Please use this identifier to cite or link to this item: http://saruna.mnu.edu.mv/jspui/handle/123456789/14288
Title: 2004 Indian ocean tsunami on the Maldives islands : initial observations
Authors: Dominey-Howes, Dale
Helsley, Charles. E.
Waheed, Zaha
Issue Date: Jan-2005
Publisher: ResearchGate
Citation: Keating, B., Helsley, C. E., & Dominey-Howes, D. (2005). 2004 Indian ocean tsunami on the Maldives islands: initial observations. Science of Tsunami Hazards, 2.
Series/Report no.: Science of Tsunami Hazards;
Abstract: Post-tsunami field surveys of the Maldives Islands where carried out to document the effects of the tsunami inundation. The study area was situated in the islands of South Male Atoll that were some of the most heavily damaged islands of the Maldive Islands. The tsunami damaged the natural environment, vegetation, man-made structures, and residents. The maximum tsunami wave height was 3-4 m. This level of inundation exceeded the height of most residents. The wave height was greatest on the eastern rim of the South Male Atoll (closest to the tsunami source) and these islands were completely flooded. The islands within the interior of the atoll saw the lowest wave heights, and these were only marginally flooded.Surveys of flood lines left on the exterior and interior of structures were measured but proved to be substantially less than that reported by survivors. It appears that the highest inundation was not preserved as flood lines. We suggest that the turbulence associated with the tsunami inundation erased the highest lines or that they did not form due to an absence of debris and organic compounds that acted as adhesion during the initial flooding. Significant erosion was documented. Deposition took place in the form of sand sheets while only desultory deposition of coral clasts in marginal areas was found. Seasonal erosion, and storms are likely to remove most or all of the traces of the tsunami within these islands.
URI: http://saruna.mnu.edu.mv/jspui/handle/123456789/14288
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