1933 sanriku earthquake

George Pararas-Carayannis. Sanriku earthquake, 1933. 1 INTRODUCTION. Définitions de 1933_Sanriku_earthquake, synonymes, antonymes, dérivés de 1933_Sanriku_earthquake, dictionnaire analogique de 1933_Sanriku_earthquake (anglais) Therefore, the tsunami are referred to separately as the Meiji Sanriku Earthquake Tsunami and the Sanriku Earthquake Tsunami. Dezember 1956 veröffentlicht oder vor 1946 aufgenommen und danach 10 … 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. That earthquake produced 76 aftershocks with magnitude 5 or higher. User reports for this quake. (1)The Meiji Sanriku Earthquake (June 15, 1896, M 8 1/2) and Sanriku Earthquake (March 3, 1933, M 8.1) Both earthquakes generated the tsunami that caused enormous damage. The P wave fault plane solution, the amplitude of long-period (100 s) Love and Rayleigh … The earthquake from March 2, 1933, led to many damages and 3000 victims. A static dislocation model of the Sanriku earthquake of 1933 is proposed which is consistent with the initial motion of the tsunami. Javascript is required to view shouts on this page. It happened too far off-shore to be dangerous but the afterward tsunami turned into something lethal. 1933-03-02 17:31:00 (UTC) 39.209°N 144.590°E; 15.0 km depth; Official Magnitude updated 07-Nov-2016 Reference: Kanamori, H. (1971). 昭和三陸地震, Shōwa Sanriku jishin) war ein Erdbeben, das sich am 2.März 1933 (Shōwa 8) 290 km östlich von Japan ereignete.Es folgte ein Tsunami mit einer Wellenhöhe bis 28,7 m, der die Sanriku-Küste traf. The 1933 Sanriku earthquake (昭和三陸地震, Shōwa Sanriku Jishin) occurred on the Sanriku coast of the Tōhoku region of Honshū, Japan on March 2 with a moment magnitude of 8.4. Metrics details. The 1933 Sanriku-oki earthquake offshore northern Honshu, Japan (Mw 8. Seismological evidence for a lithospheric normal faulting—The Sanriku earthquake of 1933. Distribution of first motion polarities of the Showa Sanriku earthquake. Figure 8. A great earthquake occurred on March 2, 1933 (UTC DATE) in the Sanriku region of Japan and generated a destructive tsunami that caused extensive damage along the Sanriku coast of the Tohoku region of the island of Honshu. 295 Accesses. 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 Ground shaking was felt with intensities of 4 to 5 in a wide area of eastern Japan, not only in Tohoku but also in the Kanto region to the south. The song was inspired by Max Miller's 1932 best-selling novel I Cover the Waterfront. Physics of the Earth and Planetary Interiors, 4(4), 289-300. The wave equations of a tsunami were solved numerically on the displacement fields for various fault parameters and the computed time histories of the water surface elevation at the coast were compared with the observed initial motions. Meiji-Sanriku earthquake, 1896 (Magnitude 8.5) Another devastating earthquake that took the lives of over 27,000 people. INTRODUCTION. JAPAN - EARTHQUAKE AND TSUNAMI OF 3 MARCH 1933 IN SANRIKU. In 1933, Japan was shacked by a strong earthquake, with a 8.5 Richter power. The 1933 Showa Sanriku earthquake is con-sideredtohavebeenanouter-riseearthquake, the rupture of a normal fault in the oceanic plate entering the Japan Trench. An 8.4 magnitude earthquake on March 2, 1933 triggered a tsunami which caused widespread damage to towns on the Sanriku coast of the Tohoku region of Honshu. The 1933 Sanriku earthquake (昭和三陸地震, Shōwa Sanriku Jishin) occurred on the Sanriku coast of the Tōhoku region of Honshū, Japan on March 2 with a moment magnitude of 8.4. 0 Altmetric. 1933 Sanriku (Sanriku-oki) Earthquake, Japan: USGS: Note: for quakes of 2012 and earlier, our database often contains only records from USGS. More than 3,000 people were killed. Se vi volas enigi tiun artikolon en la originalan Esperanto-Vikipedion, vi povas uzi nian specialan redakt-interfacon. The associated tsunami caused widespread damage. ^ a b "Historical Earthquakes:The 1933 Sanriku earthquake". 4) is the largest earthquake that has recogniz ed to date in the outer-rise/outer-trench- slope regions of the Earth. Earthquake []. While the powerful quake struck about 180 miles offshore, the tsunami it triggered was strong enough to wash away around 3,000 homes. La ĉi-suba teksto estas aŭtomata traduko de la artikolo 1933 Sanriku earthquake article en la angla Vikipedio, farita per la sistemo GramTrans on 2015-09-20 07:11:20. The epicenter was located offshore, 290 kilometres (180 mi) east of the city of Kamaishi, Iwate.The main shock occurred at 02:31 AM local time on March 3, 1933 (17:31 UTC March 2, 1933) and measured 8.4 on the moment magnitude scale. The 2003 Hokkaidō earthquake, scientifically named the 2003 Tokachi-Oki earthquake (十勝沖地震, 2003 Tokachi-Oki Jishin), occurred off the coast of Hokkaidō, Japan on 26 September at 04:50 local time (19:50 UTC 25 September). Kamaishi Bay, Iwate, Japan after 1933 Sanriku earthquake: Datum: 1933: Quelle: Iwate Prefectural government: Urheber: Autor unbekannt: Genehmigung (Weiternutzung dieser Datei) Public domain Public domain false false: Dieses fotografische Werk wurde im Zuständigkeitsbereich der Regierung von Japan entweder vor dem 31. Contributed by OFFICIAL 3 ISCGEM ; Regional Information . Interactive Map. User reports estimate the perceived ground shaking intensity according to the MMI (Modified Mercalli Intensity) scale. Most recent quakes Top 20 quakes past 24 hrs Quakes in Japan. The 1933 Sanriku earthquake (昭和三陸地震, Shōwa Sanriku Jishin) occurred on the Sanriku coast of the Tōhoku region of Honshū, Japan on March 2 with a moment magnitude of 8.4. On June 15, 1896, an earthquake of magnitude 8.5 struck the Sanriku coast on the northeast of Honshu, Japan, in the Iwate Prefecture. The 2011 Tohoku earthquake generated a huge, destructive tsunami with coastal heights of up to 40 m recorded along northern Honshu. Abstract. In Japan wurden etwa 3000 Häuser komplett zerstört und weitere 2000 wurden beschädigt. Tsunamis generated by both earthquakes caused severe damage along the Sanriku coast. Ground shak-ing was felt with intensities of 4 to 5 in a wide area of eastern Japan, not only in Tohoku but also in the Kanto region to the south. 1). The blue line reproduces his nodal line (Knotenlinie), separating compressional and dilatational arrivals under his conical model. which used exclusively arrival times at Japanese stations. The 869 Sanriku earthquake (貞観地震, Jōgan jishin) and associated tsunami struck the area around Sendai in the northern part of Honshu on 9 July 869 (26th day of 5th month, 11th year of Jōgan). The Sanriku region was the most affected area in Japan. On the basis of the P times obtained at more than 200 stations, it is confirmed that the hypocenter of this earthquake is within the lithosphere beneath the Japan trench. The 1933 Showa Sanriku earthquake is considered to have been an outer-rise earthquake, the rupture of a normal fault in the oceanic plate entering the Japan Trench. The associated tsunami caused widespread damage.. Earthquake. ^ title ^ "日本海溝・千島海溝周辺海溝型地震に関する専門調査会報告" by 日本海溝・千島海溝周辺海溝型地震に関する専門調査会 ^ "Outer trench-slope faulting and the 2011 M w 9.0 off the Pacific coast of Tohoku Earthquake" by T. Lay, C. J. Ammon, H. Kanamori, M. J. Kim, and L. Xue The ground shaking at Sanriku coast about 300 km to the west of this source was not so large, but the rupture caused a huge tsunami that led to about 3000 deaths (The Central Meteorological Observatory 1933 ). Its epicenter was ninety miles offshore, near an area of very deep water known as the Japan Trench. Eventualaj ŝanĝoj en la angla originalo estos kaptitaj per regulaj retradukoj. Waves up to 94ft were reported at … The Sanriku coast experienced similar tsunamis and damage from the 1896 and 1933 Sanriku earthquakes, whereas the only damaging tsunamis on both the Ibaraki and Chiba coasts in the previous century were from the 1960 and 2010 Chile earthquakes. The Sanriku (Japan) Earthquake Seawaves of 1933. The people remained with no homes, security and protection. The focal process of the Sanriku earthquake of March 2, 1933, is discussed in relation to the bending mechanism of the lithosphere. It is in this context that we present here a modern seismological reassessment of the 1933 Showa Sanriku earthquake. The strong power of the earthquake caused a tsunami with almost 30 m height. This Mercator projection complements Matuzawas (1942; fig. In 1933, an 8.4 magnitude earthquake triggered a tsunami, causing widespread damage to towns on the Sanriku coast of the Tohoku region of … Das Shōwa-Sanriku-Erdbeben (jap. It was in approximately the same location as the 1896 Sanriku earthquake and it occurred far enough away from the town that shaking did little damage. 5 - Sanriku earthquake, 1933. I Cover The Waterfront Lyrics: I cover the waterfront / I'm watching the sea / Will the one I love be coming back to me? 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