Kobe Earthquake, Japan

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CASE STUDY – Kobe Earthquake, Japan

Japan is positioned on the margin of the Eurasian Plate.  Where these plates meet it is known as a subduction zone, where effectively one plate slides under the other.  Along these subduction zones there are both deep and shallow earthquakes that occur due to the compressive forces against the meeting of the plates.  Kobe lies in a region where the Philippine Sea Plate is thrust under the Eurasian Plate (See picture below)

At Osaka Bay there is a fault called the Median Tectonic Line (MTL), and it was sudden movement along this fault that triggered the earthquake that hit Kobe.

The earthquake happened early morning 5:45am JST January 17 1995, the epicentre was at Akachi.  It was 7.2 on the Richter scale; this earthquake was a national catastrophe.  Kobe has 1.5 million residents and is the worlds 6th largest city and port.

Impacts of the Earthquake : 

Surface Fault Rupture: It was noticed that along the fault that there was a maximum vertical displacement of 1.2m with a right-lateral slip of 2.1m.  The surface fault rupture was found to stretch over 60km from the Kobe-Nishinomiya area to the Akashi Strait.  The earthquake also had a shaking intensity of X to XI on the Mercalli scale and had a maximum horizontal acceleration of 0.84g.

Liquefaction:  This is the result of water saturated sands found in soil being disturbed by intense shaking.  This leads to buildings collapsing and for sand to 'explode' onto the surface to create 'sand volcanoes' and 'boils'.  In Kobe the effects of liquefaction were felt primarily along the waterfront although the effects were found as far as 3km inland.  Parts of Kobe were built on reclaimed land as well as artificial islands.  These were constructed using various sands as well as decomposed granite.  Due to the nature of these materials it is made very easy for liquefaction to take place if it was not compacted well enough. 

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Lateral spreading was found to be responsible for the lateral ground movement of 2-3m in the region resulting in structural damage especially to the port side buildings and walls.  The damage inflicted by this resulted in the majority of the port shutting down

Primary effects:

  • Violent shaking of the earth and buildings for 20 seconds
  • 1320 aftershocks were recorded, of which 150 were felt by people
  • Over 5500 people killed and 35000 injured
  • Nearly 7500 houses were destroyed by fired which rages out of control for several days.  
  • Gas mains fractured, electricity cut off, many fires started. Almost ...

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