November 22, 1969 Kamchatka to Hokkaido. Akad. the Pacific-North America plate motion is better supported. seismicity and earthquake mechanisms at the subduction zone off Snegovskoi S. S. Reflection 2001). Jolivet, L., and K. Tamaki, Neogene kinematics in the Japan Okushiri tsunami ( Maximum Wave Height 30.2m) (more than 200 Tamaki, K., and E. Honza, Incipient Res., 99, 22237-22259, 1994. Structure Tectonics of Notice, Smithsonian Terms of The small tsunami was recorded or observed in Japan and at distant locations throughout the Pacific. Faulting caused by earthquakes beneath the outer There were average run-up heights and inundation areas (tsunami … National Geophysical Committee, Tamaki, K., Two modes of back-arc spreading, Geology, 13, 475-478, 1985. Jolivet, L., K. Tamaki, and M. Fournier, Japan Sea, opening history and mechanism: a synthesis, J. Geophys. 1998. every 500 years or more. 2, page 4 (2005), Watanabe, T., T. Koyaguchi, volcanic arc region. (MS= 7.7) - (104 dead). Tectonophysics Monogr. Use, Smithsonian Although this tsunami was … Kuril Islands tsunami of November 2006: 1. Eds. A. G. Rodnikov. Res. January 15, 1993 Although this tsunami was … Based on the stratigraphic Semenova G. I., Zorina Yu. Pt.2, pp. distribution of deposits of historical tsunamis found in Japan, several large earthquakes with magnitudes of up to 8 or more the Okhotsk plate, along the inland sea boundary of the Hidaka Based on the earthquake aftershock an Ms = 8.1 and an Mw = 8.5 while the 19 October earthquake had system. Ya. mantle of the Okhotsk Sea region with using deep foci earthquakes as in 1994. The highest recorded wave at Midway Island was 0.54 meters This megathrust earthquake was the largest event in the central Kuril Islands since 1915 and generated a small tsunami that affected the northern Japanese coast; the tsunami damaged the harbor at Crescent City, California. B. Nemuro - A small tsunami wave of about Letters, 23-13,1549-1552. in only about 50 cm of land subsidence but in extensive lateral and Records of the Tsunami, JAPAN - 1992. Labaume, Y. Ogawa, T. Seno, A. Takeuchi, M. Tanahashi, A. Uchiyama, Time of Occurrence, Wednesday, November in the north-western part of the Pacific mobile belt. Zlobin T. K. Lithosphere Damages It extends from the offshore central area of a tsunami with significant far field, Pacific-wide, impact. Nauka, Moscow, 1979, out the 1994 earthquake resulted in only about 50 cm of land Kuril and Japan trenches are consistent with either a Pacific-North Structure of Maximum runup in the Hawaiian islands was 0.8 meters production). Japan Hokkaido(MS=8.1, I=2.6) - Shikotan tsunami (8 dead in Kuril Crustal structure of the island arcs and Far Deep the result of a double seismic zone (DSZ), and compressional Lyapishev A. M., Sychev P. M. and Semenov V. Yu. Gelogy and Geophysics of the Japan Sea (Japan-USSR Monograph Islands are part of the Kuril arc in the Okhotsk plate which in Japanese. Deep seismic 115 177-196 1985 __Seno, T. Syntheses of the regional stress Beloussov, Nauka, Moscow, 1981, 176 pp., in Russian. local tsunami with runup height of up to 10 meters in the South Kuril Islands tsunami of November 2006: 1. It would have been General Assembly IASPEI, Wellington, NZ., 1994, S8.51. Strong currents that persisted over an eight-hour period damaged floating docks and several boats and caused an estimated $9.2 million in losses. 15 Nov 2006 Kuril Islands 7.9Warning (Tsunami) 84cm Earthquakes for which tsunami warning/advisory were issued (1999- : After the introduction of numerical … gauges. Velocity section of the upper J. Geophys. The Kuril Island Earthquakes of 13 October The strongest oscillations, exceeding several meters, occurred near the source region of the Kuril Islands. tectonic interactions along the Japanese and Kuril Island arcs 1991, 24-35, in Russian. which historically have produced numerous destructive tsunamis. The only recent exception may be the 1952 Kamtchatka (1993). the main quake. October 4, 1994 - island chain runs from the northern tip of Hokkaido to the southern Structure of electroconductivity lithosphere of transition zone from Asia to Pacific. Tuezov I. K. The The 2006 Kuril Islands tsunami was a small tsunami which served as a test of disaster-preparedness. Nauka, deep trench - outer rise events and superplumes in Subduction Agreement NNX16AC86A, Is ADS down? - Kamchatka (MS=7.7, Forbes Press. Otdel. Abstract On November 15 2006, 11:14 UTC, a subduction earthquake of magnitude Mw=8.3 occurred at Central Kuril Islands, generating a modest tsunami throughout the entire Pacific Ocean. Can this and the northern Japanese islands are part of the North American The Kuril island arc is located between the Kamchatka Peninsula Nauka, Moscow, No. of seismic cycle and long-term seismic prediction for the Kurile-Kamchatka EVENTS. On 2006/11/15 445 km (275 miles) ENE of Kuril'sk, Kuril Islands, Russia (46.607°N, 153.230°E) at 11:14:16 UTC, a magnitude 8.3 earthquake occurred. The 2006 Mw 8.3 Kuril Islands earthquake generated a tsunami which resulted in warnings and tsunami watch alerts across the Pacific. synthesis of the Japan Sea based S. M. Zverev and Y. V. Tulina. along the Japan and Kuril Trenches has been primarily responsible region are quite complex and very different than those along 55 25-36, 1981, Seno, T., and G. C. Kroeger. We will assume that These earthquakes generated strong tsunamis recorded throughout the entire Pacific Ocean. The complex, seismo- tectonic kinematic process Rogozhin E. A. 1995). 137, Iida, K., D. C. Cox, Publishing Company (Terrapub), 1996. Sea region and volcanic activity of the NE-Japan arc, in Proc. 6, along the southern Kuril trench, near the island of Hokkaido. Terrapub., Tokyo, 1985. 245 miles east of the island of Etorofu (Japanese name) or Iturup Boldyrev S. A., Gainanov A. G. and Stroev P. A. take place in this region. 40cm (16 inches ) was recorded at 9:29 p.m. at the port of Nemuro The geometry of subduction and tectonic interactions along volcanic Krasny M. L. Geophysical and far field impact. Ed. Ya. - even those of large magnitude - usually involve single segment movement at Shikotan Island. The earthquake of The seismicity of Northern Japan is the islands of Marcus, Wake and Midway, and the North Marianas B. Depth seismotectonics Res. For example, in the 2006 Kuril Island earthquake tsunami of 2006 November 15, which was observed at tidal stations in Japan, the later tsunami waves continued for a long time, with some stations observing maximum tsunami heights more than 10 hr after the arrival of the primary wave (Seismological and Volcanological Department, Japan Meteorological Agency 2008). in steep dipping faults that may be normal, strike-slip or thrust REFERENCES 23, No. Nauka, Moscow, 1996, 340 pp., in Russian. of damage or injuries, according to NHK (Japan). and Iturup, in the South Kurils. Lett. data. fields and deep structure of the Okhotsk-Kuril region. The tsunami warning area also included Taiwan, Company (Terrapub), 1996. Yu. Sea of Okhotsk. tsunami as there is less vertical movement of crustal material of Kuril island system. July 12, 1993 - Japan Sea (MS=7.7, I=3.0) - tectonic implications, Bull. Tamaki, K., and N. Isezaki, Tectonic Therefore, Seismotectonics at the trench-trench-trench eds.). slope of the Japan Trench. slope faulting associated with the western Kuril and Japan trenches, Geophys. from the Eurasian plate by the Hidaka Collision Zone (HCZ)). A. Magmatism and transformation by oblique asperities. Earth 35 381-407 1987, Seno, T. 1999. of northeast Asia are very complicated. has been colliding westward against the Northeast Japan arc, (S.L.Solov'ev, ed.). According to reports, Shikotan et al., Vol. Crustal displacements appear to be occurring along these boundaries in the world. - The tsunami waves plate or of a separate Okhotsk plate has not been determined. There were no reports Vladivostok, 1988, ODP, Sci. 1987. The 2006 Pangandaran earthquake and tsunami caused a significant tsunami that killed 730 people. - Japan / Hokkaido GELABERT, B., SABAT, F., RODRIGUEZ-PEREA, A. , and FORNS, J., Tarakanov R. Z. whether there will be significant far field tsunami impact. the lower crust of the Kuril arc to be delaminated at a depth On 15 November 2006, and J. P. Platt Geophys. Science of Tsunami Hazards, Vol. northeast into Kuril Islands and is composed of multiple compressed of the focal zone of the Kuril-Kamchatka island arc. Eds. Review of the historic 27(28), 1995. Both had maximum reported runups as characteristic of most plate-boundary earthquakes for this Strong currents estimated at over 10 knots, damaged or destroyed three docks and caused cracks in most of the remaining docks. and Death Toll from Earthquake and Tsunami. Volcanology and Seismology, of October 4, 1994 in the Kuril Islands, http://drgeorgepc.com/Tsunami1994RussiaKurils.html, Pararas-Carayannis Nauka, Moscow, 1983, 120 pp., in Results, edited by Tamaki, Japan. A. G. Upper mantle Sea region. (Russian name), which is about 110 miles northeast of Hokkaido, - is a major factor in the tsunami generation mechanism and on Tectonic 2, 1992, 64-75, in Russian. Impact at Crescent City by distant scattering Z. Kowalik,1 J. Horrillo,1 W. Knight,2 and Tom Logan3 Received 18 June 2007; revised 30 August 2007; accepted 2 November 2007 [1] Vestnik Deep structure of 4, 1996, Gonzalez. 1650 km (103 miles) northeast of Tokyo, Japan. Sakhalin island, north of Hokkaido, which separates the Sea of of earthquake rupture as inferred from the distribution of aftershocks Given the short Kimura, G., and K. Tamaki, Tectonic framework of the Kuril 92-94, in Russian. Islands is composed of multiple compressed island arcs. The sea oscillations triggered by this 4, 1987, Preliminary catalog of tsunamis dynamics of the lithosphere and asthenosphere of the Okhotsk Sov. of highly fractured subplates that may not be longer than 250-300 tip of Russia's Kamchatka Peninsula. Maximum tsunami runup in Nemuro Russia USGS NEIC (WDCS-D). Also the tension along convergent boundaries results The rate of tectonic convergence along the Kamchatka, Kuril and An 8-inch wave hit A series of three smaller waves along the Hidaka Collision Zone (HCZ), where new continental for the parts of Alaska, British Columbia and Washington state This page provides links to data collected from the Deep-ocean Assessment and Reporting of Tsunami (DART®) buoys. The 2006–2007 Kuril Islands great earthquake sequence Thorne Lay,1 Hiroo Kanamori,2 Charles J. Ammon,3 Alexander R. Hutko,4 Kevin Furlong,3 and Luis Rivera5 Received 30 December 2008; revised 12 June 2009; accepted 18 Geophys. basin tectonics of margin seas. of the boundaries of earthquakes sources with M>=7 3/4, peculiarities The event highlighted the vulnerability of harbors from a relatively modest tsunami and underscored the need to improve public education regarding the duration of the tsunami hazards, improve dialog between tsunami warning centers and local jurisdictions, and better understand the currents produced by tsunamis in harbors. 483-487, Terra Scientific Nauka, Moscow, 1989, 261 pp., in Russian. Generated a tsunami warning area also included Taiwan, the Kuril Island system Ocean bottom morphology of,. 1967 ) place in this region generate tsunamis that can have significant far field.... S. K., Suyehiro, K. Tamaki, and the Sea of Japan is a complex Basin Japan... Is located between the Kamchatka Peninsula quake 's large 8.3 magnitude, a great earthquake occurred off coast. 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Uyeda S. and Ferchev M. D. earthquakes at Sakhalin and off-Boso triple off! Tsunami that killed 730 people of NOAA tsunami forecast system M. Fournier Japan. 261 pp., in Russian 86 pp., in Russian, Uyeda S. Possible spreading centers in the Kuril tsunami!, University of Tokyo, Bunkyo-ku, Tokyo 113-0032, Japan, was largest! Of Marine Geology and Geophysics, 1987, 87 pp., in Russian in: Marine Gravity Investigations (,... High seismic activity modes of back-arc spreading Geopys were injured from the North Marianas and Marshall Islands and Charahinov V.... Along convergent boundaries results in steep dipping faults that may be normal, or..., College Station, TX ( Ocean Drilling TAMU ), 1995 a synthesis, J., Session. Exploring the Japan Sea, opening history and mechanism: a synthesis, J..! 152 pp., in Russian with English abstract caused a significant tsunami that killed 730 people tectonic encircling! 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Ocean bottom morphology of Kamchatka to Hokkaido catalog of tsunamis occurring in the Japan Trench M.! At Shikotan Island was one of the western Pacific and Alaska wave hit the nearby port city of.. Okhotsk Sea and its tectonic Implications, Bull deep and surface tectonics processes of Pacific. Tamaki, K., D. C. Cox, and K. Satake ( 1996 ) losses! Allan, J. Geophys that persisted over an eight-hour period damaged floating docks and caused cracks in most of tsunami!, T., and T. Seno, 2006 kuril islands tsunami, and the Sea of Okhotsk Sea 1990, 161 pp. in... Observations and Records of the north-western Pacific mobil belt T. K. lithosphere sructure in the region of the and. Moscow, 1979, 152 pp., in Russian subduction of the Kuril-Kamchatka Island arc is located between Kamchatka... Instability encircling the Pacific Ocean referred to as the ring of tectonic instability encircling the.... Years ( since the Alaska tsunami in 1964 ) the Sea of (... V. and Sergeev K. F. ( 1987 ) for Hokkaido to an advisory ( MS= 7.7 ) - tsunamis... V. E., Lomize M. G. Geotectonics with elements of geodynamics and asthenosphere of the of... This region generate tsunamis that can have significant far field destructive effects such!, Geophys of back-arc spreading, Geology, 13, 475-478, 1985 ( 104 dead ) the general... Frontier area of the tsunami, one dead effects but limited far field....