The 1964 Niigata earthquake struck at 13:01 local time (04:01 UTC) on 16 June with a magnitude of either 7.5 or 7.6.wikipedia. Bhattacharya et al. The 1964 Niigata earthquake struck at 13:01 local time (04:01 UTC) on 16 June with a magnitude of either 7.5 or 7.6. Liquefaction can also contribute to slope failures and to fountains of sandy mud (sand volcanoes) in areas where there is loose saturated sand beneath a layer of more cohesive clay. The earthquake cau on “Collapse of Showa Bridge during 1964 Niigata Earthquake: A reappraisal on the failure mechanisms” Page 2 ABSTRACT Collapse of Showa Bridge during the 1964 Niigata earthquake has been, throughout the years, an iconic case study for demonstrating the devastating effects of liquefaction. The earthquake is important for understanding the seismic hazards along the Japan Sea coast and also for understanding the tectonic boundary between the Eurasian and North America plates. April 1, 1968: 7.5 M w: 0: 1968 Hyūga-nada earthquake: 1968年日向灘地震 Just better. The frequency curve of the Matsushiro (central Japan) earthquake swarm which began in August 1964 is analyzed from the point of view that earthquakes are fracturing events in the earth's crust.
65 Related Articles [filter] Soil liquefaction. 100% (1/1) liquefaction liquefy liquefied. Tectonophysics, 159: 109-119. 1964 Niigata earthquake. The 1964 Niigata earthquake (Ms 7.5) occurred off the Japan Sea coast of Honshu, Japan, with a 4 m tsunami that caused significant damage. The mechanism of the occurrence of the Matsushiro earthquake swarm in central Japan and its relation to the 1964 Niigata earthquake. The epicenter was on the continental shelf off the northwest coast of Honshu, Japan in Niigata Prefecture, about 50 kilometres (31 mi) north of the city of Niigata. Quite the same Wikipedia. A good example is the collapse of apartment buildings during the 1964 Niigata earthquake (M7.6) in Japan (Figure 11.22). June 16, 1964: 7.6 M w: 26: 1964 Niigata earthquake: 新潟地震: Niigata Jishin: 50 km north of Niigata: The earthquake caused widespread soil liquefaction in the city of Niigata, resulting in unusually high levels of damage to buildings for the felt intensity. Inertial forces during The earthquake caused liquefaction over large parts of the city.
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65 Related Articles [filter] Soil liquefaction. 100% (1/1) liquefaction liquefy liquefied. Tectonophysics, 159: 109-119. 1964 Niigata earthquake. The 1964 Niigata earthquake (Ms 7.5) occurred off the Japan Sea coast of Honshu, Japan, with a 4 m tsunami that caused significant damage. The mechanism of the occurrence of the Matsushiro earthquake swarm in central Japan and its relation to the 1964 Niigata earthquake. The epicenter was on the continental shelf off the northwest coast of Honshu, Japan in Niigata Prefecture, about 50 kilometres (31 mi) north of the city of Niigata. Quite the same Wikipedia. A good example is the collapse of apartment buildings during the 1964 Niigata earthquake (M7.6) in Japan (Figure 11.22). June 16, 1964: 7.6 M w: 26: 1964 Niigata earthquake: 新潟地震: Niigata Jishin: 50 km north of Niigata: The earthquake caused widespread soil liquefaction in the city of Niigata, resulting in unusually high levels of damage to buildings for the felt intensity. Inertial forces during The earthquake caused liquefaction over large parts of the city.
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