The Indian Ocean Tsunami (also known as the ‘Boxing Day Tsunami’) was a catastrophic event that occurred on December 26th 2004.

At 07.58 local time an earthquake measuring 9.3 and lasting 8-10 minutes – the the longest in time and third largest in force ever recorded – struck in the ocean near Sumatra, Indonesia. The tsunamis this triggered struck at least 14 countries. It’s exact death toll is unknown, but general estimates range from 250 000 to 300 000+ people.

Forshadowing Disaster

On November 2nd 2002 an earthquake measuring 7.3 hit near Sumatra, Indonesia. Only 3 people died. However, the movement of the plates had left them badly out of line.

The Scale of the Earthquake

The quake involved two ruptures of the earth’s surface: the first 400km long followed by another 100 seconds later. The area releasing energy was 160km long. The fault slipped 15m and it is believed the whole earth vibrated 1cm.

The one earthquake accounted for 1/8th of all seismic activity in the hundred years to that date. If added together, the Chilean earthquake of 1960, Alaskan earthquake of 1964, and Sumatra earthquake of 2004 accounted for 1/2 of seismic movement in the previous 100 years.

Timeline

00.58 GMT (07.58 Indonesia): The first earthquake strikes off Sumatra and is felt in several countries. It is initially measured at 8.9. Although there is a Pacific Tsunami Warning Center (PTWC), none of the countries in the region are a part of it.

01.00 – 01.30GMT (08.00-08.30 Indonesia): The tsunami hits north of Indonesia, including Banda Aceh. Tsunami waves also hit India’s Nicobar and Andaman Islands.

02.30 GMT: Beaches in Thailand are hit by the tsunami, killing locals and tourists.

03.00 – 03.23 GMT: The tsunami reaches India and Sri Lanka.

04.00 GMT: The Maldives is the next country hit by the wave.

07.00 GMT: The tsunami reaches its final countries on the east of Africa.

A Failure in Warning Systems

There were earthquake and tsunami warning centers set up around the Pacific, but they were run by developed countries and did not connect to the poorer nations that were hit. For most people the only warning they got before the wave was the sea retreating and divers reporting strong currents and no fish.

By the time the US system in Hawaii and the Australian system in the north of the country understood what was happening, the damage in Indonesia, Sri Lanka, India and Thailand had already been done.

Deaths and Damage

It is impossible to know the exact number of people who died because of the Indian Ocean Tsunami: the wide area the disaster hit, and the poverty of some of many areas, means there is some guesswork. For example, the US Geological Survey initially estimated 227 000 people died, but the Indonesian Government puts the death toll in Indonesia alone at 220 000.

Wikipedia states the approximate death tolls per country as follows:

Indonesia: 168000

Sri Lanka: 35000

India: 18000

Thailand: 8000

Myanmar: 600

Somalia: 289

Maldives: 108

Many other countries suffered less than 100 deaths.

The tsunami also resulted in widescale environmental destruction, with habitats destroyed, plantations lost, drinking water contaminated, and waste and chemicals spread over a large area. It is impossible to know the damage to animal life and ecosystems in the area.

Rebuilding and Continued Threat

International aid poured into the region to help the humanitarian effort. However it will take generations to rebuild the areas and families hit.

In 2005 the plates near Sumatra moved again – causing an 8.7 quake, the 7th largest since 1900.

 

 

Further Reading: What creates a tsunami?

The process that creates a tsunami is as follows:

1. An earthquake on the ocean floor creates a wave of energy called a ‘Rayleigh Wave’. Although the push of energy can be very fast – sometimes faster than the speed of sound – the important part is the length of the wave: this energy wave can go for hundreds of kilometres.

2. This energy wave pushes a huge amount of water forward; essentially tens or hundreds of kilometres of water are all being pushed forwards at the same time in one long wave.

3.  If there was no land to slow or stop this wave of energy and water it could travel around the world several times. However, as it comes to land the front of the wave slows. The water at the back of the wave helps push the front of the wave upwards.  The longer the wave of water moving forward, the more water pushing the wave upwards.

4. An unusual thing about tsunamis is the habit of making water ‘disappear’ from the beach before it hits. The theory to why this happens is the same as the ‘undertow’ a normal wave experiences: water pulling back into the space beneath a wave as it rises. As a tsunami wave is rising to great heights it draws a lot of water beneath it.

Tsunamis can occur in any area where a fault line lies beneath the ocean, but are most common on the Asian side of the Pacific Ocean (‘The Pacific Rim’).