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2004 Indian Ocean Earthquake and Tsunami: A Catastrophic Event

The 2004 Indian Ocean earthquake and tsunami was a devastating natural disaster that struck off the coast of Sumatra, Indonesia, on December 26, 2004. With a moment magnitude of 9.1–9.3, it caused massive destruction and around 227,898 deaths across 14 countries. The quake resulted from the subduction of the Indo-Australian Plate beneath the Burma Plate, leading to tsunamis with waves up to 30 meters high. This event prompted a significant international humanitarian response and highlighted the destructive power of tectonic processes.

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1

Date and location of 2004 earthquake

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December 26, 2004, off the coast of Sumatra, Indonesia.

2

Plates involved in 2004 earthquake

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Rupture between Burma Plate and Indian Plate.

3

Impact of 2004 tsunami in Aceh province

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Aceh, Indonesia most affected with highest casualties.

4

The initial estimate of the ______ earthquake's magnitude was 8.8, but it was later adjusted to a range of ______.

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2004 Indian Ocean 9.1 and 9.3

5

The ______ of the earthquake stretched for approximately ______ km and persisted for an unusually long time of ______.

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fault rupture 1,200 to 1,300 ten minutes

6

Located between ______ and ______, the earthquake's epicenter was the origin of tremors felt in multiple countries.

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the island of Simeulue mainland Sumatra

7

Countries such as ______, ______, and ______ were among those affected by the earthquake, leading to substantial destruction and fatalities.

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Bangladesh India Sri Lanka

8

Date of the 2004 Tsunami

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Occurred on December 26, known as Boxing Day.

9

Impact on Coastal Communities

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Coastal communities were devastated, with entire areas erased.

10

Effect on Local Economies

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Disaster disrupted economies, causing significant financial strain.

11

The faulting during the earthquake happened in two phases, with a ______ km long and ______ km wide segment slipping first, followed by a rupture extending towards the ______ and ______ Islands.

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400 100 Andaman Nicobar

12

This seismic activity was caused by the - Plate subducting under the ______ Plate at the ______ Trench, which also leads to volcanic activity in the ______ Arc.

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Indo-Australian Burma Sunda Sunda

13

Global seismic moment contribution of 2004 Indian Ocean earthquake

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Provided considerable portion of global seismic moment for past century.

14

Population density impact on 2004 earthquake severity

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Severe impact due to densely populated coastlines, unlike sparser areas in other major quakes.

15

The displacement of a vast amount of water due to the seafloor's elevation resulted in the creation of ______.

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tsunamis

16

The 2004 ______ led to a small, yet permanent rise in global sea levels by approximately 0.1 mm.

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Indian Ocean earthquake and tsunami

17

Following the main seismic event, over a thousand ______ occurred, indicating continuous geological changes.

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aftershocks

18

The 2004 natural disaster is a stark reminder of the ______ and sometimes destructive power of the Earth's tectonic movements.

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dynamic

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2004 Indian Ocean Earthquake and Tsunami: A Catastrophic Event

On December 26, 2004, the world witnessed one of the most catastrophic natural disasters in recent history when an undersea megathrust earthquake, later known as the Sumatra-Andaman earthquake, struck off the coast of Sumatra, Indonesia. With a moment magnitude of 9.1–9.3, it was one of the most powerful earthquakes ever recorded. The earthquake resulted from a rupture along the boundary between the Burma Plate and the Indian Plate, with some areas experiencing shaking up to IX on the Mercalli intensity scale. The quake generated a series of tsunamis, with waves as high as 30 meters, leading to widespread devastation and approximately 227,898 deaths in 14 countries. Indonesia's Aceh province was the hardest hit, with the highest number of casualties. The event marked the deadliest natural disaster of the 21st century and prompted a global humanitarian response.
Coast devastated by a tsunami with scattered debris, uprooted trees, capsized boats and damaged buildings, calm sea in the background.

The Earthquake's Magnitude and Global Impact

The 2004 Indian Ocean earthquake's magnitude was initially underestimated at 8.8 but was later corrected to between 9.1 and 9.3 after further analysis. The seismic force was so immense that it caused the Earth to oscillate by up to 10 mm and set off earthquakes as distant as Alaska. The fault rupture, the longest ever recorded, extended for about 1,200 to 1,300 km and lasted for an extraordinary duration of ten minutes. The epicenter was situated between the island of Simeulue and mainland Sumatra. The tremors were felt across a wide area, impacting countries such as Bangladesh, India, Malaysia, Myanmar, Thailand, Sri Lanka, and the Maldives, and causing significant damage and loss of life.

Tsunami Aftermath and International Aid Effort

The ensuing tsunamis, which occurred on the day after Christmas, known as Boxing Day, resulted in unprecedented destruction. Entire communities along the coastlines were wiped out, and the disaster significantly disrupted the lives and economies of the affected regions. The international community responded swiftly and generously, with donations surpassing US$14 billion. This response was indicative of the global solidarity and commitment to aid the recovery and rebuilding efforts in the countries hit by the disaster.

Seismological Features of the Earthquake

The earthquake exhibited remarkable geological and seismological features. Its hypocenter was located about 160 km off the western coast of northern Sumatra at a depth of 30 km. The faulting process occurred in two stages: initially, a segment of the fault 400 km in length and 100 km in width slipped, and after a brief intermission, the rupture extended towards the Andaman and Nicobar Islands. This seismic event was a result of the subduction of the Indo-Australian Plate beneath the Burma Plate at the Sunda Trench, a process that also contributes to volcanic activity along the Sunda Arc.

Historical Context and Earthquake Comparisons

The 2004 Indian Ocean earthquake is one of the most significant seismic events in recorded history, contributing a considerable portion of the global seismic moment for the past century. In terms of magnitude, it is surpassed only by the 1960 Valdivia earthquake in Chile and the 1964 Alaska earthquake. The impact of the 2004 earthquake was particularly severe due to the densely populated coastlines it affected, unlike the more sparsely populated areas impacted by the other major earthquakes.

Tectonic Shifts and Aftershock Sequence

The earthquake caused a massive shift in the tectonic plates, with an estimated 1,600 km of the fault line moving about 15 meters along the subduction zone. This movement elevated the seafloor and displaced an enormous volume of water, leading to the formation of the tsunamis. The event also contributed to a slight but permanent increase in global sea levels by an estimated 0.1 mm. Numerous aftershocks, over a thousand in the following weeks, highlighted the ongoing geological adjustments after the main quake. The 2004 Indian Ocean earthquake and tsunami serve as a powerful reminder of the dynamic and potentially destructive nature of Earth's tectonic processes.