Its epicenter was ninety miles offshore, near an area of very deep water known as the Japan Trench. It occurred along the Japan Trench in the northern tsunami source area of the 2011 Tohoku earthquake where a delayed tsunami generation has been proposed. The governmental agencies dispatched inspectors and the army sent medical specialists. More than 1,000 people were killed in the Sanriku region in 1933 by another massive earthquake and tsunami. The associated tsunami caused widespread damage. After a small earthquake, there was little concern because it was so weak and many small tremors had also been felt in the previous few months. The 1896 Sanriku earthquake was a typical ‘tsunami earthquake’ which caused large tsunami despite its weak ground shaking. The earthquake lasted for five minutes and was accompanied by a slow shaking.Many villagers were at the beach celebrating two events when the earthquake occurred: the return of soldiers from a successful war with China, the first Sino-Japanese War of 1894, and the annual Boys’ Festival. On June 15, 1896, an earthquake of magnitude 8.5 struck the Sanriku coast on the northeast of Honshu, Japan, in the Iwate Prefecture. Photo 1 is the press photo of the catastrophic tsunami.

The impact on shore was much weaker than would normally be expected from such a powerful earthquake so there was little expectation of a tsunami, even though this part of the Japanese coast experiences earthquakes frequently. The 8.5 magnitude earthquake occurred at … At the same time it pointed out that a loud noise like thunder might indicate an approaching tsunami. On the evening of June 15, 1896, communities along the Sanriku coast in northern Japan were celebrating a Shinto holiday and the return of soldiers from the First Sino-Japanese War. Other things listed in the booklet included avoiding the recession of the tsunami’s first wave and being prepared to evacuate the coast quickly and move to higher ground. Usually victims in tsunami disasters die by drowning but, in the Sanriku tsunami, there was extensive damage to the bodies of victims; fractured skulls, bodies heavily scarred, and legs and arms broken. There were also reports of unusual phenomenon on that same day—low water levels in wells and large numbers of tunas every day.

However 35 minutes later the first tsunami wave struck the coast, followed by a second a few minutes later. The June 15, 1896 Sanriku earthquake generated devastating tsunamis with the maximum run‐up of 25 m and caused the worst tsunami disaster in the history of Japan, despite its moderate surface wave magnitude (M s =7.2) and weak seismic intensity. Seismologists have discovered the The epicenter lies just to the west of the The unusual disparity between the magnitude of the earthquake and the subsequent tsunami may be due to a combination of forces:Scientists believe the effect of subducted sediment beneath the On the evening of June 15, 1896, communities along the The power of the tsunami was great: large numbers of victims were found with broken bodies or missing limbs.Wave heights of up to 9 meters (30 ft) were also measured in Preventive coastal measures were not implemented until after another tsunami struck in 1933.

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