Kobe Earthquake 1995
Earthquakes are natural hazards, which occur on plate margins. Earthquakes are the result of plate movements. The strain builds up along the fault line between two plates until they move causing earthquakes.So why did the Kobe earthquake happen? Japan is at a high risk to earthquakes. Kobe is no exception. Japan’s second most major port is situated on a minor fault, the Nojma Fault. Unfortunately it lies above a destructive plate margin. Kobe is located above where the Philippines crust (oceanic crust) and the Eurasion crust (continental crust) meet. It was along this fault that the 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 the largest earthquake in Japan since 1923. It was recorded at 7.2 on the Richter scale and lasted for 20 seconds. During this time the ground moved 18cm horizontally and 12cm vertically. The earthquake was not only powerful but the epicentre was only 20km away from 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 20k
. . .
Some common words found in the essay are:
Fault Unfortunately, Secondary Effects, Kyoto Himeji, Akashi Bridge, Earthquakes Earthquakes, Hanshin Expressway, San Francisco, Mitsubishi Panasonic, Primary Effects, kobe earthquake, earthquakes kobe, earthquakes kobe earthquake, withstand earthquakes, earthquakes ·, electricity gas, expressway bridges, effects ·, hanshin expressway, withstand earthquakes ·, primary effects, secondary effects,
Approximate Word count = 805
Approximate Pages = 3 (250 words per page double spaced)
|
 |
