On the 26th
December 2004 one of the largest earthquakes in the last century struck off the
west coast of Sumatra. This resulted in one of the largest
tsunamis seen in modern times affecting many countries surrounding the Indian
Ocean including Indonesia, Sri Lanka, Thailand, Malaysia, India and Eastern
Africa. It was the deadliest tsunami in recorded history killing over 220,000
people. Many bodies were lost at sea or buried in mass graves and not
recorded meaning an accurate number will never been known. This disaster opened the world’s eyes to how destructive natural disasters
can be and how vulnerable and unprepared countries are to these events. Since
then significant improvements have been made to mitigate the effect of
tsunamis, with modelling, prediction and warning systems introduced in many
areas.
On 26th December 2004 a large mega-thrust earth
quake of MW 9.3 struck the Sumatra-Andaman Region and resulted in the formation of
numerous large tsunami waves which spread out across the Indian Ocean and
devastating areas along the coasts. The earthquakes epicentre was 3.09oN
and 94.26oE, 100km off the Sumatran coast and occurred along a fault
line stretching from Indonesia to the Andaman Islands in the North where the
Indo-Australian Plate was subducting beneath the Sunda and Burma sub-plates.
The earthquake occurred due to the overriding plate becoming locked
meaning bending and buckling was occurring of this plate, until there is an
abrupt slip and the plate rebounds back (Fig.2) causing a large earthquake and
displacing a large volume of water.(Stein and Okal, n.d.)
The area affected by the Tsunami was vast and even small displacements could be seen on the East Coast of South America. Image from Titov
et al. 2005
The waves were 3-11m high and caused devastation, even today there are scars of the event on the coastlines.
Today an Early Warning Tsunami System has been implemented across the whole of the Indian Ocean and it is constantly monitored due to the risk of the tsunamis.
It was one of the worst events in recorded history and today we remember all those people lost and those affected around the world, ten years on.
Stein, S., and Okal, E.A. (n.d.) Long period seismic moment of the 2004 Sumatra earthquake and
implications for the slip process and tsunami generation [Online] Available at:
< http://www.earth.northwestern.edu/people/seth/research/sumatra.html> [28.02.2012]
Titov, V., Rabinovich, A.B., Mofjield, H., Thompson, R., and
Gonzalez, F. (2005) The Global Reach of the 26 December 2004 Sumatra Tsunami. Science. 309, pp.2045-2048.
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