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Indonesia was the first country to be seriously affected by the earthquake and tsunami created by the 2004 Indian Ocean earthquake on 26 December 2004, swamping the northern and western coastal areas of Sumatra, and the smaller outlying islands off Sumatra.
The Andaman and Nicobar Islands comprise 572 islands (land masses at low and high tide), of which 38 are inhabited by people from the mainland and indigenous tribes. The islands were just north of the earthquake epicentre, and the tsunami reached a height of 15 metres (49 ft) in the southern Nicobar Islands. The official death toll was 1,310 ...
A massive tsunami with waves up to 30 m (100 ft) high, known as the Boxing Day Tsunami after the Boxing Day holiday, or as the Asian Tsunami, [10] devastated communities along the surrounding coasts of the Indian Ocean, killing an estimated 227,898 people in 14 countries, violently in Aceh , and severely in Sri Lanka, Tamil Nadu , and Khao Lak ...
A woman enjoys the Lampuuk beach in Aceh Besar, Indonesia, on Dec. 24, 2024, ahead of the 20-year anniversary of the devastating tsunami that struck the city on December 26, 2004.
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Maximum recession of the sea at Kata Noi Beach at 10:25 a.m., prior to the third—and strongest—tsunami wave. The economic impact of the tsunami on Thailand was considerable, though not as great as in poorer countries such as Indonesia or Sri Lanka. Thailand has a liberalised, flexible and robust economy, which has shown powers of rapid ...
The train which was struck by the tsunami. Remains of a house near Telwatte, photographed in March 2008. In Ampara District alone, more than 10,000 people died. A holiday train, the "Queen of the Sea", was struck by the tsunami near the village of Telwatta as it travelled between Colombo and Galle carrying at least 1,700 passengers, killing all but a handful on board.
Earthquake environmental effects are divided into two main types: Coseismic surface faulting induced by the 1915 Fucino, Central Italy, earthquake. Primary effects: which are the surface expression of the seismogenic source (e.g., surface faulting), normally observed for crustal earthquakes above a given magnitude threshold (typically M w =5.5 ...