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The 2004 Indian Ocean tsunami has been one of the most dangerous and most destructive lately. It had been even catastrophic to get a state like Maldives which never experienced disasters of these scale. Although some of the islands in Maldives were totally destroyed and a substantial number of lives lost; the harms to market, infrastructure, environment and human mind was immeasurable (Pardasani, 2006, p. 80). Having just dealt with storm surges and localized flooding, "that there were not any operational plans or ability to deal with a disaster of this size" at Maldives (Government of Maldives, et al., 2005, p. 9). Despite some organizational flaws, mostly because of their lack of expertise in handling large-scale disasters and limited capacities, research conducted by specialists and specialist bodies (such as Patel Pardasani, 2006; United Nations Children's Fund, 2006) suggest a swift and satisfactory response from the Maldivian Government and response resources. On Sunday, 26 December 2004, a magnitude Mw 9.1-9.3 earthquake happened in the epicentre off the west coast of Sumatra, Indonesia. Both tectonic plates, Indian and Asian, altered by 1,000 km fault line by as much as 20 meters. According to Charles Ammon, professor of geosciences at Penn State University, the earthquake lasted for 500-600 seconds as opposed to the typical couple of seconds, releasing energy equal to a 100 gigaton bomb and also inducing the entire world to vibrate as much as half an inch (Walton, 2005). Although an appalling earthquake, it was the tsunami that did a lot of the damages. Several aftershocks and earthquakes were recorded, some registering up to 6.1 magnitudes. The repercussion of this disaster trigger dormant volcanoes and triggered othe...