology 37, 995–998.Google Scholar
MacInnes, B., Fitzhugh, B., Holman, D., 2014. Controlling for landform age when determining the settlement history of the Kuril Islands. Geoarchaeology 29 (3), 185-201.Google Scholar
Mackey, K.G., Fujita, K., Gunbina, L., Kovalev, V., Imaev, V., Kozmin, B., 1997. Seismicity of the Bering Strait region: evidence for a Bering block. Geology 25, 979–982. http://dx.doi.org/10.1130/0091-7613(1997)025<0979:SOTBSR>2.3.CO;2.2.3.CO;2.>Google Scholar
Minoura, K., Gusiakov, V.G., Kurbatov, A., Takeuti, S., Svendsen, J.I., Bondevik, S., Oda, T., 1996. Tsunami sedimentation associated with the 1923 Kamchatka earthquake. Sedimentary Geology 106 (1), 145–154.Google Scholar
Miyatake, K., 1934. On the explosion of volcano Harumukotan-jima, central Kurile (Chishima), in Jan., 1933. Bulletin of the Volcanological Society of Japan 2, 76–85 (in Japanese).Google Scholar
Morton, R.A., Gelfenbaum, G., Jaffe, B.E., 2007. Physical criteria for distinguishing sandy tsunami and storm deposits using modern examples. Sedimentary Geology 200, 184–207.Google Scholar
Nakagawa, M., Ishizuka, Y., Hasegawa, T., Baba, A., Kosugi, A., 2008. Preliminary Report on Volcanological Research of KBP 2007–08 Cruise by Japanese Volcanology Group. The Digital Archaeological Record, tDAR ID: 391304. http:// dx.doi.org/10.6067/XCV8668F2H.Google Scholar
Nanayama, F., Satake, K., Furukawa, R., Shimokawa, K., Atwater, B.F., Shigeno, K., Yamaki, S., 2003. Unusually large earthquakes inferred from tsunami deposits along the Kuril trench. Nature 424 (6949), 660–663.Google Scholar
National Geophysical Data Center/World Data Service (NGDC/WDS). Global Historical Tsunami Database. National Geophysical Data Center, NOAA. doi: 10.7289/V5PN93H7 (accessed 2014).Google Scholar
Nelson, A.R., Briggs, R.W., Dura, T., Engelhart, S.E., Gelfenbaum, G., Bradley, L.-A., Forman, S.L., Vane, C.H., Kelley, K.A., 2015. Tsunami recurrence in the eastern Alaska-Aleutian arc: a Holocene stratigraphic record from Chirikof Island, Alaska. Geosphere 11 (4). http://dx.doi.org/10.1130/GES01108.1.Google Scholar
Nelson, A.R., Kelsey, H.M., Witter, R.C., 2006. Great earthquakes of variable magnitude at the Cascadia subduction zone. Quaternary Research 65 (3), 354–365.Google Scholar
Ogryzko, I.I., 1953. Discovery of Kurile Islands, The Scientific Notes of Leningrad State University, Faculty of Northern People, vol. 2, p. 157.Google Scholar
Okal, E., 1992. Use of mantle magnitude Mm for the reassessment of the moment of historical earthquakes I: shallow events. Pure and Applied Geophysics 139, 17-57.Google Scholar
Okal, E.A., Synolakis, C.E., 2004. Source discriminants for near-field tsunamis. Geophysical Journal International 158 (3), 899–912.Google Scholar
Pacheco, J.F., Sykes, L.R., 1992. Seismic moment catalog of large shallow earthquakes, 1900 to 1989. Bulletin of the Seismological Society of America 8, 1306–1349.Google Scholar
Pinegina, T., 2014. Time-space Distribution of Tsunamigenic Earthquakes along the Pacific and Bering Coasts of Kamchatka: Insight from Paleotsunami Deposits. Doctor of Geological Science dissertation. Institute of Oceanology RAS, Moscow, 235 pp. [in Russian].Google Scholar
Pinegina, T.K., Bourgeois, J., Bazanova, L.I., Melekestsev, I.V., Braitseva, O.A., 2003. A millennial-scale record of Holocene tsunamis on the Kronotskiy Bay coast, Kamchatka, Russia. Quaternary Research 59 (1), 36–47.Google Scholar
Pinegina, T.K., Bourgeois, J., Kravchunovskaya, E.A., Lander, A.V., Arcos, M.E., Pedoja, K., MacInnes, B.T., 2013. A nexus of plate interaction: vertical deformation of Holocene wave-built terraces on the Kamchatsky Peninsula (Kamchatka, Russia). Geological Society of America Bulletin 125, 9–10, 1554-1568.Google Scholar
Rabinovich, A.B., Lobkovsky, L.I., Fine, I.V., Thomson, R.E., 2008. Source observations and modeling of the Kuril Islands tsunamis of 15 November 2006 and 13 January 2007. Advances in Geosciences 14, 105–116.Google Scholar
Razzhigaeva, N.G., Ganzei, L.A., Grebennikova, T.A., Kharlamov, A.A., Ilyev, A.Y., Kaistrenko, V.M., 2008. The geological record of paleotsunamis striking Shikotan Island, in the lesser Kurils, during Holocene time. Journal of Volcanology and Seismology 2 (4), 262–277.Google Scholar
Razjigaeva, N.G., Ganzey, L.A., Grebennikova, T.A., Ivanova, E.D., Kharlamov, A.A., Kaistrenko, V.M., Shishkin, A.A., 2012. Coastal sedimentation associated with the Tohoku tsunami of 11 March 2011 in South Kuril Islands, NW Pacific Ocean. Pure and Applied Geophysics. http://dx.doi.org/10.1007/s00024-012-0478-4.Google Scholar
Romundset, A., Bondevik, S., 2011. Propagation of the Storegga tsunami into ice-free lakes along the southern shores of the Barents Sea. Journal Of Quaternary Science 26 (5), 457–462. http://dx.doi.org/10.1002/jqs.1511.Google Scholar
Sadler, P.M., 1981. Sediment accumulation rates and the completeness of stratigraphic sections. The Journal of Geology 569–584.Google Scholar
Sawai, Y., Kamataki, T., Shishikura, M., Nasu, H., Okamura, Y., Satake, K., Thomson, K.H., Matsumoto, D., Fujii, Y., Komatsubara, J., Aung, T.T., 2009. Aperiodic recurrence of geologically recorded tsunamis during the past 5500 years in eastern Hokkaido, Japan. Journal of Geophysical Research: Solid Earth (1978–2012) 114 (B1).Google Scholar
Schumer, R., Jerolmack, D., McElroy, B., 2011. The stratigraphic filter and bias in measurement of geologic rates. Geophysical Research Letters 38 (11). http:// dx.doi.org/10.1029/2011GL047118.Google Scholar
Shevchenko, G., Ivelskaya, T., 2015. Estimation of extreme sea levels for the Russian coasts of the Kuril Islands and the Sea of Okhotsk. Pure and Applied Geophysics. http://dx.doi.org/10.1007/s00024-015-1077-y.Google Scholar
Shevchenko, G., Saveliev, V.Yu, 1999. Spatial variability of the wind field in the area of the Kuril Islands. In: Proceedings of the Second Workshop on the Okhotsk Sea and Adjacent Areas, 12, pp. 49–53. PICES Sci. Rep.Google Scholar
Soloviev, S.L., Ferchev, M.D., 1961. Summary of data on tsunamis in the USSR. Bulletin of the Council for Seismology 9, 1–37 (in Russian).Google Scholar
Song, T.A., Simons, M., 2003. Large trench-parallel gravity variations predict seismogenic behavior in subduction zones. Science 301, 630–633. http:// dx.doi.org/10.1126/science.1085557.Google Scholar
Sugawara, D., Imamura, F., Matsumoto, H., Goto, K., 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).Google Scholar
Szczuciński, W., Kokociński, M., Rzeszewski, M., Chagué-Goff, C., Cachão, M., Goto, K., Sugawara, D., 2012. Sediment sources and sedimentation processes of 2011 Tohoku-oki tsunami deposits on the Sendai Plain, JapaneInsights from diatoms, nannoliths and grain size distribution. Sedimentary Geology 282, 40–56. http://dx.doi.org/10.1016/j.sedgeo.2012.07.019.Google Scholar
Tanigawa, K., Sawai, Y., Shishikura, M., Namegaya, Y., Matsumoto, D., 2014. Geological evidence for an unusually large tsunami on the Pacific coast of Aomori, northern Japan. Journal of Quaternary Science 29 (2), 200–208.Google Scholar
Wiberg, P., 2000. A perfect storm: formation and potential for preservation of storm beds on the continental shelf. Oceanography 13 (3), 93–99. http://dx.doi.org/ 10.5670/oceanog.2000.18.Google Scholar
Witter, R.C., Kelsey, H.M., Hemphill-Haley, E., 2003. Great Cascadia earthquakes and tsunamis of the past 6700 years, Coquille River estuary, southern coastal Oregon. Geological Society of America Bulletin 115 (10), 1289–1306.Google Scholar
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