Immediately south of Osaka Bay is a fault called the Median Tectonic Line ( MTL) , and it was sudden movement along this fault that triggered the earthquake that hit Kobe. At 5.46am on January 17th 1995, whilst many of its citizens were still asleep

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The Kobe Earthquake

Introduction 

Japan is positioned on the margin of the Eurasian Plate. The Philippine Sea Plate is subducted below the Eurasian plate, resulting in Japan having greater than average seismic and volcanic activity. Immediately south of Osaka Bay is a fault called the Median Tectonic Line ( MTL) , and it was sudden movement along this fault that triggered the earthquake that hit Kobe.

At 5.46am on January 17th 1995, whilst many of its citizens were still asleep, the Japanese city of Kobe was hit by largest earthquake in Japan since 1923. The Hyogo-ken Nanbu earthquake was not only powerful ( magnitude 6.9 ), but with the epicentre only 20km southwest of the city, it resulted in massive damage to property and loss of life. The worst effected area was in the central part of Kobe, a region about 5km by 20km alongside the main docks and port area. This area is built on soft and easily moved rocks, especially the port itself which is built on reclaimed ground. Here the ground actually liquefied and acted like thick soup, allowing buildings to topple sideways, resulting in the huge cranes in the harbour toppling over into the sea.

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Large earthquakes in remote, uninhabited areas can do relatively little damage to the human population, but when they strike in places like the Kobe / Osaka region with a population of 10 million people, the damage levels will always be significant. More than 102,000 buildings were destroyed in Kobe, leaving over a fifth of the city population, some 300, 000 people, homeless. The local government's estimate of the cost to restore the basic infrastructure of the city was about $150 billion dollars, and that was just for the state owned buildings and services. When all the costs are added up, ...

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