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sanriku japan tsunami 1933

http://www.dpbolvw.net/click-5028330-10426267 which used exclusively arrival times at Japanese stations. RESEARCH ARTICLE Open Access Paleo-tsunami history along the northern Japan Trench: evidence from Noda Village, northern Sanriku coast, Japan Taiga Inoue1*, Kazuhisa Goto2, Yuichi Nishimura3, Masashi Watanabe4, Yasutaka Iijima1,5 and Daisuke Sugawara2,6 Abstract Throughout history, large tsunamis have frequently affected the Sanriku area of the Pacific coast of the Tohoku Because of the steep-sloped valleys, alluvial deposits are … 2012), 1611 Keicho (Hatori 2009), 1896 Meiji Sanriku (Tanioka and Satake 1996; Tanioka and Seno 2001), 1933 Sanriku (Kanamori 1971), and 2011 Tohoku-oki earthquakes (Ozawa et al. The paper was improved through the comments of two anonymous reviewers. 昭和三陸地震, Shōwa Sanriku jishin) war ein Erdbeben, das sich am 2. From Wikimedia Commons, the free media repository. http://www.dpbolvw.net/click-5028330-10426267 Here you can help japan and change the world a little. The Sanriku region was the most affected area in Japan. N2 - After 83 yr, the great normal-faulting earthquake of 1933 March 2, which took place off the Japan Trench and produced a devastating tsunami on the Sanriku coast and damaging waves in Hawaii, remains the largest recorded normal-faulting earthquake. It was quite a different story with the 1933 event. Relocated aftershocks show a band of genuine shallow aftershocks parallel to the Japan Trench under the outer trench slope and a region of post-mainshock events landward of the trench axis that occur over roughly the same latitude range and are thought to be the result of stress transfer to the interplate thrust boundary following the normalfaulting rupture. 1933 Sanriku Earthquake damage at Onagawa.jpg 590 × 330; 91 KB Kamaishi Bay after 1933 tsunami.jpg 628 × 286; 65 KB The stone monuments for the 1933 Showa Sanriku tsunami and the 1960 Chile tsunami in Minami-Sanriku town -25-3-2011-.jpg 746 × 278; 40 KB 869 … ACKNOWLEDGEMENTS We are grateful to Hiroo Kanamori for sending us a preliminary write up of his solution for the moment of the 1933 earthquake, and to Naoki Uchida for collaboration and a data set of Uchida et al. The 1896 event with the same name and a greater magnitude, 8.5, occurred on a reverse fault, as an interplate event, instead of the normal pattern, and this resulted in less shaking and slower initial speed. Magnitude - Mw 8.4 We need to formulate future strategies for post-disaster recovery policy and planning based on the lessons of past disasters. The 1933 Sanriku earthquake (昭和三陸地震 Shōwa Sanriku Jishin?) keywords = "Earthquake source observations, Intra-plate processes, Tsunamis". The ground shaking was much more violent as the tsunami reached the shore about forty minutes after the earthquake. Its epicenter was ninety miles offshore, near an area of very deep water known as the Japan Trench, where the Pacific Plate subducts beneath the Asian Plate. 2011) are shown by colored lines off the Sanriku coast. In 1933, this town was hit again by the Showa Sanriku tsunami, and 911 people were killed. Japan is sinds 1933 nog vaker getroffen geweest door zware aardbevingen en tsunami's. The 1933 Sanriku-oki earthquake offshore northern Honshu, Japan (M w 8.4) is the largest earthquake that has recognized to date in the outer-rise/outer-trench-slope regions of the Earth. In some places the tsunami’s wave reached a height of 125 feet. Tsunamis können als integraler Bestandteil der Geschichte der Sanriku-Region betrachtet werden. Date and Origin Time - March 3, 1933 at 02:31 AM (Japan Standard Time); March 02 at 17:31 UTC . and Kirby, {Stephen H.} and Nikos Kalligeris". An almost identical event occurred in the same location in 1896, causing the deaths of more than 26,000 people. The paper was improved through the comments of two anonymous reviewers. The 1896 Sanriku earthquake was one of the most destructive seismic events in Japanese history. Based on a combination of P-wave first motions and inversion of surface wave spectral amplitudes, we propose a normal-faulting focal mechanism (φ = 200°, δ = 61° and λ= 271°) and a seismic moment M0 = (7 ± 1) × 1028 dyn cm (Mw = 8.5). This study emphasizes the need to include off-trench normal-faulting earthquake sources in global assessments of tsunami hazards emanating from the subduction of old and cold plates, whose total length of trenches exceed 20 000 km, even though only a handful of great such events are known with confidence in the instrumental record. Of 8.6 on the surface wave magnitude scale the 869 Jogan ( Sawai et.. 1933 event 26,000 people violent as the tsunami reached the shore about minutes! Author = `` the Showa Sanriku earthquake = `` earthquake source observations, Intra-plate processes, Tsunamis '' aardbevingen tsunami... 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