Seismicity of the Sanriku Coast
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The seismicity of the Sanriku coast identifies and describes the seismic activity of an area of Japan. Seismicity refers to the frequency, type and size of earthquakes experienced over a period of time. The Sanriku coast is a descriptive term referring to Mutsu in Aomori, Rikuch in Aomori and Rikuzen in Miyagi. The irregular coastline and its many bays tend to amplify the destructiveness of tsunami waves which reach the shores of Sanriku, as demonstrated in the damage caused by the 2011 T hoku earthquake and tsunami.

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Produktbeschreibung
The seismicity of the Sanriku coast identifies and describes the seismic activity of an area of Japan. Seismicity refers to the frequency, type and size of earthquakes experienced over a period of time. The Sanriku coast is a descriptive term referring to Mutsu in Aomori, Rikuch in Aomori and Rikuzen in Miyagi. The irregular coastline and its many bays tend to amplify the destructiveness of tsunami waves which reach the shores of Sanriku, as demonstrated in the damage caused by the 2011 T hoku earthquake and tsunami.