Kobe, Japan (Case Study)

Authors Avatar

Matt Bodell 9R                 Geography Mr. Willis

Kobe, Japan

(Case Study)

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, and it was sudden movement along this fault that triggered the earthquake that hit Kobe.

 Kobe is located farther than many other cities in Japan from the dangerous intersection of three : the Pacific, Eurasian, and Philippine. This triple junction is a junction of three compressive subduction zones. There had been a subduction fault that had already been broken in great earthquakes in 1944 and 1946. Kobe is also somewhat off the Median Tectonic Line, a zone of strike-slip faults.

Join now!

 

At 5.46am on January 17th 1995, whilst many of its people of Kobe were still asleep, the Japanese city of was hit by the largest earthquake in Japan since 1923. The earthquake was not only powerful (Richter scale 6.9 ), but with the epicenter 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 ...

This is a preview of the whole essay