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2004 Sumatra Earthquake – Geographic
Aftermath of the Sumatra earthquake and tsunami on December 26, 2004 in Banda Aceh, Indonesia.
by Victoria Heath
On Boxing Day 2004, a magnitude 9.1 earthquake was recorded off the coast of Sumatra, Indonesia. A 900-mile stretch of fault line where the Indian and Australian tectonic plates meet has been torn apart, causing the ocean floor to rise about 40 meters. Also known as the Sumatra-Andaman earthquake, the disaster triggered the deadliest tsunami on record.
In the aftermath of the Sumatra earthquake and tsunami in Indonesia
The resulting tsunami occurred within just 20 minutes of the Sumatra earthquake. 100-foot waves hit the beaches of Banda Aceh in Indonesia, killing more than 100,000 people.
The western part of Banda Aceh has an almost flat terrain. The waves in these areas reached between 4-8 metres, reaching greater numbers in the mountainous areas south of Banda Aceh.
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If buildings in the area survived the initial shaking caused by the earthquake, most of them would have been destroyed by tsunamis. Debris from the impact of three successive tsunami waves caused large projectile impacts such as cars, trucks, and boats to previously undamaged facilities. Buttresses blocking roads and bridges were swept away and hundreds of bridges destroyed.
Mount Sinabung in North Sumatra, Indonesia, about 400 miles from the city of Banda Aceh where the tsunami triggered by the Sumatra earthquake struck. Image: shutterstock
According to the United Nations field office, nearly 131,000 people are confirmed dead and 37,000 people are missing in the North Aceh province of Sumatra. Eighty thousand homes were severely damaged or completely collapsed, and more than 500 thousand people in Sumatra were displaced from their homes.
Tsunami effect elsewhere
The devastation quickly spread to the coasts of Thailand, India and Sri Lanka, as tsunamis moved across the Indian Ocean at 500 miles per hour. Eight hours after the earthquake, more than 5,000 miles away, a tsunami hit the coast of South Africa. In total, the disaster killed nearly 230,000 people in 14 countries.
What caused the earthquake and tsunami?
The earthquake, known as a massive bottom earthquake, occurred as a result of the sliding of a heavy ocean plate under a lighter continental plate. The disaster was caused by the subduction of the India Plate (which was forced under) the delicate Burma Plate, which forms part of the larger Sunda Plate.
Children outside their destroyed home following the Sumatra earthquake and tsunami in Lokanja, Aceh, Indonesia. Photo: France Delien/Shutterstock
It is estimated that the earthquake itself released energy equivalent to 23,000 Hiroshima-type atomic bombs, and was so large that the planet’s rotation changed as the Earth’s mass changed.
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Learning from the Sumatra earthquake
Three weeks after the tsunami, representatives of 168 countries agreed to the Hyogo Framework for Action which encouraged global support and cooperation for disaster risk reduction.
The Indonesian government, NGOs, donors and individuals have contributed nearly $7 billion. In Aceh, the government has established a high-ranking office to organize recovery work.
At the time of the disaster, there was no official tsunami warning system, with the last major tsunami occurring in 1883. Some small island communities had information about tsunamis from tsunami stories passed down through generations, which helped prevent further loss of life.
However, other witnesses came to the water to explore the ocean floor, or went about their daily activities. Although there were signs such as the sea withdrawing, and unusually large (but not harmful) waves, they were not widely understood as warnings.
An earthquake and tsunami detector installed since 2005 in Aceh, Indonesia
To detect and warn of underwater earthquakes sooner, earthquake sensors have been installed on the ocean floor, along with training for communities in disaster response and evacuation. Now, National Tsunami Warning Centers have also been set up in the countries of the Indian Ocean region which can help alert citizens of impending disasters.
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