The tsunami disaster

Authors Avatar

The tsunami disaster

At 0059 GMT on 26 December 2004, a magnitude 9.3 earthquake ripped apart the seafloor off the coast of northwest Sumatra.

Over 100 years of accumulated stress was released in the second biggest earthquake in recorded history.

It unleashed a devastating tsunami that travelled thousands of kilometres across the Indian Ocean, taking the lives of nearly 300,000 people in countries as far apart as Indonesia, the Maldives, Sri Lanka and Somalia.  

THE EARTHQUAKE

Two hundred and forty kilometres (150 miles) off the coast of Sumatra, deep under the ocean floor, at the boundary between two of the world's tectonic plates, lay a 1,200km (745 miles) trench called the Andaman-Sumatran subduction zone.

At about the same speed as your fingernails grow, the lower plate, carrying India, is being forced or subducted beneath the upper plate, carrying most of South-East Asia, dragging it down, causing huge stresses to build up.

These stresses were released on 26 December. Shaking from this giant mega-thrust earthquake woke people from sleep as far away as Thailand and the Maldives.

Unlike the more frequent strike-slip earthquakes of Kobe or Los Angeles, which last for a matter of seconds, subduction zone quakes last for several minutes.

Join now!

The shaking during the Indonesian event went on for eight minutes.

Nobody knows how many died in the actual quake itself, but scientists have since visited the nearby island of Simueleu and found something astonishing.

The whole island has been tilted by the force of the earthquake, causing coral, submerged beneath the ocean for thousands of years, to be thrust out of the water on the east side; bays in the west have been drained.

"We were astonished to find ourselves walking through a pristine marine ecosystem, missing only its multitude of colours, its fish, and its ...

This is a preview of the whole essay