Earthquakes are caused by the movement of melting rock called mantle under the earth's surface called tectonic plates. The areas around the boundaries between plates are more likely to have earthquake. The center of the crashing or movement between plates are called the "epicenter". The epicenter seds out seismic waves through layers of rocks to the top surface of the plate where human's structures are built. The severity of an earthquake is measured by the Richter scale, which varies from 1 to 10, having 10 as the most severe.
[Waugh, David. The New Wider World. The United Kingdom: Nelson Thornes, 2003. ]
Earth's Tectonic plates
Among one of the disastrous nature hazard ever occurred in the 20th century, The Chi Chi earthquake in Taiwan in 1999 is recognized as one of the most destructive earthquakes. The earthquake strucked on September 21st in ChiChi Township in the County of Nantou in central Taiwan. The damage caused by the earthquake is considered very severe. There were more than 2,400 deaths and people missing, about 11,400 severely injured, 44,000 structures destroyed, 40,000 structures severely damaged. The reason why this earthquake caused so much damage is that it occurred in the middle of the night, at 1.47am, while the people were not aware, and the epicenter is only about 100 km away from the capital city, Taipei. The severity was recorded at 7.0 Richter scale.
"Chichi (Taiwan) Earthquake".http://www.rcep.dpri.kyoto-u.ac.jp/~sato/taiwan/. December 2nd, 2007
Damaged building
"Damaged provincial government building in ChunHsingHsinTsun ". http://www.rcep.dpri.kyoto-u.ac.jp/~sato/taiwan/twpics/tw/tw043.JPG. December 2nd, 2007
Damaged buildings in Fong Yen
"Earthquake in FongYen". http://www.rcep.dpri.kyoto-u.ac.jp/~sato/taiwan/twpics/tw/tw014.JPG . December 2nd, 2007
Why and How ?
According to the tectonic plates of Taiwan, Taiwan is located along the boundaries of the Eurasian plate and the Philippines plate. The Eurasian plate is a continental crust, while the Philippines plate is an oceanic crust. When both of them moved towards each other, it creates a destructive margin. Destructive margin occurs when an oceanic crust moves toward a continental crust and is forced downward, which can triggers severe earthquake or volcanic eruptions. The earthquake destroyed the whole town of ChiChi, and its aftershock severely damaged five surrounding towns. The map below shows where the aftershocks occured. The blue star is the location of the epicenter in the center of ChiChi.
Map of the Aftershocks
[http://www.rcep.dpri.kyoto-u.ac.jp/~sato/taiwan/index.html]
Tectonic plate map of Taiwan
[http://www.rcep.dpri.kyoto-u.ac.jp/~sato/taiwan/images/twmap2.gif]
Effects on the Economy
Taiwan's central government has estimated the total financial and property loses from the earthquake at 10$-12 $ billion. The earthquake brought down Taiwan's gross domestic product (GDP) for 0.5%. The 3.4$ billion Taiwanese stock market plunged, but very soon recovered.
http://www.rms.com/Publications/Taiwan_Event.pdf
http://www.rms.com/Publications/Taiwan_Event.pdf
http://www.takenaka.co.jp/takenaka_e/rodin_e/structure/structure.html
Picture of the Seismic Isolation System
http://www.takenaka.co.jp/takenaka_e/rodin_e/structure/img/z_02.gif
[http://www.rcep.dpri.kyoto-u.ac.jp/~sato/taiwan/]
[Waugh, David. The New Wider World. The United Kingdom: Nelson Thornes, 2003. ]
[http://en.wikipedia.org/Chi-Chi_earthquake]
http://www.rms.com/Publications/Taiwan_Event.pdf
http://www.takenaka.co.jp/takenaka_e/rodin_e/structure/structure.html
Images Bibliography
[http://www.rcep.dpri.kyoto-u.ac.jp/~sato/taiwan/twpics/tw/tw043.JPG]
http://www.rcep.dpri.kyoto-u.ac.jp/~sato/taiwan/twpics/tw/tw014.JPG
http://www.rcep.dpri.kyoto-u.ac.jp/~sato/taiwan/index.html
http://www.rcep.dpri.kyoto-u.ac.jp/~sato/taiwan/images/twmap2.gif
[http://cache.eb.com/eb/image?id=3537&rendTypeId=4]
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