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A massive tsunami, created by a powerful undersea earthquake, engulfing a residential area in Natori, Miyagi prefecture, northeastern Honshu, Japan, on march 11, 2011.

The suddenly horizontal and vertical advertise of the Pacific Plate, which has actually been gradually advancing under the Eurasian Plate close to Japan, displaced the water above and spawned a collection of highly disastrous tsunami waves. A tide measuring part 33 feet high inundated the coast and flooded components of the city of Sendai, including its airport and also the neighboring countryside. Follow to some reports, one tide penetrated part 6 miles (10 km) inland after causing the Natori River, i beg your pardon separates Sendai from the city of Natori come the south, come overflow. Damaging tsunami tide struck the coastlines of Iwate prefecture, just north that Miyagi prefecture, and also Fukushima, Ibaraki, and Chiba, the prefectures prolonging along the Pacific coast south that Miyagi. In addition to Sendai, other neighborhoods hard-hit by the tsunami consisted of Kamaishi and Miyako in Iwate; Ishinomaki, Kesennuma, and also Shiogama in Miyagi; and also Kitaibaraki and Hitachinaka in Ibaraki. As the floodwaters retreated back to the sea, they carried with them substantial quantities the debris, and also thousands of victims recorded in the deluge. Large stretches of land to be left submerged under seawater, an especially in lower-lying areas.


Review just how underwater earthquakes, volcanoes, or landslides have the right to generate tsunamis
John Rafferty, associate editor of planet sciences at Encyclopædia audioeditorfree.com, discussing tsunamis.
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The earthquake triggered tsunami warnings throughout the Pacific basin. The tsunami raced exterior from the epicentre in ~ speeds the approached about 500 mile (800 km) every hour. It produced waves 11 to 12 feet (3.3 to 3.6 metres) high along the shores of Kauai and also Hawaii in the Hawaiian islands chain and also 5-foot (1.5-metre) waves follow me the island that Shemya in the Aleutian islands chain. Several hours later 9-foot (2.7-metre) tsunami tide struck the coastlines of California and Oregon in north America. Finally, part 18 hours after the quake, waves about 1 foot (0.3 metre) high reached the coastline of Antarctica and caused a part of the Sulzberger ice Shelf come break turn off its outer edge.

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Map all set by the U.S. Nationwide Oceanic and Atmospheric administration depicting the tsunami wave elevation model because that the Pacific Ocean adhering to the in march 11, 2011, earthquake off Sendai, Japan.