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This city of Sendai was 80 miles (128 km) from the epicentre of the March 11, magnitude 9.0, Japan Earthquake. The Japan earthquake was caused by the buildup of strain between the Eurasian plate and the Pacific plate. As the convection currents in the Mantle tried to move the crustal plates around, they were unable to move due to friction. Overtime, this is how strain was built up. The strain reaches its limit and then the plates suddenly move (destructive plate boundary). This action releases shock waves. These are what we feel in an earthquake. When the strain was released the Eurasian plate jolted/ slide upwards above the Pacific plate. This caused an upward wave to be formed. The water flowed in large circular waves which flowed in and out not reaching high land. But when enough strength in the water is gathered it can flow straight, like a wall of water. Now, with enough energy the water can flow over the land and travel as far as it can.

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Q: How far is Sendai from the epicentre of the 2011 earthquake?
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How far was the 2011 earthquake from japan's shore?

The epicenter for the magnitude 9.0 earthquake in Japan on March 11, 2011 was reported to be 129 kilometers (80 miles) off the east coast of the Oshika Peninsula, Tōhoku, near Sendai.


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The USGS reported that the quake shifted portions of northeastern Japan by as much as 2.4 m (7.9 ft) closer to North America and made portions of Japan's landmass wider than before. This was a result of the 9.0 magnitude earthquake on March 11, 2011.


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