[8] In the Nara Basin, the earthquake made the soil behave like a liquid. Earthquake. Tsunami simulation for the great 1707 Hoei, Japan, earthquake - NASA/ADS Based on recent findings of geodetic and geological investigations, we present a revised source-rupture model for the great 1707 Hoei earthquake that occurred in the Nankai Trough off southwestern Japan. Places like Shikoku, Honshu, and Kyushu were severely damaged. Location Date Magnitude 350,000 2004 9.0 Indian Ocean 100,000 1410 b.c. Nankaido japan 28 october 1707 a magnitude 84. 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It took place on the Eurasian plate, which is near the Philippine sea plate, both being transform faults. Tsunami Facts in Wake of Japan Earthquake Learn how the killer waves are formed. Location: Nankaido, Japan Year: 1707 On 28th October, a magnitude 8.4 earthquake caused sea waves as high as 25 metres to hit the coasts of Kyushyu, Shikoku and Honshin. The tsunami height increased by 0.1–0.4 m compared to that estimated by the Hoei earthquake. of Deaths, as follows: Background. [5] In 1707, the earthquakes were either at the same time, or close enough together so that writing from that time do not describe them separately. [6] This landslide was one of the three largest in Japan and is called the Ohya Landslide. [6] In 1707, the earthquakes were either at the same time, or close enough together so that writing from that time do not describe them separately. [7] In the Nara Basin, the earthquake made the soil behave like a liquid. The Nankai megathrust has five parts (A-E) that can break one by one. Indian Ocean Tsunami: The Deadliest in History. The area is convergent, or the plates were running into each other. Damage [ edit ] The earthquake caused more than 5,000 casualties, destroyed 29,000 houses, and triggered at least one major landslide , the Ohya slide in Shizuoka . It caused a consequent tsunami that led to the sea waves as high as 25 m to hammer into the Pacific coasts of Kyushu, Shikoku, and Honshin. Séisme de 1707 de l'ère Hōei: Date 28 octobre 1707 à 14 h 00 (heure locale) Magnitude: 8,6 (estimée) Épicentre: 33° 12′ 00″ nord, 135° 54′ 00″ est: Hauteur maximale du tsunami 25,7 m: Régions affectées Honshu, Kyushu, Shikoku: Victimes 5 000 Géolocalisation sur la carte : océan Pacifique. From Simple English Wikipedia, the free encyclopedia, "Catalog of Damaging Earthquakes in the World (Through 2007)", "Source mechanisms and tectonic significance of historical earthquakes along the nankai trough, Japan", "Status of historical seismology in Japan", "Precise real-time observatory and simulating phenomena of earthquakes and tsunamis around the Nankai Trough - Towards the understanding of mega thrust earthquakes", "Triggering Mechanisms of Landslides and Debris Flows and Their Linkages: Hydrogeomorphic and Hydropedologic Influences", "Liquefaction Caused by the 1707 Hoei Earthquake as Observed in the Nara Basin, Central Japan", "The 1707 Hoei Earthquake, as an Example of a combined Gigantic Tokai-Nankai Earthquake", "Field investigations of the Nankaido Tsunamis in 1707 and 1854 along the South-west coast of Shikoku", https://simple.wikipedia.org/w/index.php?title=1707_Hōei_earthquake&oldid=7090014, Creative Commons Attribution/Share-Alike License. Along the southwestern coast of Kōchi, the average increase in sea level was 7.7 m. In some places it rose up to 10.2 m[11]. There are also records of tsunami at distant locations, such as Nagasaki and Jeju-do, South Korea. Changes in stress caused by large earthquakes may be enough to cause volcanic eruptions, when the magma system of the volcano is close to a critical state. It was a hot afternoon when an 8.4 magnitude earthquake sent sea waves at a height of 25 meters to hammer parts of Japan. Japan was hit by a 9.0 magnitude earthquake on March 11, 2011, that triggered a deadly 23-foot tsunami in the country's north. ; Pollitz F. & Newhall C. (2002). This marks the place where the Philippine Sea Plate moves under the Eurasian Plate. 8 - Nankaido earthquake, 1946. At Shirahama the waves reached a height of 38.2 m damaging more than 11thousand … Difference between Tidal Wave and Tsunami (CSS-2018) A tidal wave is essentially a high tide that rises fast enough to appear in the form of a wave. 7. Tsunamis in Japan Bei insgesamt 141 als Tsunami eingestuften Flutwellen seit 684 kamen in Japan insgesamt 130.974 Menschen ums Leben. Keywords: The 1707 Hoei earthquake, Tsunamis in Korea, Nankai earthquake tsunamis 29,000 houses were destroyed and more than 5,000 people were killed. The 1946 Nankai earthquake (昭和南海地震 Shōwa Nankai jishin) was a great earthquake in Nankaidō, Japan. The waves of the tsunami extended several kilometers inland and as many as a dozen occurred over a one hour period. 1707 Hōei earthquake Date October 28 1707 () Magnitude 8.6 M L: Epicenter location 33°00′N 136°00′E  /  33.0°N 136.0°E  / Coordinates: 33°00′N 136°00′E  /  33.0°N 136.0°E  / Countries or regions affected Japan: Chūbu region, Kansai region, Shikoku, Kyūshū: Tsunami yes Casualties >5,000 All probably killed in excess of 10,000 people, though the historical records are not completely reliable. In the 1707 event, the earthquakes were either simultaneous, or close enough in time to not be distinguished by historical sources. It caused moderate to severe damage throughout southwestern Honshu, Shikoku and southeastern Kyūshū. The Worst Tsunami in History! The affected areas were Kyushu, Shikoku, Honshin, and Osaka. Nankaido, Japan - 28 October 1707. This page was last changed on 31 August 2020, at 16:15. Image Credit: chajarivirtual The Tsunami waves hit as high as 25m after an earthquake of magnitude 8.4 hit Japan. [1] The earthquake measured between 8.1 and 8.4 on the moment magnitude scale , … A total of 30,000 people died as a result of the tsunami. Nankaido Japan 28 October 1707 A magnitude 84 earthquake caused tsunamis as. Type: Tsunami Earthquake Casualties: 30,000 Location: Honshu, Shikoku, and Kyushu Date: October 28, 1707. Tokaido-Nankaido, Japan Tsunami – A earthquake of 8.4 magnitude which caused 25 meter waves to engulf the coastal regions of Kyushyu, Shikoku, Honshin and Osaka in 1707. Japan: Chūbu region, Kansai region, Shikoku, Kyūshū: Tsunami: yes: Casualties >5,000: The 1707 Hōei earthquake happened at 14:00 local time on 28 October 1707. Thousands were killed as a result of both the earthquake and tsunami and many more were displaced. A total of nearly 30,000 buildings were damaged in the affected regions and about 30,000 people were killed. Circles represent observed 1707 tsunami inundation heights (Hatori, 1974, 1985; Murakami et al., 1995; black if the discrepancy between modeled and observed tsunami heights is <25% of the observed height, and red if not). The powerful quake generated a massive tsunami that stood 25 meters tall and hit the coasts of Kyushu, Shikoku, and Honshin. [10], The tsunami that followed the earthquake raised water along the coast. Video footage showed cars racing away from surging waves. Each time, the northeastern part broke before the southwestern part. The 1707 Hōei earthquake, which occurred at 14:00 local time on October 28, 1707, was the largest earthquake in Japanese history until the 2011 Tōhoku earthquake surpassed it.It caused moderate to severe damage throughout southwestern Honshu, Shikoku and southeastern Kyūshū. A magnitude 8.4 earthquake produced 25m high sea waves that rushed towards the cities. It was the largest earthquake in Japanese history. It had a magnitude estimated at 8.6 Ms and triggered a large tsunami. [12] The great earthquake in 1707 may have changed pressure in the magma under Mount Fuji. Tsunamis therefore occur comparatively often in this country. On December 20, 1946, while Japan was recovering from all the devastation of World War II, it was hit once again with the Nankaido earthquake, a very powerful one of magnitude 8.1, along this line. Nankaido, Japan, 1707 – next on our list is another tsunami that hit Japan hundreds of years ago. Tsunami in Japan Japan was hit by a 9.0 magnitude earthquake on March 11, 2011, that triggered a deadly 23-foot tsunami in the country's north. 7. Several observations show that the Hōei earthquake was bigger. The casualty and damage caused by them are beyond repair a… A total of nearly 30,000 buildings were damaged in the affected regions and about 30,000 people were killed. [11] It was reported that roughly a dozen large waves were counted between 3 pm and 4 pm, some of them extending several kilometres inland at Kochi. Many thousands of Japanese have been killed by them in recent centuries. The earthquake and tsunami happened on October 28, 1707 in Tokaido - Nankaido, Japan. Par exemple, le 11 Mars 2011, le Japon a été frappé par une magnitude 9,0 tremblement de terre qui a été centré dans l’océan 80 miles (130 km) à l’ est de la ville de Sendai. The 1707 Hōei earthquake happened at 14:00 local time on 28 October 1707. Movement on this boundary causes many earthquakes; some of them are megathrust earthquakes. Some content of the original page may have been edited to make it more suitable for younger readers, unless otherwise noted. The earthquake was felt from Northern Honshu Japan… Content is available under the Creative Commons Attribution-ShareAlike License; additional terms may apply. The earthquake, and the resulting destructive tsunami, caused more than 5,000 casualties.