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The tremors lasted for approximately 20 seconds. The focus of the earthquake was located 17 km beneath its epicenter, on the northern end of Awaji Island, 20 km away from the center of the city of Kobe. At least 5,000 people died as a result of this earthquake; about 4,600 of them were from Kobe. [7]
Nojima Fault (野島断層, Nojima Dansō) is a fault that was responsible for the Great Hanshin earthquake of 1995 (Kobe Quake). [1] It cuts across Awaji Island , Japan and it is a branch of the Japan Median Tectonic Line which runs the length of the southern half of Honshu island. [ 2 ]
The Great Hanshin-Awaji Earthquake Memorial Disaster Reduction and Human Renovation Institution (阪神・淡路大震災記念 人と防災未来センター) is the earthquake disaster memorial museum that located in Chūō-ku, Kobe (HAT Kobe), Hyōgo Prefecture in Japan.
An earthquake is what happens when the seismic energy from plates slipping past each other rattles the planet's surface. Those seismic waves are like ripples on a pond, the USGS said.
- On Jan. 16, 1995, an earthquake with a magnitude of 7.3 hit central Japan, devastating the western port city of Kobe. The worst earthquake to hit the country in 50 years killed more than 6,400 ...
About 55 earthquakes a day – 20,000 a year – are recorded by the National Earthquake Information Center.Most are tiny and barely noticed by people living where they happen. But some are strong ...
In 1995, this island was the epicenter of the Kobe earthquake, which killed over 5,502 people. The earthquake caused enormous damage around the northern part of the island, which experienced a severe earthquake with a seismic intensity 7. The earthquake has a seismic fault called Nojima Fault.
Although the effects of soil liquefaction have been long understood, engineers took more notice after the 1964 Alaska earthquake and 1964 Niigata earthquake. It was a major cause of the destruction produced in San Francisco's Marina District during the 1989 Loma Prieta earthquake, and in the Port of Kobe during the 1995 Great Hanshin earthquake.