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Brahaminical Hegemony has nothing to do with Calamity Management in the DMK ruled Anti Brahamin Aboriginal Humanscape and the Tsunami experience had no lesson to be learnt as Tamilnadu and Andhra are subjected to Natural Calamities time and again. It


Brahaminical Hegemony has nothing to do with Calamity Management in the DMK ruled Anti  Brahamin Aboriginal Humanscape and the Tsunami experience had no lesson to be learnt  as Tamilnadu and Andhra are subjected to Natural Calamities time and again. It is only the Death Toll which counts!


Indian Holocaust My Father`s Life and Time - FIVE Hundred  Thirty Five

Palash Biswas

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It seems that the Brahaminical Hegemony has nothing to do with Calamity Management in the DMK ruled Anti  Brahamin Aboriginal Humanscape and the Tsunami experience had no lesson to be learnt  as Tamilnadu and Andhra are subjected to natural calamities time and again.

It is only the Death Toll which counts!

It is also raining in West Bengal coastal areas but it is welcome as it brings the most wanted Winter, always an enjoyable weather in Bengali lifestyle!

Heavy rains pounded Tamil Nadu for the second day today, throwing normal life out of gear and leading to closure of educational institutions in many districts.

Over 179 people have been killed in rain-related incidents across the state since the onset of the northeast monsoon in October, which is vigorous over Tamil Nadu and Puducherry.

As Mr Gopalan had warned taht it would be raining in Tamilnadu, we had Rain all over the state during our visit.In Andhra, specially in Vishakhapattanam it was too hot.

Even while we were returning from Bangaluru where it was cold and we were wearing sweaters and warm clothes but as soon as we reached in Vellore district it was Hot once again.

We knew the climate cycle and all about the late Monsoon.

It was Cyclone which hit the East Coast just before we had to reach Tamilnadu.

Now,a fresh low pressure trough in the Bay of Bengal is giving no respite to the rain battered Tamilnadu where a flood-like situation prevails in majority of the coastal districts.

All the reserviors in the state are full and there has been enormous damage to crops. Schools in eleven districts including Chennai, Cuddalore, Nagapattinam and Trichy will remain closed on Monday.Heavy rain is expected in again in many northern districts of Tamil Nadu.

Fishermen have been warned not to venture into the sea.

Meanwhile, the death toll in rain related incidents in Tamil Nadu has crossed one hundred and fifty.

A majority of deaths were due to electrocution, wall collapses, lightning and drowning in flood waters. More than 1,500 head of cattle have perished in the rains.

We have witnessed the signs of Tsunami still Fresh in Marina Beach, Chennai, though it did not touch RAMESHWARAM which further strenthened the Aryan superstitious Charisma of God Rama, the Killer!

I am sorruy that despite feeling the Refugee Influx from Srilanka in and around Ramnathpuram disrtict of Rameshwaram, I was unable to vist any Tamil Refugee camp.

As we did not know Tamil and were quite helpless to interact with the Rural Population which speaks only Tamil!

Now, LeT planned to set up base in TN, it is the latest story thanks to wikileaks!

Comparatively, the Cow belt is most inflicted with Terror and the Shaffron Terror is phennomenal there, but the Ruling Hegemony tend to brand Tamilnadu as a Terrorist state which is far better than any North Indian state as far as Law and Order is concerned. Sabita noted it minutely  that women and children could travel with Heavy Jwellery everywhere in the South which we may never imagine in the North.

Tamilnadu is tagged with Maosit Hit Central India, North east and Kashmir, all of which makes the Aboriginal Humanscape.

The Antipathy against the Non Aryan Dravid people is quite evident despite the presence of south Indian Politicians and Officers in abundance in the centre.

It is the same case with the SC OBC bengali refugess who face Mass Destruction just because of the Brahamin ruling Bengal as well as India.

South Indian leadership has nothing to do with either the Tamil Refugees or the Rural Coastal pouplation Dravid Non Aryan!

The morning newspapers in Kolakta published stories about Maoist PREPAK nexus today.

Earlier they had been highlighting Litte Maoist link or ISI Maoist link as they fail to establish any link with China as china is least interested with the internal matters of India.

Had it been the case, it would have been very impossible to defend integrity and unity in the North East.

Though it was soothing experience for the eyes to see peasants busy in the Green fields harvesting paddy crop and at the same time planting the Paddy all over the South.

We could not stay in Khurda Road or Brahamapur to visit the Chilka Lake where our people the Scheduled caste Bengali Untouchable Refugees have been resettled.

In the Tanjavur district tribal region , as Waaman Meshram, the Bamcef chairperson told me, there is also a refugee Resettlement.It is also in the East Coast most cyclone prone.

I came to know about this only in Kanyakumari while Meshram and I interacted on mobile phone.

Later, Mangesh Kumar from OOTY also informed me that Persecuted Bengali Refugees are resettled somewhere in Nilgiri district but we could not locate them.

In Raichur district of Karnataka, near the kurnul ditrict of Andhra, more than 2200 hundred families of SC Bengali refugees are resettled and we remain disconnected to all these black untouchbales.

These people had been habitual of the climate conditions in the Bay of bengal region in their earst while homeland in East Bengal. But destiny ejected them and resettled in yet another cyclone prone zone!

We never know the casaulty inflicted upon them.

But the Non Aryan Dravid communities are NO diferent from these people, we have realised this time as Never before!

The rain fury has claimed as many as 179 lives in Tamil Nadu since the onset of northeast monsoon in late October. Chief Minister M. Karunanidhi Monday held an emergency meeting of officials to take stock of the situation.

According to the police control office here, the majority of deaths have taken place due to wall collapses and lightning strikes. The weather department has predicted rains till Tuesday evening in coastal districts due to low pressure in Bay of Bengal over Tamil Nadu.

In state capital Chennai, the incessant rains since Sunday night threw life out of gear.

Karunanidhi held a meeting with Chief Secretary S. Malathi and others to review the rain related damage and the relief measures being undertaken. The officials looked into the relief measures taken and checked whether the compensation amount has been properly distributed.

Meanwhile, eight senior officials continued their survey and estimation of rain damage in nine districts -- Cuddalore, Nagapattinam, Thanjavur, Thiruvarur, Villupuram, Tuticorin, Tirunelvelli, Pudukottai and Ramanathapuram.

The officials will submit their report Tuesday and the state cabinet will deliberate on that the same day.

The government has already announced Rs.100 crore towards relief operations in the first phase.

The weather office has predicted more rains during the next 24 hours beginning 0830 hrs today due to a well marked low pressure over the Bay of Bengal.

Chief Minister M Karunanidhi reviewed the situation with Chief Secretary S Malathi and Revenue officials.

"The well marked low pressure over Bay of Bengal is moving northwards. Under its influence heavy rains would continue to occur over coastal areas of Tamil Nadu and Puducherry during the next 24 hours starting today at 8.30 AM,", officials said.

They warned fishermen against venturing into the sea.

Strong onshore winds with speeds reaching 45-55 kmph are likely to blow along North Tamil Nadu and Puducherry coasts in the next 24 hours starting 0830 hrs today.

Thousands of acres of standing crops remained submerged across the state. Special officers appointed by the state government are on a tour of the rain-hit districts to assess the damage caused by the rain.

The officers would submit a report on the damage to crops and property, which will be discussed at an emergency meeting of the state Cabinet here tomorrow being chaired by Karunanidhi.

In Chennai, heavy rains since Sunday led to flooding of low-lying areas, making life difficult for office-goers, who had to wade through the water. Many trees were uprooted due to gusty winds.Corporation officials were working in full swing for rehabilitating people affected in the rain.

Traffic congestion was reported from different parts of the city especially in areas such as Guindy where preliminary works for the Metro rail project are underway.

Schools in Chennai and many other districts remained closed.

Educational institutions in neighbouring Puducherry also remained closed for the fifth successive day.

The state government had announced a sum of Rs 2 lakh to the kin of persons killed in rain-related incidents and allocated a sum of Rs 100 crore towards relief and repairs.

The water level in the Mettur dam in Salem this morning stood at 120.05 feet against the full level of 120 feet.

All the seven rivers running across different communes in Karaikal were in spate.
Kamayani Bali Mahabal posted in Say No to UID.
*
Kamayani Bali Mahabal

11:23pm Dec 6



Aadhar And UIDAI Are Tools Of Social Oppression

Posted on December 2, 2010 < http://www.facebook.com/l/a12ce8y_nBB3t37yld39g_nTOlQ;cjnews.noads.biz/?p=847> by Catherine

Fernandes < http://www.facebook.com/l/a12ceL2GNpVPyopxPBcVeDhUEIg;cjnews.noads.biz/?author=2>

*

*


*Aadhar project of India* < http://www.facebook.com/l/a12ceE8jv9tbFYzVR8FxATJ3CJQ;perry4law.com/hr/uid.html> or UID project

of India is often portrayed as a tool of social inclusion. But this is just

a façade. The truth is that Aadhar is a tool and instrumentality of social

oppression and social exploitation of Indians.


To achieve this exploitative purpose, unique identification authority of

India (UIDAI) has been established. Despite the ferocious protests by civil

liberty activists, neither Aadhar project nor UIDAI are empowered by a legal

framework. Even the National Identification Authority of India Bill 2010

(Bill) has failed to provide adequate safeguards against privacy violations

and data breaches.


Interestingly, even if the Bill proposed by UIDAI is made an enforceable

law, it still remains unconstitutional. According to *Praveen

Dalal*< http://www.facebook.com/l/a12cep3NtFb7K3Tgo0X5LJD9cOg;hrpic.blogspot.com/2010/06/appraisal-of-national-identification.html>,

Supreme Court Lawyer and leading Techno Legal Expert of India, even if the

Bill becomes an enforceable piece of Legislation, it still is vulnerable to

the attacks of "Unconstitutionality". In the absence of "Proper Laws and

Adequate Safeguards", both Aadhar Project and UIDAI would remain

"Unconstitutional", warns Praveen Dalal.


The *privacy rights issues* < http://www.facebook.com/l/a12ceGXNiNmkEsekjbAJ7tBi9rA;cjnews.noads.biz/?p=834> are currently

pending before the Supreme Court of India. It would be a good idea to

strengthen Privacy and Data Protection Laws of India by "*Judicial

Activism*< http://www.facebook.com/l/a12ceZgU8GawF5hqLofuWNL84iw;cjnews.noads.biz/?p=844>"

in the absence of "Parliamentary Will", suggest Praveen Dalal.


Behind the façade of social inclusion and welfare scheme, the naked face of

Aadhar and UIDAI is very apparent. Aadhar project is an

instrumentality of *e-surveillance

in India* < http://www.facebook.com/l/a12cetWvx1GMzQPwrAooKj_8Fgg;cjnews.noads.biz/?p=824>. Its only purpose is to serve the

unlawful interests of intelligence agencies of India and law enforcement

demands in India.


Let us not be fooled by the façade of social inclusion and welfare scheme

and ask the government of India to enact suitable and adequate privacy and

data protection laws before Aadhar is fully operational in India.


http://www.facebook.com/l/a12cebJScAWqC0fzE-gqbL-eT7Q;cjnews.noads.biz/?p=847


Damaging downpour

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Former Bengal captains want Sourav in KKR

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'Moner Manush' captures the life of Bengal poet

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Ikene return will boost Salgaocar''s attack

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Rs 745-crore plan for renovating dams in TN

Express News Service
First Published : 21 Nov 2010 02:52:59 AM IST
Last Updated : 21 Nov 2010 09:50:16 AM IST

CHENNAI: Chief Minister M Karunanidhi on Saturday constituted an 11-member empowered committee headed by Chief Secretary S Malathi to expedite the Rs 745.49-crore plan drawn for renovating the dams in Tamil Nadu over a period of six years.The scheme will be implemented in a phased manner from next financial year. As many as 66 dams maintained by the Water Resources Department and 38 dams under the control of Tamil Nadu Electricity Board (TNEB) would be renovated under this scheme with an assistance from the World Bank.

Karunanidhi makes cryptic remark on Alagiri

"People are calling my son 'Anjanenjan Alagiri'. Just at the mention of the name Alagiri, some smile, others get angry and a few others feel hatred. But I think he is like a sugarcane. If one tastes the cane from the bottom, it tastes sweet. But if we go on tasting it up to its tip, one would taste sourness instead of sweetness."Similarly, the people of Tamil Nadu as well as DMK cadre in Madurai should use Alagiri the way they taste sugarcane.... If they go overboard and start using him to the tip thinking that he is just the son of Karunanidhi, it would be like tasting the tip of the sugarc­ane — it will tear their tongue.... My dear son Alagiri is a blend of all qualities," he said.The sugarcane metaphor assumes significance as there have been reports of simmering discontent in the mind of Alagiri, despite the bonhomie shared by various members of the Karunanidhi family at the wedding celebrations.Given the talk that Alagi­ri would mobilise support in the party after his son's wedding to push his case to lead the DMK, a question pops up: was Karunanidhi's suggestion that Alagiri has his limitati­ons aimed at telling his supporters not to aspire for anything big for their leader?

'Seeking resignation on CAG report unfair'

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TN political scene set to change

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TNUSRB Results 2010: TNUSRB publishes Police Constables Recruitment Result

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Tamilnadu Jai Bharath Mills to consider FCD issue on Dec 01, 2010

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Infighting a democratic right: YC observer

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Govt gives nod to setting up of 14 world-class universities

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YC claim on government scheme irks DMK

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Though the article indicates DMK's reluctance to hit out at its ally, it is clear that is gripped with fears over the growth of the Congress in Tamil Nadu.

TamilNadu Farmers face acute shortage of fertilizers

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Paddy grown in 440 acre damage due to rains in Sirsi

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Essar Hypermart targets 30% expansion of steel retail chain in TN by 2011

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Director locks lips with Heroine

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After Adarsh Chavan, it's Licence Raja

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Dr.Farooq Abdullah visits Suzlon's Wind-Farm at Radhapuram

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Private hospitals to start ICTC under PPP mode

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Karunanidhi writes to PM

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Coconut oil to rise further on low supplies

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IMD Weekly Whether Updates:

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Ranji Trophy 2010-11 : Karnataka vs Orissa : Hosts script an innings win

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Legal literacy camp held

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World Organ Donation Day 2010: 'Take 2, Give a Second Chance in Life'

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Nene Ambani releasing on December 10th!

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Dolphy Dsouza : Young and Emerging Political Face of DK

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Development of SCs

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... Jharkhand, Kerala, Maharashtra, Manipur, Meghalaya, Mizoram, Nagaland, Punjab, Rajasthan , Sikkim , Tamilnadu, Tripura and West Bengal . ...

Ranil Wickremasinghe leaves to India

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Kiddy watch

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'Yadharthaa'- Tamilnadu Children Film Society has brought wide sub-genres of children films by various globally wel




LeT planned to set up base in TN: Wikileaks

Tamil Nadu was on the radar of the Lashkar-e-Toiba when it was planning to set up training sites and operational bases in southern India in the middle of 2009, according to US embassy cables released by WikiLeaks.

A June 18, 2009 document, titled 'US climate change negotiators targeted by cyber attack' and "derived from multiple sources", said Pakistan-based LeT member Shafiq Khafa was "possibly preparing for operations" and an LeT member based in India, Hussein, continued operational planning on three tasks, including a possible assassination of Gujarat Chief Minister Narendra Modi, in early June.

Khafa, who along with an India-based associate, SJ, prepared for operations in mid-June, was looking for information on possible training sites in Tamil Nadu, Karnataka and Kerala, revealed the document, uploaded by the Guardian newspaper's website.

The network of Khafa strove to put up two teams in the South, which would rely on the support of LeT members in India, Sri Lanka, Pakistan and Nepal, though specific details of planned attacks remained unknown.

Intelligence gathered in late- May, however, indicated Khafa's cell was engaged in surveillance activities of potential targets in southern India, stated the document.

Early May reports stated that Tamil Nadu and Kerala could be used as a base of operations following the establishment of a facilitation team in Sri Lanka.

The document added that the facilitation route and camps were estimated to be set up in two to three months.

The source for the document was marked 25X1-human and the reference to south India and Tamil Nadu is made under sub-head 'Key Concerns'.

Congress may capture power in TN: PC

.  Speaking at a memorial meeting organised by K Selvaperunthagai besides others in the Tamil Nadu Congress Committee (TNCC) to mark the death anniversary of Babasaheb BR Ambedkar here, Chidambaram regretted that Dalits continued to face discrimination like untouchability even in urban areas.A way out of the situation was offered by education, he said and urged the oppressed people to use education and the support provided by the government as tools to overcome discrimination and succeed in life."Education would propel people to high positions in life besides providing the ability to solve tricky issues", he pointed out.  The Congress-led UPA government had been implementing support schemes worth several thousands of crores to ensure that Dalits received good education. "Dalits are given incentives, financial assistance and reservation besides educational loans," he said and urged them to take this as a good opportunity and become qualified."Get good education. Please don't ignore it, because it is both a shield and weapon. Then, take positions in the party and then assume responsibilities in the government," he said.  Stressing that the Congress party had always respected Dalits, Chidambaram pointed out that his party made Kakkanji the home minister in Tamil Nadu and Babu Jagjivan Ram the defence minister at the Centre.Expressing strong belief that the Congress party would get an opportunity to rule Tamil Nadu in future, he said: "At that point in time, when the Congress gets opportunity, a Dalit would be a home minister, a finance minister and a Dalit would even be the Chief Minister," he said.

TMMK demands handing over of Babri Masjid site to Muslims

                                                                
Submitted by admin3 on 6 December 2010 - 7:36pm
By TCN News,
Chennai: Tamilnadu Muslim Munnetra Kazhagam (TMMK) conducted sit-in at 42 important cities and towns of Tamilnadu today to remember the 18th anniversary of Babri Masjid demolition and express displeasure against the Allahabad High Court verdict of September 30.
At the dharnas, TMMK demanded prosecution of 68 persons accused by the Liberhan Commission as responsible for Babri Masjid demolition, expedition of the Babri Masjid criminal case pending in the Raebareli and speedy disposal of the appeal petition filed against the judgement given by the Allahabad High Court in the Babri Masjid title suit.
Prof. M.H. Jawahirullah, President, TMMK, led a dharna in which political activists Mr. Jagaveerapandian, Mr. Che. Ku. Tamilarasan, Advocate Muthukrishnan, CPM State Executive committee Member Mr. Shanmugam, besides others participated to express their solidarity.
Speaking on the occasion Prof. M.H. Jawahirullah said all illegal activities relating to Babri Masjid have happened when Congress was ruling the country. He said prayers were held in Babri Masjid from 1528 to 1949 December 22. On the night of December 22 idols were placed under the central dome of the Masjid when Congress was ruling the centre and the state of UP. Similarly on February 1, 1985, when Congress was ruling the country and the UP state the locks of Babri Masjid were ordered to be opened by the Faizabad District court which has no jurisdiction to pass such an order. The court order came a few days after the then Prime Minister Mr. Rajiv Gandhi has promised that the locks of Babri Masjid would be opened to allow Darshan before Shivaratri. Babri Masjid was demolished on 6th December 1992 when the P.V. Narasimsha Rao led Congress Government was in power at the centre. The then Congress Prime Minister had promised the nation in
his televised speech that the Masjid would be reconstructed at the spot where it stood. Successive Congress Governments have failed to keep up this promise.
"To add salt to the wound, the Lucknow Bench of the Allahabad High Court has given a judgement which is a black dot in the history of Indian Judiciary when Congress is again ruling the nation. The Congress party should remember that it lost power in UP and
subsequently in Delhi for its anti secular and anti constitutional misdemeanours in the Babri Masjid case," TMMK chief said.
http://twocircles.net/2010dec06/tmmk_demands_handing_over_babri_masjid_site_muslims.html

Rahul's mission TN to take off with YC yatra


CHENNAI: Youth Congress activists will tour the length and breadth of State's hinterland in the next four months to unleash an information blitzkrieg on the achievements of the Union government as part of the 'Mission Tamil Nadu' launched by Rahul Gandhi.The State executive committee of the TN Youth Congress met at Delhi on Thursday and several plans to help galvanise the party in the State through the youth wing ahead of the 2011 polls were finalised by Rahul Gandhi.Speaking to Express, State Youth Congress president M Yuvaraja said Rahul Gandhi was determined to see the party rise in the State. Rahul unveiled a plan, "Mission Tamil Nadu," which aimed at strengthening the party at the grassroot level.As part of the plan, youth wing workers would tour rural regions to publicise the Centre's schemes. The rural padyatra will commence on December 28 and conclude on January 26. This will be the first step of the mission to be followed by streetcorner and public meetingsFor the next four months, programmes have been finalised that had a twin objective of understanding the commonman's problems better and to sensitise them to the measures taken by the Centre."Rahul appreciated our recent padyatra campaign. He stressed the need to do more especially in rural areas," Yuvaraja said adding this was the first time Rahul that participated in the executive meet of a State youth unit. Mission Tamil Nadu is part of a comprehensive plan to help brighten the party prospects which is not only aimed at the legislative assembly elections.
http://expressbuzz.com/states/tamilnadu/rahuls-mission-tn-to-take-off-with-yc-yatra/227920.html

Tapes talk volumes about MK's family: Jaya


CHENNAI: The telephonic conversations corporate lobbyist Niira Radia had with former Union telecom minister A Raja, some industrialists and journalists "mainly show the first family of Tamil Nadu in their true colours," AIADMK general secretary J Jayalalithaa charged on Friday.In a statement, Jayalalithaa said: "In the brouhaha over the Rs1,76,379 crore 2-G spectrum scam perpetrated by A Raja of the DMK, an interesting side-show has gone largely unnoticed, at least in Tamil Nadu: the series of telephonic conversations between the various dramatis personae with Niira Radia, a liaison agent for large corporates like the Tatas and Ambanis, who is also a political wheeler-dealer, apparently wielding considerable extra-constitutional influence in the corridors of power." "A conversation between Niira Radia and senior journalist Vir Sanghvi (who was apparently an interlocutor between the Karunanidhi family and the Congress leadership), shows the utter disdain the Central leadership has for its Tamil Nadu allies."An excerpt from the tapes shows  Sanghvi as saying: "As far as we are concerned, there are two wives, one brother, one sister, one nephew… It's all got very complicated for us… This is not a Congress-DMK problem. This is an internal DMK problem because they can't get their act together between all his wives and children and nephews…"Jayalalithaa said Karunanidhi's daughter Kanimozhi is on record demanding for herself the Environment portfolio, failing which she wants Health or Aviation or Tourism and Culture. Kanimozhi is also on record making an impassioned plea for the telecom portfolio for her close friend, A Raja, while foul-mouthing another aspirant, her nephew and Karunanidhi's grand-nephew Dayanidhi Maran."Another senior journalist Barkha Dutt is recorded conveying the Congress leadership's exasperation over a media announcement by T R Baalu that the DMK was planning to boycott the swearing-in ceremony to embarrass the Congress and pressure them to yield to the DMK's multifarious demands," she pointed out in the statement.One conversation reveals that Dayanidhi Maran had been carrying out a smear campaign in Delhi circles against his uncle and Karunanidhi's elder son M K  Alagiri, whom Dayanidhi had described as uneducated, having studied only up to Class V and illiterate in English. Yet another conversation indicates that Dayanidhi was canvassing for a "lucrative" infrastructure portfolio for himself, against the wishes of the DMK chief."A person like Alagiri, whom the Tamil Nadu population know as one accused in murder cases, and whose close circle of friends include 'Attack' Pandi, 'Sori' Murugan, 'Auto' Ravi, 'Ochu' Balu and 'Blade' Pakiri, has been projected to the Central leadership as a 'mass leader'.""In yet another conversation between Niira Radia and Vir Sanghvi, it comes out that despite Karunanidhi's objections to Dayanidhi Maran, the Maran scion's candidature was being actively canvassed by M K Stalin and M K Selvi, who is married to Murasoli Maran's brother Selvam."The reason for pushing Dayanidhi does not apparently stem from blood ties, but "from the fact that Dayanidhi had paid a whopping Rs 600 crore to Stalin and Selvi's mother and one of Karunanidhi's wives, Dayalu." This is in addition to the "rounded up" sum paid by Kalanidhi Maran to the Karunanidhis for relinquishing their shares in the Sun TV network in 2007, the AIADMK leader said.She said the period of the recordings leaked in the media relate to the days of ministry formation of UPA-2, when Karunanidhi was bargaining hard to get the maximum number of plum portfolios with money-earning potential, not for the DMK members, but for the various members of his own huge family."The IT Department was trying to trace the trail of the illegal funds of political persons obtained through extending favours to corporate houses and for this purpose had placed the telephones and mobile phones of Niira Radia under surveillance for a certain period," Jayalalithaa said.

Ahead of Pongal, actor Vijay may float new party

.At the closed-door meeting of the office-bearers of his fan club held at V S Kalayana Mandapam in Vadapalani, the actor reportedly sought the views of his fans on his entering politics. They overwhelmingly supported the idea of a new party and entering the electoral arena solo rather than his joining some other party. However, some fans suggested that the new party could forge an alliance with the AIADMK.Deliberations were on inside the mandapam with the media kept at bay since noon. Around 7.30 pm, when the fans dispersed, they were confident that a new party would be launched.It is said that Vijay had been speaking his mind to fans at the district level for quite some time, though this was the first time he had called fan club leaders from all over the State for a meeting. However, it remains to be seen if the new party would make any impact in State politics, for Vijay's following is more or less restricted to his fan clubs. He also has a string of box office failures and had political ambitions.Over a year ago, he even went to New Delhi to meet AICC general secretary Rahul Gandhi. Though nothing came of the meeting — it was then said that he wanted to be the chief of the Tamil Nadu Congress unit — and he continued to act in films, it now appears that he has dropped the Congress option.Be that as it may, with a whole host of political parties in the scene, Vijay might not be able to make a mark as a leader.It is also doubtful whether people would accept him as a politician at a time when he is also not seen as a successful actor.
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2004 Indian Ocean earthquake and tsunami

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2004 Indian Ocean earthquake
Tsunami strikes Ao Nang, Thailand.
Date December 26, 2004 (2004-12-26)
Magnitude 9.1 Mw
Depth 30 km (19 mi)
Epicenter location 3°18′58″N 95°51′14″E / 3.316°N 95.854°E / 3.316; 95.854Coordinates: 3°18′58″N 95°51′14″E / 3.316°N 95.854°E / 3.316; 95.854
Type Undersea (subduction)
Countries or regions affected Indonesia (mainly in Aceh)
Sri Lanka
India (mostly in Tamil Nadu)
Thailand
Maldives
Tsunami Yes
Casualties 230,000+[1][2] (the fifth deadliest earthquake in recorded history)
2004 Indian Ocean
earthquake
2004 Indian Ocean earthquake and tsunami

Events

Response

See also



The 2004 Indian Ocean earthquake was an undersea megathrust earthquake that occurred at 00:58:53 UTC on December 26, 2004, with an epicentre off the west coast of Sumatra, Indonesia. The quake itself is known by the scientific community as the Sumatra-Andaman earthquake.[3][4] The resulting tsunami is given various names, including the 2004 Indian Ocean tsunami, Asian Tsunami, Indonesian Tsunami, and Boxing Day Tsunami.

The earthquake was caused by subduction and triggered a series of devastating tsunamis along the coasts of most landmasses bordering the Indian Ocean, killing over 230,000 people in fourteen countries, and inundating coastal communities with waves up to 30 meters (100 feet) high.[5] It was one of the deadliest natural disasters in recorded history. Indonesia was the hardest hit, followed by Sri Lanka, India, and Thailand.

With a magnitude of between 9.1 and 9.3, it is the third largest earthquake ever recorded on a seismograph. This earthquake had the longest duration of faulting ever observed, between 8.3 and 10 minutes. It caused the entire planet to vibrate as much as 1 cm (0.4 inches)[6] and triggered other earthquakes as far away as Alaska.[7] Its hypocenter was between Simeulue and mainland Indonesia.[8]

The plight of the many affected people and countries prompted a worldwide humanitarian response. In all, the worldwide community donated more than $14 billion (2004 U.S. dollars) in humanitarian aid.[9]

Contents

[hide]

Earthquake characteristics

The earthquake was initially reported as moment magnitude 9.0. In February 2005 scientists revised the estimate of the magnitude to 9.3.[10] Although the Pacific Tsunami Warning Center has accepted these new numbers, the United States Geological Survey has so far not changed its estimate of 9.1. The most recent studies in 2006 have obtained a magnitude of Mw 9.1–9.3. Dr. Hiroo Kanamori of the California Institute of Technology believes that Mw 9.2 is a good representative value for the size of this great earthquake.[11]

The hypocentre of the main earthquake was approximately 160 km (100 mi), in the Indian Ocean just north of Simeulue island, off the western coast of northern Sumatra, at a depth of 30 km (19 mi) below mean sea level (initially reported as 10 km). The northern section of the Sunda megathrust, which had been assumed dormant, ruptured; the rupture having a length of 1300 km.[8] The size of the rupture caused plate shifting of up to 20 m,[citation needed] causing the earthquake (followed by the tsunami) to be felt simultaneously as far away as Bangladesh, India, Malaysia, Myanmar, Thailand, Singapore and the Maldives.[12] Splay faults, or secondary "pop up faults", caused long, narrow parts of the sea floor to pop up in seconds. This quickly elevated the height and increased the speed of waves, causing the complete destruction of the nearby Indonesian town of Lhoknga. [13]

The epicentre of the earthquake, just north of Simeulue Island.

Indonesia lies between the Pacific Ring of Fire along the north-eastern islands adjacent to and including New Guinea and the Alpide belt along the south and west from Sumatra, Java, Bali, Flores, and Timor.

Great earthquakes such as the Sumatra-Andaman event, which are invariably associated with megathrust events in subduction zones, have seismic moments that can account for a significant fraction of the global earthquake moment across century-scale time periods. The Sumatra-Andaman earthquake was the largest earthquake since 1964, and the second largest since the Kamchatka earthquake of October 16, 1737.

Of all the seismic moment released by earthquakes in the 100 years from 1906 through 2005, roughly one-eighth was due to the Sumatra-Andaman event. This quake, together with the Good Friday Earthquake (Alaska, 1964) and the Great Chilean Earthquake (1960), account for almost half of the total moment. The much smaller but still catastrophic 1906 San Francisco earthquake is included in the diagram below for perspective. Mw denotes the magnitude of an earthquake on the moment magnitude scale.

Since 1900 the only earthquakes recorded with a greater magnitude were the 1960 Great Chilean Earthquake (magnitude 9.5) and the 1964 Good Friday Earthquake in Prince William Sound (9.2). The only other recorded earthquake of magnitude 9.0 or greater was off Kamchatka, Russia, on November 4, 1952 (magnitude 9.0).[14] Each of these megathrust earthquakes also spawned tsunamis in the Pacific Ocean, but the death toll from these was significantly lower. The worst of these caused only a few thousand deaths, primarily because of the lower population density along the coasts near affected areas and the much greater distances to more populated coasts.

Other very large megathrust earthquakes occurred in 1868 (Peru, Nazca Plate and South American Plate); 1827 (Colombia, Nazca Plate and South American Plate); 1812 (Venezuela, Caribbean Plate and South American Plate) and 1700 (western North America, Juan de Fuca Plate and North American Plate). All of them are believed to be greater than magnitude 9, but no accurate measurements were available at the time.

Tectonic plates

A pie graph of the largest earthquakes from 1906 to 2005.

The megathrust earthquake was unusually large in geographical and geological extent. An estimated 1,600 km (994 mi) of fault surface slipped (or ruptured) about 15 m (50 ft) along the subduction zone where the India Plate slides (or subducts) under the overriding Burma Plate. The slip did not happen instantaneously but took place in two phases over a period of several minutes:

  • Seismographic and acoustic data indicate that the first phase involved a rupture about 400 km (250 mi) long and 100 km (60 mi) wide, located 30 km (19 mi) beneath the sea bed—the largest rupture ever known to have been caused by an earthquake. The rupture proceeded at a speed of about 2.8 km/s (1.7 mi/s) or 10,000 km/h (6,300 mph), beginning off the coast of Aceh and proceeding north-westerly over a period of about 100 seconds.
  • A pause of about another 100 seconds took place before the rupture continued northwards towards the Andaman and Nicobar Islands. However, the northern rupture occurred more slowly than in the south, at about 2.1 km/s (1.3 mi/s) or 7,600 km/h (4,700 mph), continuing north for another five minutes to a plate boundary where the fault type changes from subduction to strike-slip (the two plates slide past one another in opposite directions). This reduced the speed of the water displacement and so reducing the size of the tsunami that hit the northern part of the Indian Ocean.[15]

The India Plate is part of the great Indo-Australian Plate, which underlies the Indian Ocean and Bay of Bengal, and is drifting north-east at an average of 6 cm/year (2 inches per year). The India Plate meets the Burma Plate (which is considered a portion of the great Eurasian Plate) at the Sunda Trench. At this point the India Plate subducts beneath the Burma Plate, which carries the Nicobar Islands, the Andaman Islands, and northern Sumatra. The India Plate sinks deeper and deeper beneath the Burma Plate until the increasing temperature and pressure drive volatiles out of the subducting plate. These volatiles rise into the overlying plate causing partial melting and the formation of magma. The rising magma intrudes into the crust above and exits the Earth's crust through volcanoes in the form of a volcanic arc. The volcanic activity that results as the Indo-Australian Plate subducts the Eurasian Plate has created the Sunda Arc.

As well as the sideways movement between the plates, the sea floor is estimated to have risen by several metres, displacing an estimated 30 km3 (7 cu mi) of water and triggering devastating tsunami waves. The waves did not originate from a point source, as was inaccurately depicted in some illustrations of their paths of travel, but rather radiated outwards along the entire 1,600 km (994 mi) length of the rupture (acting as a line source). This greatly increased the geographical area over which the waves were observed, reaching as far as Mexico, Chile, and the Arctic. The raising of the sea floor significantly reduced the capacity of the Indian Ocean, producing a permanent rise in the global sea level by an estimated 0.1 mm (0.01 cm or 0.0001 m).[16]

Aftershocks and other earthquakes

Locations of initial earthquake and all aftershocks measuring greater than 4.0 from December 26, 2004 to January 10, 2005. The site of the original quake is marked by the large star in the lower right square of the grid.

Numerous aftershocks were reported off the Andaman Islands, the Nicobar Islands and the region of the original epicentre in the hours and days that followed. The largest aftershock, which originated off the coast of the Sumatran island of Nias, registered a magnitude of 8.7,[17] prompting debate among seismologists as to whether it should be classified as an aftershock of the December 2004 quake or as a "triggered earthquake" (which typically differs from an aftershock in that it is not located along the same fault line and may be as large or larger than the earthquake which triggered it).[18] This earthquake was so large that it produced its own aftershocks (some registering a magnitude of as great as 6.1) and presently ranks as the 7th largest earthquake on record since 1900. Other aftershocks of up to magnitude 6.6 continued to shake the region daily for up to three or four months.[19][20] As well as continuing aftershocks, the energy released by the original earthquake continued to make its presence felt well after the event. A week after the earthquake, its reverberations could still be measured, providing valuable scientific data about the Earth's interior.

The 2004 Indian Ocean earthquake came just three days after a magnitude 8.1 earthquake in an uninhabited region west of New Zealand's sub-Antarctic Auckland Islands, and north of Australia's Macquarie Island. This is unusual, since earthquakes of magnitude 8 or more occur only about once per year on average.[21] Some seismologists have speculated about a connection between these two earthquakes, saying that the former one might have been a catalyst to the Indian Ocean earthquake, as the two earthquakes happened on opposite sides of the Indo-Australian Plate. However, the U.S. Geological Survey sees no evidence of a causal relationship in this incident. Coincidentally, the earthquake struck almost exactly one year (to the hour) after a 6.6 magnitude earthquake killed an estimated 30,000 people in the city of Bam in Iran on December 26, 2003.[22]

Some scientists confirm that the December earthquake had activated Leuser Mountain, a volcano in Aceh province along the same range of peaks as Mount Talang, while the 2005 Sumatran earthquake had sparked activity in Lake Toba, an ancient crater in Sumatra.[23] Geologists say that the eruption of Mount Talang in April 2005 is connected to the December earthquake.[24]

Energy released

The energy released on the Earth's surface only (ME, which is the seismic potential for damage) by the 2004 Indian Ocean earthquake and tsunami was estimated at 1.1×1017 joules,[25] or 26.3 megatons of TNT. This energy is equivalent to over 1502 times that of the Hiroshima atomic bomb, but less than that of Tsar Bomba, the largest nuclear weapon ever detonated. However, this is but a tiny fraction of the total work done MW (and thus energy) by this quake, 4.0×1022 joules (4.0×1029 ergs),[26] the vast majority underground. This equates to 4.0×1022 J, over 363,000 times more than its ME. This is a truly enormous figure, equivalent to 9,560 gigatons of TNT equivalent (550 million times that of Hiroshima), or about 370 years of energy use in the United States at 2005 levels of 1.08×1020 J.

The only recorded earthquakes with a larger MW were the 1960 Chilean and 1964 Alaskan quakes, with 2.5×1023 joules (250 ZJ) and 7.5×1022 joules (75 ZJ) respectively.[27]

The earthquake generated a seismic oscillation of the Earth's surface of up to 20–30 cm (8–12 in), equivalent to the effect of the tidal forces caused by the Sun and Moon. The shock waves of the earthquake were felt across the planet; as far away as the U.S. state of Oklahoma, where vertical movements of 3 mm (0.12 in) were recorded. By February 2005, the earthquake's effects were still detectable as a 0.02 mm complex harmonic oscillation of the Earth's surface, which gradually diminished and merged with the incessant free oscillation of the Earth more than 4 months after the earthquake.[28]

Because of its enormous energy release and shallow rupture depth, the earthquake generated remarkable seismic ground motions around the globe, particularly due to huge Rayleigh (surface) elastic waves that exceeded 1 cm in vertical amplitude everywhere on Earth. The record section plot below displays vertical displacements of the Earth's surface recorded by seismometers from the IRIS/USGS Global Seismographic Network plotted with respect to time (since the earthquake initiation) on the horizontal axis, and vertical displacements of the Earth on the vertical axis (note the 1 cm scale bar at the bottom for scale). The seismograms are arranged vertically by distance from the epicenter in degrees. The earliest, lower amplitude, signal is that of the compressional (P) wave, which takes about 22 minutes to reach the other side of the planet (the antipode; in this case near Ecuador). The largest amplitude signals are seismic surface waves that reach the antipode after about 100 minutes. The surface waves can be clearly seen to reinforce near the antipode (with the closest seismic stations in Ecuador), and to subsequently encircle the planet to return to the epicentral region after about 200 minutes. A major aftershock (magnitude 7.1) can be seen at the closest stations starting just after the 200 minute mark. This aftershock would be considered a major earthquake under ordinary circumstances, but is dwarfed by the mainshock.

Vertical-component ground motions recorded by the IRIS/USGS Global Seismographic Network.

The shift of mass and the massive release of energy very slightly altered the Earth's rotation. The exact amount is not yet known, but theoretical models suggest the earthquake shortened the length of a day by 2.68 microseconds, due to a decrease in the oblateness of the Earth.[29] It also caused the Earth to minutely "wobble" on its axis by up to 2.5 cm (1 in) in the direction of 145° east longitude,[30] or perhaps by up to 5 or 6 cm (2.0 to 2.4 in).[31] However, because of tidal effects of the Moon, the length of a day increases at an average of 15 µs per year, so any rotational change due to the earthquake will be lost quickly. Similarly, the natural Chandler wobble of the Earth, which in some cases can be up to 15 m (50 ft), will eventually offset the minor wobble produced by the earthquake.

More spectacularly, there was 10 m (33 ft) movement laterally and 4–5 m (13–16 ft) vertically along the fault line. Early speculation was that some of the smaller islands south-west of Sumatra, which is on the Burma Plate (the southern regions are on the Sunda Plate), might have moved south-west by up to 36 m (118 ft), but more accurate data released more than a month after the earthquake found the movement to be about 20 cm (7.9 in).[32] Since movement was vertical as well as lateral, some coastal areas may have been moved to below sea level. The Andaman and Nicobar Islands appear to have shifted south-west by around 1.25 m (4.1 ft) and to have sunk by 1 m (3.28 ft).[33]

In February 2005, the Royal Navy vessel HMS Scott surveyed the seabed around the earthquake zone, which varies in depth between 1,000 m and 5,000 m (3,300 ft and 16,500 ft). The survey, conducted using a high-resolution, multi-beam sonar system, revealed that the earthquake had made a huge impact on the topography of the seabed. 1,500-meter (5,000 ft) high thrust ridges created by previous geologic activity along the fault had collapsed, generating landslides several kilometers wide. One such landslide consisted of a single block of rock some 100 m high and 2 km long (300 ft by 1.25 mi). The momentum of the water displaced by tectonic uplift had also dragged massive slabs of rock, each weighing millions of tons, as far as 10 km (7 mi) across the seabed. An oceanic trench several kilometres wide was exposed in the earthquake zone.[34]

The TOPEX/Poseidon and Jason 1 satellites happened to pass over the tsunami as it was crossing the ocean.[35] These satellites carry radars that measure precisely the height of the water surface; anomalies of the order of 50 cm (20 in) were measured. Measurements from these satellites may prove invaluable for the understanding of the earthquake and tsunami.[36] Unlike data from tide gauges installed on shores, measurements obtained in the middle of the ocean can be used for computing the parameters of the source earthquake without having to compensate for the complex ways in which close proximity to the coast changes the size and shape of a wave.

Tsunami characteristics

Animation of the tsunami caused by the earthquake showing how the tsunami radiated from the entire length of the 1,600 km (994 mi) rupture.
Scale showing the size of the tsunami waves that hit Indonesia.

The sudden vertical rise of the seabed by several metres during the earthquake displaced massive volumes of water, resulting in a tsunami that struck the coasts of the Indian Ocean. A tsunami which causes damage far away from its source is sometimes called a teletsunami and is much more likely to be produced by vertical motion of the seabed than by horizontal motion.[37]

The tsunami, like all others, behaved very differently in deep water than in shallow water. In deep ocean water, tsunami waves form only a small hump, barely noticeable and harmless, which generally travels at a very high speed of 500 to 1,000 km/h (310 to 620 mph); in shallow water near coastlines, a tsunami slows down to only tens of kilometres an hour, but in doing so forms large destructive waves. Scientists investigating the damage in Aceh found evidence that the wave reached a height of 24 m (79 ft) when coming ashore along large stretches of the coastline, rising to 30 m (98 ft) in some areas when travelling inland.[5]

Radar satellites recorded the heights of tsunami waves in deep water: at two hours after the earthquake, the maximum height was 60 centimetres (2.0 ft). These are the first such observations ever made. Unfortunately these observations could not be used to provide a warning, since the satellites were not built for that purpose and the data took hours to analyze.[38][39]

According to Tad Murty, vice-president of the Tsunami Society, the total energy of the tsunami waves was equivalent to about five megatons of TNT (20 petajoules). This is more than twice the total explosive energy used during all of World War II (including the two atomic bombs), but still a couple of orders of magnitude less than the energy released in the earthquake itself. In many places the waves reached as far as 2 km (1 mi) inland.[40]

Tsunami wave field in the Bay of Bengal one hour after the M=9.2 earthquake. View to the northwest.

Because the 1,600 km (994 mi) fault affected by the earthquake was in a nearly north-south orientation, the greatest strength of the tsunami waves was in an east-west direction. Bangladesh, which lies at the northern end of the Bay of Bengal, had very few casualties despite being a low-lying country relatively near the epicenter. It also benefited from the fact that the earthquake proceeded more slowly in the northern rupture zone, greatly reducing the energy of the water displacements in that region.

Coasts that have a landmass between them and the tsunami's location of origin are usually safe; however, tsunami waves can sometimes diffract around such landmasses. Thus, the Indian state of Kerala was hit by the tsunami despite being on the western coast of India, and the western coast of Sri Lanka also suffered substantial impacts. Also distance alone was no guarantee of safety; Somalia was hit harder than Bangladesh despite being much farther away.

Because of the distances involved, the tsunami took anywhere from fifteen minutes to seven hours (for Somalia) to reach the various coastlines.[41][42] The northern regions of the Indonesian island of Sumatra were hit very quickly, while Sri Lanka and the east coast of India were hit roughly 90 minutes to two hours later. Thailand was also struck about two hours later despite being closer to the epicentre, because the tsunami travelled more slowly in the shallow Andaman Sea off its western coast.

The tsunami was noticed as far as Struisbaai in South Africa, some 8,500 km (5,282 mi) away, where a 1.5 m (5 ft) high tide surged on shore about 16 hours after the earthquake. It took a relatively long time to reach this spot at the southernmost point of Africa, probably because of the broad continental shelf off South Africa and because the tsunami would have followed the South African coast from east to west. The tsunami also reached Antarctica, where tidal gauges at Japan's Showa Base recorded oscillations of up to a metre, with disturbances lasting a couple of days.[43]

Some of the tsunami's energy escaped into the Pacific Ocean, where it produced small but measurable tsunamis along the western coasts of North and South America, typically around 20 to 40 cm (7.9 to 15.7 in).[44] At Manzanillo, Mexico, a 2.6 m (8.5 ft) crest-to-trough tsunami was measured. As well, the tsunami was large enough to be detected in Vancouver, British Columbia, Canada. This puzzled many scientists, as the tsunamis measured in some parts of South America were larger than those measured in some parts of the Indian Ocean. It has been theorized that the tsunamis were focused and directed at long ranges by the mid-ocean ridges which run along the margins of the continental plates.[45]

Signs and warnings

Maximum recession of tsunami waters at Kata Noi Beach, Thailand, before the third, and strongest, tsunami wave (sea visible in the right corner, the beach is at the extreme left), 10:25 a.m. local time.

Despite a lag of up to several hours between the earthquake and the impact of the tsunami, nearly all of the victims were taken completely by surprise. There were no tsunami warning systems in the Indian Ocean to detect tsunamis or to warn the general populace living around the ocean. Tsunami detection is not easy because while a tsunami is in deep water it has little height and a network of sensors is needed to detect it. Setting up the communications infrastructure to issue timely warnings is an even bigger problem, particularly in a relatively poor part of the world.

Tsunami are much more frequent in the Pacific Ocean because of earthquakes in the "Ring of Fire", and an effective tsunami warning system has long been in place there. Although the extreme western edge of the Ring of Fire extends into the Indian Ocean (the point where this earthquake struck), no warning system exists in that ocean. Tsunamis there are relatively rare despite earthquakes being relatively frequent in Indonesia. The last major tsunami was caused by the Krakatoa eruption of 1883. It should be noted that not every earthquake produces large tsunamis; on March 28, 2005, a magnitude 8.7 earthquake hit roughly the same area of the Indian Ocean but did not result in a major tsunami.

In the aftermath of the disaster, there is now an awareness of the need for a tsunami warning system for the Indian Ocean. The United Nations started working on an Indian Ocean Tsunami Warning System and by 2005 had the initial steps in place. Some have even proposed creating a unified global tsunami warning system, to include the Atlantic Ocean and Caribbean.

The first warning sign of a possible tsunami is the earthquake itself. However, tsunami can strike thousands of kilometres away where the earthquake is only felt weakly or not at all. Also, in the minutes preceding a tsunami strike, the sea often recedes temporarily from the coast. Around the Indian Ocean, this rare sight reportedly induced people, especially children, to visit the coast to investigate and collect stranded fish on as much as 2.5 km (1.6 mi) of exposed beach, with fatal results.[46] However, not all tsunami causes this "disappearing sea" effect. In some cases, there are no warning signs at all: the sea will suddenly swell without retreating, surprising many people and giving them little time to flee.

One of the few coastal areas to evacuate ahead of the tsunami was on the Indonesian island of Simeulue, very close to the epicentre. Island folklore recounted an earthquake and tsunami in 1907, and the islanders fled to inland hills after the initial shaking yet before the tsunami struck.[47] On Maikhao beach in northern Phuket, Thailand, a 10-year-old British tourist named Tilly Smith had studied tsunami in geography class at school and recognised the warning signs of the receding ocean and frothing bubbles. She and her parents warned others on the beach, which was evacuated safely.[48] John Chroston, a biology teacher from Scotland, also recognised the signs at Kamala Bay north of Phuket, taking a busload of vacationers and locals to safety on higher ground.

Anthropologists had initially expected the aboriginal population of the Andaman Islands to be badly affected by the tsunami and even feared the endangered Onge tribe could have been wiped out. Of the six native tribes only the Nicobarese, who had converted to Christianity and taken up agriculture in place of their previous hunter-gatherer lifestyle, and mainland settlers suffered significant losses.[49] Many of the aboriginal tribes evacuated and suffered fewer casualties.[50][51]

Phases and wave form

USGS graphics showing the wave structure of the 2004 Indian Ocean tsunami. Red indicate a positive wave form while blue represent a negative wave form.

A tsunami can arrive at a coastline in one of two ways. First, there's the negative wave where the trough of the wave precedes the actual arrival of the crest or "wave" itself. Here, the common and better known warning sign of an impending tsunami strike is a rapidly receding sea followed by a sudden onrushing body of water traveling inland at high speed.

The second form in which a tsunami arrives is the positive wave or crest first. In this case, the warning signs are much more vague if any. The sea will usually start rising immediately rather slowly at first without the receding phase, much more like an on-coming high tide but instead of stopping at tidal level it will keep on rising faster and faster until the crest of the tsunami passes and continues moving inland. Therefore, the second form of tsunami waves are usually more dangerous owing to the fact that it can arrive without much warning giving residents less time to prepare and outrun the tsunami. These two types of tsunamis are usually generated simultaneously (in opposing direction of travel) by a megathrust earthquake similar to the 2004 Indian Ocean earthquake.

Retreat-rise cycle (negative wave)

The tsunami was a succession of several waves, occurring in retreat and rise cycles with a period of over 30 minutes between each peak. The third wave was the most powerful and reached highest, occurring about an hour and a half after the first wave. Smaller tsunami continued to occur for the rest of the day.[citation needed]

Rise-retreat-rise cycle (positive wave)

If the crest of a tsunami arrives first, there won't be any recession. The sea level will increase rapidly to inundate everything in the path of the tsunami. This appears to be the case in countries such as Sri Lanka and India that lies to the west of the Andaman-Sumatra fault where the tsunami originates. After the first tsunami wave passed, water will then begin to flow back into the ocean receding at a quicker pace as the second wave arrives.[citation needed]

Death toll and casualties

Chennai's Marina beach after the tsunami.

According to the U.S. Geological Survey a total of 227,898 people died (see table below for details).[52] Measured in lives lost, this is one of the ten worst earthquakes in recorded history, as well as the single worst tsunami in history. Indonesia was the worst affected area, with most death toll estimates at around 170,000.[53] However, another report by health minister Fadilah Supari has estimated the death total to be as high as 220,000 in Indonesia alone, giving a total of 280,000 casualties.[54]

The tsunami caused serious damage and deaths as far as the east coast of Africa, with the furthest recorded death due to the tsunami occurring at Rooi Els in South Africa, 8,000 km (4,971 mi) away from the epicentre. In total, eight people in South Africa died due to abnormally high sea levels and waves.

Relief agencies report that one-third of the dead appear to be children. This is a result of the high proportion of children in the populations of many of the affected regions and because children were the least able to resist being overcome by the surging waters. Oxfam went on to report that as many as four times more women than men were killed in some regions because they were waiting on the beach for the fishermen to return and looking after their children in the houses.[55]

In addition to the large number of local residents, up to 9,000 foreign tourists (mostly Europeans) enjoying the peak holiday travel season were among the dead or missing, especially people from the Nordic countries. The European nation hardest hit may have been Sweden, whose death toll was 543.[56]

States of emergency were declared in Sri Lanka, Indonesia, and the Maldives. The United Nations estimated at the outset that the relief operation would be the costliest in human history. Then UN Secretary-General Kofi Annan stated that reconstruction would probably take between five and ten years. Governments and non-governmental organisations feared that the final death toll might double as a result of diseases, prompting a massive humanitarian response. In the end, this fear did not materialise.

For purposes of establishing timelines of local events, the time zones of affected areas are: UTC+3: (Kenya, Madagascar, Somalia, Tanzania); UTC+4: (Mauritius, Réunion, Seychelles); UTC+5: (Maldives); UTC+5:30: (India, Sri Lanka); UTC+6: (Bangladesh); UTC+6:30: (Cocos Islands, Myanmar); UTC+7: (Indonesia (western), Thailand); UTC+7: (Malaysia, Singapore). Since the earthquake occurred at 00:58:53 UTC, add the above offsets to find the local time of the earthquake.

Country where
deaths occurred
Deaths Injured Missing Displaced
Confirmed Estimated1
Indonesia 130,736 167,736 N/A 37,063[57] 500,000+[58]
Sri Lanka2 35,322[59] 35,322 21,411[59] N/A 516,150[59]
India 12,405 18,045 N/A 5,640 647,599
Thailand 5,3953[60] 8,212 8,457[61] 2,817[60] 7,000
Somalia 78 289[62] N/A N/A 5,000[63]
Myanmar (Burma) 61[57] 400–600[64] 45 200[65] 3,200
Maldives 82[66] 108[67] N/A 26 15,000+
Malaysia 68[68] 75 299[69] 6 N/A
Tanzania 10[70] 13 N/A N/A N/A
Seychelles 3[71] 3 57[71] N/A 200[72]
Bangladesh 2 2 N/A N/A N/A
South Africa 24[73] 2 N/A N/A N/A
Yemen 2[74] 2 N/A N/A N/A
Kenya 1 1 2 N/A N/A
Madagascar N/A N/A N/A N/A 1,000+[75]
Total ~184,167 ~230,210 ~125,000 ~45,752 ~1.69 million

Note: All figures are approximate and subject to change. The first column links to more details on specific countries.
1 Includes those reported under 'Confirmed'. If no separate estimates are available, the number in this column is the same as reported under 'Confirmed'.
2 Does not include approximately 19,000 missing people initially declared by Tamil Tiger authorities from regions under their control.
3 Data includes at least 2,464 foreigners.
4 Does not include South African citizens who died outside of South Africa (e.g., tourists in Thailand). For more information on those deaths, see this


Countries affected

Countries most affected by the tsunami, with the earthquake's epicenter.

The earthquake and resulting tsunami affected many countries in Southeast Asia and beyond, including Indonesia, Sri Lanka, India, Thailand, the Maldives, Somalia, Myanmar, Malaysia, Seychelles and others. Many other countries, especially Australia and those in Europe, had large numbers of citizens traveling in the region on holiday. Both Sweden and Germany lost over 500 citizens each in the disaster.

Event in historical context

This earthquake was the biggest in the Indian Ocean in some 700 years, or since around A.D. 1400.[76][77][78] In 2008, a team of scientists working on Phra Thong, a barrier island along the hard-hit west coast of Thailand, reported evidence of at least three previous major tsunamis in the preceding 2,800 years, the most recent from about 550 to 700 years ago. A second team found similar evidence of previous tsunamis during the last 1,200 years in Aceh, a province at the northern tip of Sumatra. Radiocarbon dating of bark fragments in soil below the second sand layer led the scientists to estimate that the most recent predecessor to the 2004 tsunami probably occurred between A.D. 1300 and 1450.[79]

Deadliest earthquakes[1]
Rank↓ Name↓ Date↓ Location↓ Fatalities↓ Magnitude↓ Comments↓
1 "Shaanxi" 01556-01-231556-01-23 Shaanxi, China 820,000– 830,000 (est.)[80] 8.0 Estimated death toll in Shaanxi, China.
2 "Tangshan" 01976-07-281976-07-28 Tangshan, China 242,419– 779,000 7.5 Estimated death toll as high as 779,000.
3 "Antioch" 00525-05-21525-05-21 Antioch, Turkey 250000 [81] VIII Procopius (II.14.6), sources based on John of Ephesus.
4 "Gansu" 01920-12-161920-12-16 NingxiaGansu, China 235,502[82] 7.8 Major fractures, landslides.
5 "Aleppo" 01138-10-111138-10-11 Aleppo, Syria 230,000 8.5 The figure of 230,000 dead is based on a historical conflation of this earthquake with earthquakes in November 1137 on the Jazira plain and the large seismic event of 30 September 1139 in the Azerbaijani city of Ganja. The first mention of a 230,000 death toll was by Ibn Taghribirdi in the fifteenth century.[83]
6 "Indian Ocean" 02004-12-262004-12-26 Sumatra, Indonesia 230,000+[84][2] 9.1 Deaths from earthquake and resulting tsunami.
7 "Haiti" 02010-01-122010-01-12 Haiti 222,570 7.0 Estimate June 2010.[85]
8 "Great Kantō" 01923-09-011923-09-01 Kantō region, Japan 142,000 7.9 An earthquake which struck the Kantō plain on the Japanese main island of Honshū at 11:58 on the morning of September 1, 1923. Varied accounts hold that the duration of the earthquake was between 4 and 10 minutes. The quake had an epicenter deep beneath Izu Ōshima Island in Sagami Bay. It devastated Tokyo, the port city of Yokohama, surrounding prefectures of Chiba, Kanagawa, and Shizuoka, and caused widespread damage throughout the Kantō region.[86] The power and intensity of the earthquake is easy to underestimate, but the 1923 earthquake managed to move the 93-ton Great Buddha statue at Kamakura. The statue slid forward almost two feet.[87] Casualty estimates range from about 100,000 to 142,000 deaths, the latter figure including approximately 40,000 who went missing and were presumed dead.
9 "Ashgabat" 01948-10-061948-10-06 Ashgabat, Turkmenistan 110,000 7.3
10 "Genroku" 01703-12-311703-12-31 Edo 108,800+ 8 This earthquake shook Edo and killed an estimated 2,300 people. The earthquake is thought to have been an interplate earthquake whose focal region extended from Sagami Bay to the tip of the Bōsō Peninsula as well as the area along the Sagami Trough in the open sea southeast of the Boso Peninsula. This earthquake then resulted in a tsunami which hit the coastal areas of the Boso Peninsula and Sagami Bay. This caused more than 6,500 deaths, particularly on the Boso Peninsula. The Habu Pond on Izu Ōshima collapsed and it rushed into the sea. The tsunami was reported to have caused more than 100,000 fatalities.
11 "Lisbon" 01755-11-011755-11-01 Lisbon, Portugal 10,000–
100,000
7.3 Includes several thousands of deaths in Morocco and Spain


This earthquake was the third most powerful earthquake recorded since 1900, and the confirmed death toll is just under 200,000 due to the ensuing tsunami. The deadliest earthquakes since 1900 were the Tangshan, China earthquake of 1976, in which at least 255,000 were killed; the earthquake of 1927 in Xining, Qinghai, China (200,000); the Great Kanto earthquake which struck Tokyo in 1923 (143,000); and the Gansu, China, earthquake of 1920 (200,000). The deadliest known earthquake in history occurred in 1556 in Shaanxi, China, with an estimated death toll of 830,000, though figures from this time period may not be reliable.[88]

The 2004 tsunami is the deadliest in recorded history. Prior to 2004, the deadliest recorded tsunami in the Pacific Ocean was in 1782, when 40,000 people were killed by a tsunami in the South China Sea.[89] The tsunami created by the 1883 eruption of Krakatoa is thought to have resulted in 36,000 deaths. The most deadly tsunami between 1900 and 2004 occurred in 1908 in Messina, Italy, on the Mediterranean Sea, where the earthquake and tsunami killed 70,000. The most deadly tsunami in the Atlantic Ocean resulted from the 1755 Lisbon earthquake, which, combined with the toll from the actual earthquake and resulting fires, killed over 100,000.

The 2004 earthquake and tsunami combined have been described as the deadliest natural disaster since either the 1976 Tangshan earthquake or the 1970 Bhola cyclone, or could conceivably exceed both of these. Because of uncertainty over death tolls, it might never be known for sure which of these natural disasters was the deadliest.

Possible human component in magnitude of damage

A town near the coast of Sumatra lies in ruin on January 2, 2005. This picture was taken by a United States military helicopter crew from the USS Abraham Lincoln that was conducting humanitarian operations.
Indonesians gather under an approaching helicopter to receive food and supplies.

In an opinion piece in the Wall Street Journal, published five days after the tsunami, a journalist, Andrew Browne, argued that the human destruction of coral reefs may have played a role in exacerbating the destruction caused by the tsunami. Many countries across Asia, including Indonesia, Sri Lanka and Bangladesh, have put forth efforts to destroy the coral surrounding their beaches, and instead make way for shrimp farms and other economic choices. On the Surin Island chain of Thailand's coast, Browne argued, people may have been saved as the tsunami rushed against the coral reefs, lessening its impact. However, there were many fewer people on these islands, which helps explain the lower death toll. Many reefs areas around the Indian Ocean have been exploded with dynamite because they are considered impediments to shipping, an important part of the South Asian economy.[90] Similarly, Browne argued that the removal of coastal mangrove trees may have intensified the effect of the tsunami in some locations. He argued that these trees, which lined the coast but were removed to make way for coastal residences, might have lessened the force of the tsunami, in certain areas. Another factor, Browne argued, is the removal of coastal sand dunes.[90]

Humanitarian, economic and environmental impact

A great deal of humanitarian aid was needed because of widespread damage of the infrastructure, shortages of food and water, and economic damage. Epidemics were of special concern due to the high population density and tropical climate of the affected areas. The main concern of humanitarian and government agencies was to provide sanitation facilities and fresh drinking water to contain the spread of diseases such as cholera, diphtheria, dysentery, typhoid and hepatitis A and B.

There was also a great concern that the death toll could increase as disease and hunger spread. However, because of the initial quick response, this was minimized.[91]

In the days following the tsunami, significant effort was spent in burying bodies hurriedly for fear of disease. However, the public health risks may have been exaggerated, and therefore this may not have been the best way to allocate resources. The World Food Programme provided food aid to more than 1.3 million people affected by the tsunami.[92]

Nations all over the world provided over US$ 14 billion in aid for damaged regions[93], with the governments of Australia pledging US$819.9 million (including a US$760.6-million aid package for Indonesia), Germany offering US$660 million, Japan offering US$500 million, Canada offering US$343 million, Norway and the Netherlands offering both US$183 million, the United States offering US$35 million initially (increased to US$350 million), and the World Bank offering US$250 million. Also Italy offered US$95 million, increased later to US$113 million of which US$42 million was donated by the population using the SMS system[94] According to USAID, the US has pledged additional funds in long-term U.S. support to help the tsunami victims rebuild their lives. On February 9, 2005, President Bush asked Congress to increase the U.S. commitment to a total of $950 million. Officials estimated that billions of dollars would be needed. Bush also asked his father, former President George H. W. Bush, and former President Bill Clinton to lead a U.S. effort to provide private aid to the tsunami victims.[95]

In mid-March the Asian Development Bank reported that over US$4 billion in aid promised by governments was behind schedule. Sri Lanka reported that it had received no foreign government aid, while foreign individuals had been generous.[96] Many charities were given considerable donations from the public. For example, in the UK the public donated roughly £330,000,000 sterling (nearly US$600,000,000). This considerably outweighed the donation by the government and came to an average of about £5.50 (US$10) donated by every citizen.

In August 2006, fifteen local aid staff working on post-tsunami rebuilding were found executed in northeast Sri Lanka after heavy fighting, the main umbrella body for aid agencies in the country said. There had been reports and rumors that the local aid workers had been killed.

Economic impact

The impact on coastal fishing communities and fisherfolk, some of the poorest people in the region, has been devastating with high losses of income earners as well as boats and fishing gear.[97] In Sri Lanka artisanal fishery, where the use of fish baskets, fishing traps, and spears are commonly used, is an important source of fish for local markets; industrial fishery is the major economic activity, providing direct employment to about 250,000 people. In recent years the fishery industry has emerged as a dynamic export-oriented sector, generating substantial foreign exchange earnings. Preliminary estimates indicate that 66% of the fishing fleet and industrial infrastructure in coastal regions have been destroyed by the wave surges, which will have adverse economic effects both at local and national levels.[98]

The tsunami created demand for fiberglass reinforced plastic catamarans in boatyards of Tamil Nadu.[99]

But some economists believe that damage to the affected national economies will be minor because losses in the tourism and fishing industries are a relatively small percentage of the GDP. However, others caution that damage to infrastructure is an overriding factor. In some areas drinking water supplies and farm fields may have been contaminated for years by salt water from the ocean.[100]

Both the earthquake and the tsunami may have affected shipping in the Malacca Straits by changing the depth of the seabed and by disturbing navigational buoys and old shipwrecks. Compiling new navigational charts may take months or years.[101]

Countries in the region appealed to tourists to return, pointing out that most tourist infrastructure is undamaged. However, tourists were reluctant to do so for psychological reasons. Even beach resorts in parts of Thailand which were completely untouched by the tsunami were hit by cancellations.[102]

Environmental impact

Tsunami inundation, Khao Lak, North of Phuket, Thailand ASTER Images and SRTM Elevation Model.

Beyond the heavy toll on human lives, the Indian Ocean earthquake has caused an enormous environmental impact that will affect the region for many years to come. It has been reported that severe damage has been inflicted on ecosystems such as mangroves, coral reefs, forests, coastal wetlands, vegetation, sand dunes and rock formations, animal and plant biodiversity and groundwater. In addition, the spread of solid and liquid waste and industrial chemicals, water pollution and the destruction of sewage collectors and treatment plants threaten the environment even further, in untold ways. The environmental impact will take a long time and significant resources to assess.[103]

According to specialists, the main effect is being caused by poisoning of the freshwater supplies and the soil by saltwater infiltration and deposit of a salt layer over arable land. It has been reported that in the Maldives, 16 to 17 coral reef atolls that were overcome by sea waves are totally without fresh water and could be rendered uninhabitable for decades. Uncountable wells that served communities were invaded by sea, sand and earth; and aquifers were invaded through porous rock. Salted-over soil becomes sterile, and it is difficult and costly to restore for agriculture. It also causes the death of plants and important soil micro-organisms. Thousands of rice, mango and banana plantations in Sri Lanka were destroyed almost entirely and will take years to recover. The United Nations Environment Programme (UNEP) is working with governments of the region in order to determine the severity of the ecological impact and how to address it.[104] UNEP has decided to earmark a US$1,000,000 emergency fund and to establish a Task Force to respond to requests for technical assistance from countries affected by the tsunami.[105] In response to a request from the Maldivian Government, the Australian Government sent ecological experts to help restore marine environments and coral reefs—the lifeblood of Maldivian tourism. Much of the ecological expertise has been rendered from work with the Great Barrier Reef, in Australia's northeastern waters.

Other effects

A note signed by George W. Bush, then President of the United States, his wife Laura Bush, and former Presidents George H. W. Bush and Bill Clinton, expressing their condolences during a visit to the embassy of Sri Lanka in Washington, D.C., Monday, January 3, 2005. The President wrote, "We pray for the victims and families of this epic disaster. And the American government and American people are dedicated to helping you recover."

Many health professionals and aid workers have reported widespread psychological trauma associated with the tsunami. Traditional beliefs in many of the affected regions state that a relative of the family must bury the body of the dead, and in many cases, no body remained to be buried.

The hardest hit area, Aceh, is considered to be a religiously conservative Islamic society and has had no tourism nor any Western presence in recent years due to armed conflict between the Indonesian military and Acehnese separatists. Some believe that the tsunami was divine punishment for lay Muslims shirking their daily prayers and/or following a materialistic lifestyle. Others have said that Allah was angry that there were Muslims killing other Muslims in an ongoing conflict.[106] Women in Aceh required a special approach from foreign aid agencies, and continue to have unique needs.

The widespread devastation caused by the tsunami led the main rebel group GAM to declare a cease-fire on December 28, 2004, followed by the Indonesian government, and the two groups resumed long-stalled peace talks, which resulted in a peace agreement signed August 15, 2005. The agreement explicitly cites the tsunami as a justification.[107]

The extensive international media coverage of the tsunami, and the role of mass media and journalists in reconstruction, were discussed by editors of newspapers and broadcast media in tsunami-affected areas, in special video-conferences set up by the Asia Pacific Journalism Centre.[108]

The December 26, 2004 Asian Tsunami left both the people and government of India in a state of heightened alert. On December 30, 2004, four days after the tsunami, the Portland, Oregon-based company Terra Research notified the India government that its sensors indicated there was a possibility of 7.9 to 8.1 magnitude tectonic shift in the next 12 hours between Sumatra and New Zealand.[109] In response, the India Home Affairs minister announced that a fresh onslaught of deadly tidal waves were likely along the India southern coast and Andaman and Nicobar Islands, even as there was no sign of turbulences in the region.[109] The announcement generated panic in the Indian Ocean region and caused thousands to flee their homes, which resulted in jammed roads.[110] The announcement was a false alarm and the Home Affairs minister withdrew their announcement.[110] On further investigation, the India government learned that the consulting company Terra Research was run from the home of a self-described earthquake forecaster who had no telephone listing and maintained a website where he sold copies of his detection system.[111] Three days after the announcement, Indian National Congress president Sonia Gandhi called Science & Technology minister Kapil Sibal to express her concern about Sibal's December 30 public warning being "hogwash".[112]

Another result of the tsunami, respective toward Indian culture, was the water that washed away centuries of sand from some of the ruins of a 1,200-year-old lost city at Mahabalipuram on the south coast of India. The site, containing such notable structures as a half-buried granite lion near a 7th century Mahablipuram temple and a relic depicting an elephant, is part of what archaeologists believe to be an ancient port city that was swallowed by the sea hundreds of years ago.[113][114]

The tsunami had a severe humanitarian and political impact in Sweden. The hardest hit country outside Asia, 543 Swedish tourists, mainly in Thailand, died. With no single incident having killed more Swedish people since the battle of Poltava in 1709, the cabinet of Göran Persson was heavily criticized for lack of action. The event was examined by an independent inquiry, Katastrofkommissionen.[citation needed]

See also


Notes

  1. ^ If the death toll in Myanmar was 400–600 as claimed by dissident groups there, rather than just 61 or 90, more than 230,000 people would have perished in total from the tsunami.
  2. ^ a b "Myanmar is withholding true casualties figures, says Thai priest". A missioner in Ranong, a town on the border between Thailand and Myanmar, says locals talk about 600 victims. Burmese political dissidents say the same. AsiaNews.it. January 4, 2005. Retrieved 2006-05-07.
  3. ^ Lay, T., Kanamori, H., Ammon, C., Nettles, M., Ward, S., Aster, R., Beck, S., Bilek, S., Brudzinski, M., Butler, R., DeShon, H., Ekström, G., Satake, K., Sipkin, S., The Great Sumatra-Andaman Earthquake of December 26, 2004, Science, 308, 1127–1133, doi:10.1126/science.1112250, 2005
  4. ^ "Tsunamis and Earthquakes: Tsunami Generation from the 2004 Sumatra Earthquake - USGS Western Coastal and Marine Geology". Walrus.wr.usgs.gov. http://walrus.wr.usgs.gov/tsunami/sumatraEQ/. Retrieved 2010-08-12. 
  5. ^ a b Paulson, Tom. "New findings super-size our tsunami threat." Seattlepi.com. February 7, 2005.
  6. ^ Walton, Marsha. "Scientists: Sumatra quake longest ever recorded." CNN. May 20, 2005
  7. ^ West, Michael; Sanches, John J.; McNutt, Stephen R. "Periodically Triggered Seismicity at Mount Wrangell, Alaska, After the Sumatra Earthquake." Science. Vol. 308, No. 5725, 1144–1146. May 20, 2005.
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