The 26 December 2004 Indian Ocean Tsunami: Initial Findings from Sumatra |
||||||||||||||
|
Damage to StructuresBeing just landward of the subduction zone where the tsunami-generating earthquake occurred, northwestern Sumatra was struck by a "near field" tsunami. In contrast, areas across the ocean from the earthquake epicenter, such as Sri Lanka, were struck by "far field" tsunamis. The rapid arrival of the tsunami in near-field locations—just 15 to 20 minutes in Banda Aceh—means that a tsunami early-warning system, now in the planning stages for the Indian Ocean, should be accompanied by tsunami education and long-term emergency and land-use planning efforts for the most effective mitigation of tsunami hazards. Because the tsunami washed out many roads and bridges, the scientists had to hike long distances to reach some field areas, and on several occasions used makeshift rafts constructed from barrels and boards to cross rivers. Despite such complications, they were able to collect much data, which will be used to improve both the scientific understanding of tsunamis and the computer models used to predict tsunami effects. |
|||||||||||||
|
||||||||||||||
|
tsunami/sumatra05/damage.html
contact Guy Gelfenbaum
last modified 2005