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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 ...
Malé, the capital island of the Maldives was severely hit by the tsunami. In the independent republic of Maldives , all islands except for 9 were hit by the 2004 Indian Ocean tsunami. 82 people were killed and 24 reported missing and presumed dead after the archipelago was hit by a tsunami caused by the 2004 Indian Ocean earthquake on 26 ...
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.
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 ...
Aerial view of new village in Banda Aceh to house people left homeless by the tsunami Indonesian tsunami victims gather under an approaching US helicopter to receive food and supplies. Although Indonesia was the first and worst hit of countries in the region, it was the last to begin receiving relief aid.
Seismology (/ s aɪ z ˈ m ɒ l ə dʒ i, s aɪ s-/; from Ancient Greek σεισμός (seismós) meaning "earthquake" and -λογία (-logía) meaning "study of") is the scientific study of earthquakes (or generally, quakes) and the generation and propagation of elastic waves through planetary bodies.
Amplitude, Wave Height, or Tsunami Height: Refers to the height of a tsunami relative to the normal sea level at the time of the tsunami, which may be tidal High Water, or Low Water. It is different from the crest-to-trough height which is commonly used to measure other type of wave height.
Burma does not allow journalists into the country and maintained a strong hold on information disseminated in its state-run newspapers - some of which did not acknowledge the tsunami had hit. [10] Burma had refused foreign aid, insisting it was capable to cope by itself. [11]