The occurred on the Sanriku coast of the Tōhoku region of Honshū, Japan on March 2 with a moment magnitude of 8.4. The associated tsunami caused widespread devastation.
Earthquake The epicenter was located offshore, 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. 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. Approximately three hours after the main shock there was a magnitude 6.8 aftershock, followed by 76 more aftershocks (with a magnitude of 5.0 or greater) over a period of six months.The Meiji Sanriku Earthquake (June 15, 1896, M 8 1/2) and Sanriku Earthquake (March 3, 1933, M 8.1) This was an intraplate event that occurred within the Pacific plate,"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 and the focal mechanism showed normal faulting.
Damage Although little damage was produced from the shock, the tsunami, which was recorded to reach the height of at Ōfunato, Iwate, caused extensive damage, and destroyed many homes and caused numerous casualties.Masayuki Nakao, "The Great Meiji Sanriku Tsunami". Association for the Study of Failure The tsunami destroyed over 7,000 homes along the northern Japanese coastline, of which over 4,885 were washed away. The tsunami was also recorded in Hawaii with a height of , and also resulted in slight damage. The death toll came to 1,522 people confirmed dead, 1,542 missing, and 12,053 injured. Hardest hit was the town of Tarō, Iwate (now part of Miyako city), with 98% of its houses destroyed and 42% of its population killed.Corkill, Edan, "Heights of survival", Japan Times, 12 June 2011, pp. 9–10.
See also List of earthquakes in 1933 List of earthquakes in Japan Seismicity of the Sanriku coast
Notes
External links Historic video footage of devastation following 1933 Sanriku Earthquake