The Kobe Earthquake

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The Kobe Earthquake

Japan is situated where four of the Earth’s plates meet – the Eurasian and North American Plates to the north, and the Philippine and the Pacific Plates to the south.  Therefore it is not surprising that the islands have many volcanoes and suffer 1,000 earthquakes  every year.  Most of the quakes are quite mild, but in 1995, to the very south of the island, about 440 km from Tokyo, there was a massive quake.  The industrial port of Kobe suffered the worst damage with collapsing buildings and ruptured gas mains bursting into flames all over the city.  Many of the city’s newer buildings survived, however, because they had been built with quakes in mind.

Plate Tectonics

The Kobe earthquake disaster occurred because of the effects of plate tectonics.  

Plate tectonics are a theory of geology which looks at the earth and the underlying continental drift.  This theory suggests that the earth’s outermost surface is made up of two sub layers, the rigid litosphere and the semi-molten asthenosphere.

Tectonic plates are roughly divided into two types: continental and oceanic plates. How they are divided is by the thickness of the plates; oceanic plates are thinner than continental plates, this is why the oceanic plates generally lie below sea level, while the continental plate’s project above sea level.

The boundaries between plates are known as fault lines. Individual faults are regions where two plate sections are moving with respect to one another.  There are three movements at these fault lines: together, apart and side to side.  Pressure builds up along these regions as the plates are drawn in different directions by the underlying currents (convection currents); when the direct motion of the plate’s releases the pressure, earthquake results.



In some areas one plate will begin to overrun another. The plate being overrun will have its edge pressed downward below the leading edge of the other plate. This process, called subjection, which results in the edge of this plate being exposed to the greater pressures and temperatures within the asthenosphere, and the rock

making it up may begin to liquefy.

                                                 


Description of the Kobe Earthquake

                                     

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

On Tuesday, January 17,1995 at 5:46 a.m. local time, an earthquake of magnitude 7.2 struck the region of Kobe and Osaka in south central Japan. This region is Japan’s second-most populated and developed area, after Tokyo, with a total population of about 10 million. The shock occurred at a shallow depth on a fault running from Awaji Island through the city of Kobe, which has a population of about 1.5 million. Strong ground shaking lasted for about 20 seconds and caused severe damage over a large area.

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There were nearly 5,500 deaths with about 35,000 injured people.  Nearly 180,000 buildings were badly damaged or destroyed, and officials estimate that more than 300,000 people were homeless on the night of the earthquake.

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 melted and acted like thick soup, allowing buildings to collapse, resulting in the huge cranes ...

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