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Map showing the provinces of Thailand affected. Thailand was one of the 14 countries affected by the 2004 Indian Ocean earthquake and tsunami on 26 December 2004. It left behind unprecedented damage and destruction in six provinces of Thailand, impacting 407 villages, completely destroying 47 of them, including prominent tourist resorts like Khao Lak.
Beyond the heavy toll on human lives, the Indian Ocean earthquake caused an enormous environmental impact that affected the region for many years. Severe damage was inflicted on ecosystems such as mangroves, coral reefs, forests, coastal wetlands, vegetation, sand dunes and rock formations, animal and plant biodiversity and groundwater.
Earthquakes data of Thailand and adjacent areas: 624 B.C. - 1983 A.D. (PDF). Thailand: Geological Society of Thailand. Archived (PDF) from the original on 4 March 2022. Lukkunaprasit, Panitan (1989). State of seismic risk mitigation in Thailand (PDF). Thailand: Chulalongkorn University. Archived (PDF) from the original on 4 March 2022.
An earthquake was recorded off the southern coast of Myanmar on Monday with tremors also felt in Thailand, but there were no immediate reports of major damage. The 5.1 magnitude quake was recorded ...
Thailand's Twelfth National Economic and Social Development Plan (2017-2021) warns that, "At present the country's natural resources and environmental quality are deteriorating, and have become a weakness in maintaining the basis of production, services and sustainable living. A large volume of the natural resources stock has been utilized for ...
2 October 2006: Remnants of Typhoon Xangsane passed over Thailand, killing 47 and damaging 1.3 million rai (2,100 square kilometres (810 sq mi) of farmland and local infrastructure. October–December 2010: Flooding in multiple regions resulted in 80 deaths in Southern Thailand and 180 deaths in upper parts of the country. Damages were ...
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 ...
The earthquake was caused by a strike-slip motion. The earthquake and the largest aftershock (magnitude 8.2, at 10:43 UTC on 11 April) had a fault displacement of 21.3 m (70 ft). [12] The strike-slip nature of the earthquake meant that the movement displaced relatively little seawater and was less likely to cause a tsunami. [13]