veD OF TSUNAMI:....ENERGY CARRIER OF NATURAL DESTRUCTION....DAY 2 REPORT
Posted by Vishva News Reporter on December 28, 2004

December 26, 2004: Burma-India Indian Ocean:
Fourth largest earthquake since 1899
created
tsunamis kill 23,000+

  • The world's most powerful earthquake in more than 40 years struck deep under the Indian Ocean off the west coast of Sumatra, triggering massive tsunamis that obliterated villages and seaside resorts in six countries across southern and Southeast Asia.
  • Tourists, fishermen, homes and cars were swept away by walls of water that rolled across the Bay of Bengal, unleashed by the 9-magnitude.
  • Families are making their way to makeshift morgues across Asia and in parts of Africa seeking lost loved ones after tsunamis swept across the Indian Ocean from Thailand to Somalia, killing more than 23,000 (count on 2nd day) people in 10 countries.
  • India: Death toll over 7000.
  •  UNICEF estimates at least a third of dead were children.
  • Sri Lanka: suffered the biggest loss of life (13,000) in the tsunami, crowds had come to the beaches to watch the sea after word spread that it was producing larger-than-normal waves. Thousands of children joined their elders to see the spectacle. The waves brought in fish. The old and the young collected them. Many waited for more fun. Then the 15 feet-to-20 feet tidal waves hit the tropical island of 19 million people. The children got caught and could not run to safety. This is the reason for so many child victims.
  • Somalia, Africa: was hit 4,500 kilometers (2,800 miles) away. Hundreds of people died and entire villages and towns disappeared when tidal waves hit Somalia's coastline in central and northeastern regions.
  • Emergency aid flowing in from many nations.
  • Survivors face the threat of typhoid, malaria, cholera, dysentery and waterborne disease in the worst-hit areas of Sri Lanka, India and Indonesia, where a combination of surging seawater, hot and humid weather, and decomposing bodies means many water supplies are contaminated.

MAP OF
DECEMBER 26, 2004 TSUNAMI

Quake, tsunamis kill thousands

DESTRUCTION FROM
INDIA -BURMA
TSUNAMI

The primary mandate of PVAF is to spread knowledge through humanity....and in compliances PVAF presents knowledge about earthquake created tsunami along with the above news posting....Please click on the next line to enlighten yourself about tsunami from Wikipedia, the free encyclopedia.......



Tsunami

From Wikipedia, the free encyclopedia

(please click on the blue underlined words to have additional information on the words)

A tsunami (from Japanese 津波 meaning wave in port or "harbour wave") is one or a series of ocean surface waves that can occur after a large earthquake (having a vertical component of movement), seaquake, volcanic activity, landslide, slumps, or meteorite impacts in or near the sea. Tsunamis are sometimes referred to as tidal waves as they often resemble a tide that keeps rising, rather than cresting waves when they reach shore. However, the term is misleading as tsunamis are not caused by tides, and its use is being discouraged by oceanographers. While it has also been noted that tsunamis often have little to do with harbors (despite the Japanese translation of the word), the term "tsunami" is used exclusively to refer to water surges caused by physical displacement of water and is thus more correct.

It is probable that the Japanese term was first coined because surges would have the greatest impact, and be most widely witnessed in coastal population centres, which are often built around natural harbours, rather than in sparsely populated or unpopulated areas.

Evidence shows that megatsunamis, which are caused by significant chunks of an island collapsing into the ocean, are also possible.

Related to a tsunami is a seiche. Often large earthquakes produce both tsunamis and seiches at the same time. In addition there is evidence that some seiches have also been caused by tsunamis.

 
Schema of a TsunamiSchema of a Tsunami

 

 

 

 

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Physics

In deep water, the energy of a tsunami is constant, a function of its height and speed. Thus, as the wave approaches land, its height increases while its speed decreases. A tsunami has a very long wave length (in the order of 100 km), which makes it act as a shallow-water wave. Since the speed of a shallow-water wave is {\sqrt{g d}}, where g is the gravitational acceleration and d is the water depth, a tsunami in the open ocean can obtain a speed of about 700 km/h. While in deep water a person at the surface of the water would probably not even notice, the wave can increase to a height of 30 m and more as it approaches the coastline. Tsunamis can cause severe destruction on coasts and islands. If it was caused by e.g. an earthquake, this may be the case at locations where the earthquake itself (with seismic waves travelling faster and therefore arriving earlier) was not even noticable without instruments.

Considering the speed of the wave and the fact that thousands of kilometers from its origin a tsunami can cause damage, there may potentially be some hours of warning time.

Typically, the sea recedes from the coast before it returns with the high wave. This is also a useful warning sign, important to know, otherwise people may stay at the shore out of curiosity.

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Warning Systems

Many cities around the Pacific, notably in Japan but also in Hawaii, have warning systems and evacuation procedures in the event of a serious tsunami. Tsunamis are predicted by various seismologic institutes around the world and their progress monitored by satellites. The first rudimentary system to alert communities of an impending tsunami was attempted in Hawaii in the 1920s. More advanced systems were developed in the wake of the April 1, 1946 and May 23, 1960 tsunamis which caused massive devastation in Hilo, Hawaii. The United States created the Pacific Tsunami Warning Center (http://www.prh.noaa.gov/pr/ptwc/) in 1949, and linked it to an international data and warning network in 1965.

One system for providing tsunami warning is the CREST Project (Consolidated Reporting of Earthquakes and Tsunamis) implemented on the West coast (Cascadia), Alaska, and Hawaii of the United States by the USGS, NOAA, the Pacific Northwest Seismograph Network, and three other university seismic networks.

Tsunami prediction remains an imperfect science. Although the epicenter of a large underwater quake and the probable tsunami arrival times can be quickly calculated, it is almost always impossible to know whether massive underwater ground shifts have occurred, resulting in tsunami waves. As a result, false alarms are common.

No system can protect against a sudden tsunami. A devastating tsunami occurred off the coast of Hokkaido in Japan as a result of an earthquake on July 12, 1993. As a result, 202 people on the small island of Okushiri lost their lives, and hundreds more were missing or injured. This tsunami struck just three to five minutes after the quake and most victims were caught while fleeing for higher ground and secure places after surviving the earthquake.

While there remains the potential for sudden devestation from a tsunami, warning systems can be effective. For example if there were a very large subduction zone earthquake (magnitude 9.0) off the west coast of the United States, people in Japan, for example, would have up to 18 hours (and likely warnings from warning systems in Hawaii and elsewhere) before any tsunami arrived, giving them some time to evacuate areas likely to be affected.

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History

There are many ancient descriptions of sudden and catastrophic waves, particularly in and around the Mediterranean. Thousands of Portuguese who survived the great 1755 Lisbon earthquake were killed by a tsunami which followed a few moments later. Before the great wave hit the harbor waters retreated, revealing lost cargo and forgotten shipwrecks.

The most recent series of lethal tsunamis occurred on December 26, 2004 in the Indian Ocean, with fatalities running in the tens of thousands, ranging from those in the immediate vicinity of the quake in Indonesia and Thailand to people thousands of kilometres away in Bangladesh, India, Sri Lanka, the Maldives, and even Somalia in eastern Africa. Unlike the Pacific Ocean there is no organised alert service covering the Indian Ocean, in part due to there having been no major tsunami there since 1883 (caused by the eruption of Krakatoa).

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Current News

Tsunamis propogatd by an earthquake occuring at Banda Aceh on the island of Sumatra in Indonesia caused devastation in the form of loss of property and lives throughout Asia, particularly Sri Lanka, Indonesia, India(most casualties have been reported in the state of Tamil Nadu and the Andaman and Nicobar Islands), Thailand, Maldives, Malaysia, Myanmar and Bangladesh. As of 9:40 PM GMT on December 27, 2004, news reports estimate the total death toll at 23,000, with Sri Lanka bracing the brunt of the devastation with 13,000 feared dead.

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See also

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External links


 


 



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