The Kobe earthquake of 1995
Kobe is a heavily populated urban area. It is here that disaster struck in 1995 when an earthquake of magnitude 7.2 hit the area. It was a major disaster in a MEDC where the modern buildings had been earthquake proofed. Many of the city’s residents had been unaware of the chances of an earthquake taking place.
The epicentre of the earthquake was located on the island of Awaji at 34.6 N 135.0 E. The earthquake had taken place because of a subduction zone on the plate margin. The type of margin where the Philippine plate and the Eurasian plate meet is a destructive margin. This means that the Philippine plate (Oceanic plate) moved under the Eurasian plate (continental plate) causing uplifting and folding of the ground that the plate was on. The ground moved 7 inches in horizontal shaking in this earthquake, and 4 inches in the vertical direction. This is the greatest recording of plate movement in Japan. The ground movement was even greater in Awaji Island where the ground moved 5 feet 7 inches (170 cm), with a vertical slip of 4 feet 3 inches (130 cm).