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https://en.wikipedia.org/wiki/2004_Indian_Ocean_earthquake_and_tsunami
https://en.wikipedia.org/wiki/2004_Indian_Ocean_earthquake_and_tsunami
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| Date | 26 December 2004[1] |
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| Origin time | 00:58:53 UTC 07:58:53 WIB |
| Magnitude | 9.1–9.3 Mw[2] |
| Depth | 30 km (19 mi)[1] |
| Epicenter | 3.316°N 95.854°ECoordinates: 3.316°N 95.854°E[1] |
| Type | Megathrust |
| Areas affected | Indonesia Sri Lanka India Thailand Maldives Somalia Malaysia |
| Max. intensity | IX (Violent)[1] |
| Tsunami | 15 to 30 metres (50 to 100 ft)[3][4] with maximum runup of 51 m (167.3 ft) at Lhoknga.[5] |
| Casualties | 230,000–280,000 dead and more missing[6][7][8][9] |
It is the third-largest earthquake ever recorded on a seismograph and had the longest duration of faulting ever observed, between 8.3 and 10 minutes.[10] It caused the entire planet to vibrate as much as 1 centimetre (0.4 inches)[11] and triggered other earthquakes as far away as Alaska.[12] Its epicentre was between Simeulue and mainland Indonesia.[13] The plight of the affected people and countries prompted a worldwide humanitarian response. In all, the worldwide community donated more than US$14 billion (2004) in humanitarian aid.[14] The event is known by the scientific community as the Sumatra–Andaman earthquake.[15][16] The resulting tsunami was given various names, including the 2004 Indian Ocean tsunami, South Asian tsunami, Indonesian tsunami, the Christmas tsunami and the Boxing Day tsunami.
Contents
Earthquake characteristics
| 2004 Indian Ocean tsunami |
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| Animation of tsunami caused by the earthquake showing how it radiated from the entire length of the 1,600 km (990 mi) rupture Events Response See also |
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The hypocentre of the main earthquake was approximately 160 km (100 mi) off the western coast of northern Sumatra, in the Indian Ocean just north of Simeulue island at a depth of 30 km (19 mi) below mean sea level (initially reported as 10 km (6.2 mi)). The northern section of the Sunda megathrust ruptured over a length of 1,300 km (810 mi).[13] The earthquake (followed by the tsunami) was felt simultaneously in Bangladesh, India, Malaysia, Myanmar, Thailand, Singapore and the Maldives.[19] Splay faults, or secondary "pop up faults", caused long, narrow parts of the sea floor to pop up in seconds. This quickly elevated the height and increased the speed of waves, causing the complete destruction of the nearby Indonesian town of Lhoknga.[20]
The epicenter of the 2004 Indian Ocean earthquake and associated aftershocks in French.
Great earthquakes such as the Sumatra-Andaman event, which are invariably associated with megathrust events in subduction zones, have seismic moments that can account for a significant fraction of the global earthquake moment across century-scale time periods. Of all the seismic moment released by earthquakes in the 100 years from 1906 through 2005, roughly one-eighth was due to the Sumatra-Andaman event. This quake, together with the Good Friday earthquake (Alaska, 1964) and the Great Chilean earthquake (1960), account for almost half of the total moment. The much smaller but still catastrophic 1906 San Francisco earthquake is included in the diagram for perspective. Mw denotes the magnitude of an earthquake on the moment magnitude scale.
Since 1900 the only earthquakes recorded with a greater magnitude were the 1960 Great Chilean earthquake (magnitude 9.5) and the 1964 Good Friday earthquake in Prince William Sound (9.2). The only other recorded earthquakes of magnitude 9.0 or greater were off Kamchatka, Russia, on 4 November 1952 (magnitude 9.0)[21] and Tōhoku, Japan (magnitude 9.0) in March 2011. Each of these megathrust earthquakes also spawned tsunamis in the Pacific Ocean. However, the death toll from these was significantly lower, primarily because of the lower population density along the coasts near affected areas and the much greater distances to more populated coasts and also due to the superior infrastructure and warning systems in MEDCs (More Economically Developed Countries) such as Japan.
Other very large megathrust earthquakes occurred in 1868 (Peru, Nazca Plate and South American Plate); 1827 (Colombia, Nazca Plate and South American Plate); 1812 (Venezuela, Caribbean Plate and South American Plate) and 1700 (western North America, Juan de Fuca Plate and North American Plate). All of them are believed to be greater than magnitude 9, but no accurate measurements were available at the time.
Foreshock
The 2002 Sumatra earthquake is believed to have been a foreshock, predating the main event by over two years.[22]Tectonic plates
Main article: Plate tectonics
A pie chart comparing the seismic moment release for the largest earthquakes from 1906 to 2005 compared to all other earthquakes for the same period
- Seismographic and acoustic data indicate that the first phase involved a rupture about 400 kilometres (250 mi) long and 100 kilometres (60 mi) wide, located 30 kilometres (19 mi) beneath the sea bed—the largest rupture ever known to have been caused by an earthquake. The rupture proceeded at a speed of about 2.8 kilometres per second (1.7 miles per second) (10,000 km/h or 6,200 mph), beginning off the coast of Aceh and proceeding north-westerly over a period of about 100 seconds.
- A pause of about another 100 seconds took place before the rupture continued northwards towards the Andaman and Nicobar Islands. However, the northern rupture occurred more slowly than in the south, at about 2.1 km/s (1.3 mi/s) (7,500 km/h or 4,700 mph), continuing north for another five minutes to a plate boundary where the fault type changes from subduction to strike-slip (the two plates slide past one another in opposite directions).
As well as the sideways movement between the plates, the sea floor is estimated to have risen by several metres, displacing an estimated 30 cubic kilometres (7.2 cu mi) of water and triggering devastating tsunami waves. The waves did not originate from a point source, as was inaccurately depicted in some illustrations of their paths of travel, but rather radiated outwards along the entire 1,600-kilometre (1,000 mi) length of the rupture (acting as a line source). This greatly increased the geographical area over which the waves were observed, reaching as far as Mexico, Chile, and the Arctic. The raising of the sea floor significantly reduced the capacity of the Indian Ocean, producing a permanent rise in the global sea level by an estimated 0.1 millimetres (0.004 in).[23]
Aftershocks and other earthquakes
Locations of initial earthquake and all aftershocks measuring greater
than 4.0 from 26 December 2004 to 10 January 2005. The site of the
original quake is marked by the large star in the lower right square of
the grid.
Other aftershocks of up to magnitude 6.6 continued to shake the region daily for up to three or four months.[25] As well as continuing aftershocks, the energy released by the original earthquake continued to make its presence felt well after the event. A week after the earthquake, its reverberations could still be measured, providing valuable scientific data about the Earth's interior.
The 2004 Indian Ocean earthquake came just three days after a magnitude 8.1 earthquake in an uninhabited region west of New Zealand's subantarctic Auckland Islands, and north of Australia's Macquarie Island. This is unusual, since earthquakes of magnitude 8 or more occur only about once per year on average.[26] However, the U.S. Geological Survey sees no evidence of a causal relationship between these events.[27]
The December earthquake is thought to have triggered activity in both Leuser Mountain[28] and Mount Talang,[29] volcanoes in Aceh province along the same range of peaks, while the 2005 Nias–Simeulue earthquake had sparked activity in Lake Toba, an ancient crater in Sumatra.
Energy released
The tsunami strikes Ao Nang, Thailand.
The only recorded earthquakes with a larger MW were the 1960 Chilean and 1964 Alaskan quakes, with 2.5×1023 joules (250 ZJ) and 7.5×1022 joules (75 ZJ) respectively.[32]
The earthquake generated a seismic oscillation of the Earth's surface of up to 20–30 cm (8–12 in), equivalent to the effect of the tidal forces caused by the Sun and Moon. The shock waves of the earthquake were felt across the planet; as far away as the U.S. state of Oklahoma, where vertical movements of 3 mm (0.12 in) were recorded. By February 2005, the earthquake's effects were still detectable as a 20 µm (0.02 mm; 0.0008 in) complex harmonic oscillation of the Earth's surface, which gradually diminished and merged with the incessant free oscillation of the Earth more than 4 months after the earthquake.[33]
Because of its enormous energy release and shallow rupture depth, the earthquake generated remarkable seismic ground motions around the globe, particularly due to huge Rayleigh (surface) elastic waves that exceeded 1 cm (0.4 in) in vertical amplitude everywhere on Earth. The record section plot displays vertical displacements of the Earth's surface recorded by seismometers from the IRIS/USGS Global Seismographic Network plotted with respect to time (since the earthquake initiation) on the horizontal axis, and vertical displacements of the Earth on the vertical axis (note the 1 cm scale bar at the bottom for scale). The seismograms are arranged vertically by distance from the epicenter in degrees. The earliest, lower amplitude, signal is that of the compressional (P) wave, which takes about 22 minutes to reach the other side of the planet (the antipode; in this case near Ecuador). The largest amplitude signals are seismic surface waves that reach the antipode after about 100 minutes. The surface waves can be clearly seen to reinforce near the antipode (with the closest seismic stations in Ecuador), and to subsequently encircle the planet to return to the epicentral region after about 200 minutes. A major aftershock (magnitude 7.1) can be seen at the closest stations starting just after the 200 minute mark. This aftershock would be considered a major earthquake under ordinary circumstances, but is dwarfed by the mainshock.
Vertical-component ground motions recorded by the IRIS/USGS Global Seismographic Network.
More spectacularly, there was 10 m (33 ft) movement laterally and 4–5 m (13–16 ft) vertically along the fault line. Early speculation was that some of the smaller islands south-west of Sumatra, which is on the Burma Plate (the southern regions are on the Sunda Plate), might have moved south-west by up to 36 m (120 ft), but more accurate data released more than a month after the earthquake found the movement to be about 20 cm (8 in).[37] Since movement was vertical as well as lateral, some coastal areas may have been moved to below sea level. The Andaman and Nicobar Islands appear to have shifted south-west by around 1.25 m (4 ft 1 in) and to have sunk by 1 m (3 ft 3 in).[38]
In February 2005, the Royal Navy vessel HMS Scott surveyed the seabed around the earthquake zone, which varies in depth between 1,000 and 5,000 m (550 and 2,730 fathoms; 3,300 and 16,400 ft). The survey, conducted using a high-resolution, multi-beam sonar system, revealed that the earthquake had made a huge impact on the topography of the seabed. 1,500-metre-high (5,000 ft) thrust ridges created by previous geologic activity along the fault had collapsed, generating landslides several kilometres wide. One such landslide consisted of a single block of rock some 100 m high and 2 km long (300 ft by 1.25 mi). The momentum of the water displaced by tectonic uplift had also dragged massive slabs of rock, each weighing millions of tons, as far as 10 km (6 mi) across the seabed. An oceanic trench several kilometres wide was exposed in the earthquake zone.[39]
The TOPEX/Poseidon and Jason-1 satellites happened to pass over the tsunami as it was crossing the ocean.[40] These satellites carry radars that measure precisely the height of the water surface; anomalies of the order of 50 cm (20 in) were measured. Measurements from these satellites may prove invaluable for the understanding of the earthquake and tsunami.[41] Unlike data from tide gauges installed on shores, measurements obtained in the middle of the ocean can be used for computing the parameters of the source earthquake without having to compensate for the complex ways in which close proximity to the coast changes the size and shape of a wave.
Tsunami
NOAA's tsunami travel time (TTT) map for the 2004 Indian Ocean tsunami.
The TTT map calculates the first-arrival travel times of the tsunami,
following their generation at the earthquake epicenter. Note that the
maps do not provide the height or the strength of the wave, only the
arrival times. The number tags represent hours after the initial event.
Map contours represent 1-hour intervals. Red indicates 1- to 4-hour
arrival times, Yellow indicates 5- to 6-hour arrival times, Green
indicates 7- to 14-hour arrival times, and Blue indicates 15- to 21-hour
arrival times. Maps were generated from earthquake epicenters in the
NGDC Global Historical Tsunami Database using NGDC 2-Minute Gridded
Global Relief Data bathymetry. The map was created through models based
on quality-controlled source data, and an integration of many data sets
together.
Scale showing the size of the tsunami waves that hit Indonesia
The tsunami, like all others, behaved very differently in deep water than in shallow water. In deep ocean water, tsunami waves form only a small hump, barely noticeable and harmless, which generally travels at a very high speed of 500 to 1,000 km/h (310 to 620 mph); in shallow water near coastlines, a tsunami slows down to only tens of kilometres per hour but, in doing so, forms large destructive waves. Scientists investigating the damage in Aceh found evidence that the wave reached a height of 24 metres (80 ft) when coming ashore along large stretches of the coastline, rising to 30 metres (100 ft) in some areas when traveling inland.[4]
Radar satellites recorded the heights of tsunami waves in deep water: at two hours after the earthquake, the maximum height was 60 centimetres (2 ft). These are the first such observations ever made. Unfortunately these observations could not be used to provide a warning, since the satellites were not built for that purpose and the data took hours to analyze.[43][44]
According to Tad Murty, vice-president of the Tsunami Society, the total energy of the tsunami waves was equivalent to about five megatons of TNT (20 petajoules). This is more than twice the total explosive energy used during all of World War II (including the two atomic bombs) but still a couple of orders of magnitude less than the energy released in the earthquake itself. In many places the waves reached as far as 2 km (1.2 mi) inland.[45]
Tsunami wave field in the Bay of Bengal one hour after the M=9.2 earthquake. View to the northwest.
Coasts that have a landmass between them and the tsunami's location of origin are usually safe; however, tsunami waves can sometimes diffract around such landmasses. Thus, the state of Kerala was hit by the tsunami despite being on the western coast of India, and the western coast of Sri Lanka suffered substantial impacts. Distance alone was no guarantee of safety, as Somalia was hit harder than Bangladesh despite being much farther away.
Because of the distances involved, the tsunami took anywhere from fifteen minutes to seven hours to reach the coastlines.[46][47] The northern regions of the Indonesian island of Sumatra were hit very quickly, while Sri Lanka and the east coast of India were hit roughly 90 minutes to two hours later. Thailand was struck about two hours later despite being closer to the epicentre, because the tsunami traveled more slowly in the shallow Andaman Sea off its western coast.
The tsunami was noticed as far as Struisbaai in South Africa, some 8,500 km (5,300 mi) away, where a 1.5 m (5 ft) high tide surged on shore about 16 hours after the earthquake. It took a relatively long time to reach this spot at the southernmost point of Africa, probably because of the broad continental shelf off South Africa and because the tsunami would have followed the South African coast from east to west. The tsunami also reached Antarctica, where tidal gauges at Japan's Showa Base recorded oscillations of up to a metre (3 ft 3 in), with disturbances lasting a couple of days.[48]
Some of the tsunami's energy escaped into the Pacific Ocean, where it produced small but measurable tsunamis along the western coasts of North and South America, typically around 20 to 40 cm (7.9 to 15.7 in).[49] At Manzanillo, Mexico, a 2.6 m (8 ft 6 in) crest-to-trough tsunami was measured. As well, the tsunami was large enough to be detected in Vancouver, British Columbia, Canada. This puzzled many scientists, as the tsunamis measured in some parts of South America were larger than those measured in some parts of the Indian Ocean. It has been theorized that the tsunamis were focused and directed at long ranges by the mid-ocean ridges which run along the margins of the continental plates.[50]
Signs and warnings
Maximum recession of tsunami waters at Kata Noi Beach,
Thailand, before the third, and strongest, tsunami wave (sea visible in
the right corner, the beach is at the extreme left), 10:25 am local
time.
Tsunamis are much more frequent in the Pacific Ocean because of earthquakes in the "Ring of Fire", and an effective tsunami warning system has long been in place there. Although the extreme western edge of the Ring of Fire extends into the Indian Ocean (the point where this earthquake struck), no warning system exists in that ocean. Tsunamis there are relatively rare despite earthquakes being relatively frequent in Indonesia. The last major tsunami was caused by the Krakatoa eruption of 1883. It should be noted that not every earthquake produces large tsunamis; on 28 March 2005, a magnitude 8.7 earthquake hit roughly the same area of the Indian Ocean but did not result in a major tsunami.
The first warning sign of a possible tsunami is the earthquake itself. However, tsunamis can strike thousands of kilometres away where the earthquake is only felt weakly or not at all. Also, in the minutes preceding a tsunami strike, the sea often recedes temporarily from the coast. This was observed on the eastern side of the rupture zone of the earthquake such as around the coastlines of Aceh province, Phuket island and Khao Lak area in Thailand, Penang island of Malaysia and the Andaman and Nicobar islands. Around the Indian Ocean, this rare sight reportedly induced people, especially children, to visit the coast to investigate and collect stranded fish on as much as 2.5 km (1.6 mi) of exposed beach, with fatal results.[52] However, not all tsunamis cause this "disappearing sea" effect. In some cases, there are no warning signs at all: the sea will suddenly swell without retreating, surprising many people and giving them little time to flee.
As a matter of fact, scuba divers diving around the abundant coral reefs in Thailand and the Maldives were reportedly caught off guard by violent, swirling underwater currents. The divers described the experience like being in a 'washing machine'. Coral reef animals like fish were also absent as the tsunami pass by.[53]
One of the few coastal areas to evacuate ahead of the tsunami was on the Indonesian island of Simeulue, very close to the epicentre. Island folklore recounted an earthquake and tsunami in 1907, and the islanders fled to inland hills after the initial shaking and before the tsunami struck. These tales and oral folklore from previous generations may have helped the survival of the inhabitants.[54] On Maikhao beach in northern Phuket, Thailand, a 10-year-old British tourist named Tilly Smith had studied tsunami in geography at school and recognised the warning signs of the receding ocean and frothing bubbles. She and her parents warned others on the beach, which was evacuated safely.[55] John Chroston, a biology teacher from Scotland, also recognised the signs at Kamala Bay north of Phuket, taking a busload of vacationers and locals to safety on higher ground.
Anthropologists had initially expected the aboriginal population of the Andaman Islands to be badly affected by the tsunami and even feared the already depopulated Onge tribe could have been wiped out.[56] Many of the aboriginal tribes evacuated and suffered fewer casualties.[57][58] Oral traditions developed from previous earthquakes helped the aboriginal tribes escape the tsunami. For example, the folklore of the Onges talks of "huge shaking of ground followed by high wall of water". Almost all of the Onge people seemed to have survived the tsunami.[59]
Aceh province, Sumatra, Indonesia
A two story house damaged by the tsunami showing the tsunami inundation height in downtown Banda Aceh.
The maximum runup height of the tsunami was measured at a hill between Lhoknga and Leupung, located on the west coast of the northern tip of Sumatra, near Banda Aceh, and reached more than 30 m (100 ft).[5]
The tsunami heights in Sumatra:[63]
• 15–30 m (49 ft-98 ft) on the west coast of Aceh.
• 6–12 m (19.7 ft-39.4 ft) on the Banda Aceh coast.
• 6 m (19.7 ft) on the Krueng Raya coast ( 3 oil tanks floated out)
• 5 m (16.4 ft) on the Sigli coast.
• 3–6 m (9.8 ft-19.7 ft) on the north coast of Weh Island directly facing the tsunami source.
• 3 m (9.8 ft) on the opposite side of the coast of Weh Island facing the tsunami.
The tsunami height on the Banda Aceh coast is lower than half of that on the west coast. Even within the Banda Aceh coast, the tsunami height was reduced by half from 12 m (39.4 ft) at Ulee Lheue to 6 m (19.7 ft) a further 8 km (4.97 miles) to the northeast. One of the reasons seems to be that there is an archipelago between Lhoknga and Banda Aceh. The tsunami advanced about 4 km (2.49 miles) inland at Banda Aceh. Within 2–3 km (1.24-1.86 miles) from the shoreline, houses, except for strongly-built reinforced concrete ones with brick walls, which seemed to have been partially damaged by the earthquake before the tsunami attack, were completely swept away or destroyed by the tsunami.[63]
In Lhoknga, a town in Aceh Besar Regency, Aceh Special Region, Indonesia, located on the western side of the island of Sumatra, 13 km (8.08 miles) southwest of Banda Aceh was completely flattened and destroyed by the 2004 Boxing Day Tsunami, where its population dwindled from 7,500 to 400. The tsunami waves were almost 30 m (98.4 ft) high. Eyewitnesses reported 10 to 12 waves, the second and third ones being the highest. The sea receded (drawback) 10 minutes after the earthquake and the first wave came rapidly landward as a turbulent flow (flood) with depths ranging from 0.5 to 2.5 m (1.64 ft-8.20 ft) high. The second and third waves was 15–30 m (49.2 ft-98.4 ft) high at the coast, described having an appearance to a surf wave (cobra-shaped) but 'taller than the coconut trees' and was 'like a mountain'.[64] Consequently, the tsunami also stranded cargo ships and barges and destroyed a cement factory near the Lampuuk coast.[5][65][66] Moreover, surveyed areas by scientists show runup heights over 20 m (65.6 ft) on the northwest coast of Sumatra in the Aceh province with a maximum runup of 51 m (167.3 ft).[67]
In Meulaboh based on survivor testimonies, tsunami arrived after the sea receded about 500 m (0.31 miles), followed by an advancing small tsunami. The second and third destructive waves arrived later, which exceeded the height of the coconut trees. The inundation distance is about 5 km (3.1 miles).[68]
Such high and fast waves arising from the epicentre by a megathrust earthquake were later found to be due to splay faults, secondary faults arising due to cracking of the sea floor to jut upwards in seconds, causing waves' speed and height to increase. A large slip of 30 m (98.4 ft) was estimated on the subfault located off the west coast of Aceh province. Another factor is subsidence at Banda Aceh (20–60 cm), Peukan Bada (>20 cm), Lhok Nga and Leupung (>1.5 m).[63]
An overturned cement carrier, the Sinar Andalas caused by the tsunami in Lhoknga.
The very high fatality in the area is mainly due to the unpreparedness of the population from such an event. Helicopter survey showed entire settlements virtually destroyed with destruction miles inland with only some mosques left standing, which provided refuge for the people from the tsunami.
Andaman and Nicobar Islands, India
The major islands affected by the tsunami were in the South, Middle, and North Andaman Islands. The tsunami arrived in the Andaman and Nicobar Islands minutes after the earthquake, and it caused extensive devastation to the islands' environment. Specifically, the Andaman Islands were moderately affected while the island of Little Andaman and the Nicobar Islands were severely affected by the tsunami.[69][70]Eyewitnesses at Port Blair recall that the water receded before the first wave, and the third wave was the tallest and caused the most damage. However, at Hut Bay, Malacca and Campbell Bay — locations far south of Port Blair — it was reported that the water level rose by about 1–2 m (3.3 ft-6.6 ft) from the normal sea level and remained there before the first wave crashed ashore.
Reports of tsunami wave height:[71]
• 8 m (26.2 ft) high at Campbell Bay (in Great Nicobar Island),
• 10–12 m (32.8 ft-39.4 ft) high at Malacca (in Car Nicobar Island) and at Hut Bay (in Little Andaman Island).
• 3 m (9.8 ft) high at Port Blair (in South Andaman Island).
The significant shielding of Port Blair and Campbell Bay by steep mountainous outcrops may have contributed to the relatively low wave heights at these locations, whereas the open terrain along the eastern coast at Malacca and Hut Bay likely contributed to the great height of the tsunami waves [70][72]
Indeed, many infrastructures near the coasts and buildings were harshly damaged by the waves.
Sri Lanka
The tsunami first arrived on the eastern coast and subsequently refracted around the southern point of Sri Lanka (Dondra Head). The refracted tsunami waves inundated the southwestern part of Sri Lanka after some of its energy has been reflected from impact with the Maldives.[73] Sri Lanka is located 1,700 km (1056.33 miles) far from the epicenter and the tsunami source, so no one felt the ground shake and the tsunami hit the entire coastline of Sri Lanka around 2 hours after the earthquake.[74] It seems that the tsunami flooding consisted of three main waves, with the second being the largest and most destructive.[75] The first tsunami waves had initially caused a small flood (positive wave) as it struck the Sri Lankan coastline. Moments later, the ocean floor was exposed to as much as 1 km (0.62 miles) in places due to drawback (negative wave). This was followed by a massive second tsunami wave, which is in the form of a flood. Certain locations managed to reduce the power of the waves through construction of seawalls and breakwaters.The largest run-up measured was at 12.5 m (41 ft) with inundation distance of 390 m to 1.5 km (0.242 miles-0.932 miles) in Yala.[76] In Hambantota, tsunami run-ups are measured at 11 m (36.1 ft) with the greatest inundation distance of 2 km (1.24 miles), and tsunami run-up measurements along the Sri Lankan coasts are at 2.4–11 m (7.87 ft-36.1 ft).[73][76] Tsunami waves measured on the east coast ranged from 4.5 m-9 m (14.8 ft-29.5 ft) at Pottuvill to around Batticaloa, 2.6 m- 5 m (8.53 ft-16.4 ft) in the northeast around Trincomalee and 4 m-5 m (13.1 ft-16.4 ft) in the west coast from Moratuwa to Ambalangoda.
Fishermen's boat stranded in Kallady, Batticaloa, Sri Lanka.
• 9 m (29.5 Ft) at Koggala.
• 6 m (19.7 ft) at Galle port.
• 4.8 m (15.7 ft) around the Galle coast.
• 8.71 m (28.6 ft) at Nonagama.
• 4.9 m (16.1 ft) at Weligama.
• 4 m (13.1 ft) at Dodundawa.
• 4.7 m (15.4 ft) at Ambalangoda.
• 4.7 m (15.4 ft) at Hikkaduwa Fishery Harbour.
• 10 m (33 ft) at Kahawa.
• 4.8 m (15.7 ft) at North Beach of Beruwala.
• 6 m (19.7 ft) at Paiyagala.
The Sumudra Devi, a passenger train out of Colombo, was derailed and overturned by the tsunami.[77] The tsunami caused the 2004 Sri Lanka tsunami-rail disaster which took at least 1,700 lives, making it the largest single rail disaster in world history by death toll. Estimates based on the state of the shoreline and a high-water mark on a nearby building place the tsunami 7.5–9 m (24.6 ft to 29.5 ft) above sea level and 2–3 m (6.6 ft to 9.8 ft) higher than the top of the train.[74]
In Sri Lanka, the civilian casualties were second only to those in Indonesia. Reports vary on the number of deaths since many people are still missing and the country lacks adequate communications. The eastern shores of Sri Lanka faced the hardest impact since they were facing the epicenter of the earthquake. The southwestern shores were hit later, but the death toll was just as severe. The southwestern shores are a hotspot for tourists as well as the fishing economy. Tourism and fishing industries created high population densities along the coast.[78]
The coastal lifestyle of people and degradation of the natural environment in Sri Lanka contributed to the high death tolls. In addition to the high number of fatalities, approximately 90,000 buildings were destroyed. Houses were easily destroyed since they were built mostly from wood.[78]
Thailand
The tsunami hit the southwest coast of southern Thailand, which was about 500 km (310.69 miles) from the epicenter. The region is famous for it's high quality resorts, pristine beaches, spectacular islands with warm Andaman blue waters and stunning scenery making it prominent with tourists internationally. Since the tsunami hit around high tide, its damage was severe. Approximately 5,400 people were killed and 3,100 people were reported missing in Thailand. The places where the tsunami attacked were Khao Lak, Phuket Island, the Phi Phi Islands, Koh Racha Yai, Koh Lanta Yai, Ao Nang of Krabi province, offshore islands like the Surin islands, the Similan islands, and in Satun, Ranong, Phang Nga, Trang and Krabi provinces.The tsunami heights recorded:[79][80]
• 6–10 m (19.7 ft-32.8 ft) in Khao Lak.
• 3–6 m (9.84 ft-19.7 ft) along the west coast of Phuket island.
• 3 m (9.84 ft) along the south coast of Phuket island.
• 2 m (6.56 ft) along the east coast of Phuket island.
• 4–6 m (13.12 ft-19.7 ft) on the Phi Phi Islands.
• 19.6 m (64.3 ft) at Ban Thung Dap.
• 5 m (16.4 ft) at Ramson.
• 6.8 m (22.3 ft) at Ban Thale Nok.
• 5 m (16.4 ft) at Hat Praphat (Ranong Coastal Resources Research Station).
• 6.3 m (20.7 ft) at Thai Muang district.
• 6.8 m (22.3 ft) at Rai Dan.
The country experienced the largest tsunami runup height of any location outside of Sumatra, which occurred at Khao Lak and the areas of Takua Pa district that are facing the Andaman Sea. Many local villagers and tourists lost their lives during the event. A maximum inundation of approximately 2 km (1.2 miles) and the inundated depths were 4–7 m (13.12 ft-23 ft) in Khao Lak. Surveys conducted show that the tsunami inundated the third floor of a resort hotel. The tsunami heights in Khao Lak were much higher than Phuket Island. The reason for this difference seems to have been caused by the local bathymetry off Khao Lak. According to some interviews with local residents and affected tourists, the leading wave produced an initial depression, called a tsunami drawback or 'disappearing sea' effect and the second wave was largest.[79] The highest recorded tsunami runup measured was at 19.6 m (64.3 ft) at Ban Thung Dap, located on the southwest tip of Ko Phra Thong Island and the second highest at 15.8 m (51.8 ft) at Ban Nam Kim.[80]
Thai navy boat 813 ( police boat ) stranded almost 2 km inland by the Khao Lak tsunami.
Tsunami wave striking Phuket coast.
Many amateur videos recorded by tourists and locals of the tsunami at Thailand were televised popularly in the media.
Mainland India
The tsunami arrived in the states of Andhra Pradesh and Tamil Nadu along the southeast coast of the Indian mainland shortly after 9:00 a.m. At least two hours later, it arrived in the state of Kerala along the southwest coast. Tamil Nadu, the union territory of Pondicherry and Kerala were extensively damaged, while Andhra Pradesh sustained moderate damage. There were two to five waves of varying height that coincided with the local high tide in some areas.[81][82][83][84]
Tsunami destruction in Chennai, Tamil Nadu, India.
The tsunami runup height measured in mainland India by Ministry of Home Affairs:[84]
• 3.4 m (11.2 ft) at Kerala, inundation distance of 0.5-1.5 km (0.31-0.62 miles) with 250 km (155.3 miles) of coastline affected.
• 4.5 m (14.8 ft) at southern coastline of Tamil Nadu, inundation distance of 0.2-2.0 km (0.12-1.24 miles) with 100 km (62.1 miles) of coast affected.
• 5 m (16.4 ft) at eastern coastline of Tamil Nadu facing tsunami source, inundation distance of 0.4-1.5 km (0.25-0.93 miles) with 800 km (497 miles) of coastline affected.
• 4 m (13.1 ft) at Pondicherry, inundation distance of 0.2-2.0 km (0.12-1.24 miles) with 25 km (15.5 miles) of coast affected.
• 2.2 m (7.22 ft) at Andhra Pradesh, inundation distance of 0.2-1.0 km (0.12-0.62 miles) with 985 km (612 miles) of coast.
The tsunami traveled 2.5 km (1.55 miles) at its maximum inland at Karaikal city.[84] The inundation distance varied between 100–500 m (0.062 miles-0.311 miles) in most areas, except at river mouths, where it was more than 1 km (0.62 miles). The inundation distance varied with topology and vegetation. Areas with dense coconut groves or mangroves had much smaller inundation distances, and those with river mouths or backwaters saw much larger inundation distances.[citation needed]Presence of seawalls at the Kerala coast and some of Tamil Nadu coast helped to reduce the impact of the waves. However, when the seawalls were made of loose stones, the stones were displaced and carried a few metres inland.[81][83][85]
The state of Kerala experienced tsunami-related damage in three southern districts, Ernakulam, Alappuzha, and Kollam, which are densely populated with villagers, due to diffraction of the waves around Sri Lanka. The southernmost district of Thiruvananthpuram, however, escaped damage, possibly due to the wide turn of the diffracted waves at the peninsular tip. Major damage occurred in two narrow strips of land bound on the west by the Arabian Sea and on the east by a network of backwaters - Kerala backwaters. The waves receded before the first tsunami with the highest fatality reported from the densely populated Alappad panchayat (including the villages of Cheriya Azhikkal and Azhikkal) at Kollam district, caused by a 4 m (13.1 ft) tsunami.[84]
The worst affected area in Tamil Nadu was Nagapattinam district, with a reported 6,051 fatalities caused by a 5 m (16.4 ft) tsunami, followed by Cuddalore district, with many villages destroyed.[84] The 13 km (8.1 miles) Marina Beach in Chennai was battered by the tsunami which swept across the beach taking morning walkers unaware. Besides that, a 10 m (33 ft) black muddy tsunami reportedly ravaged the city of Karaikal, where 492 lives were lost. The city of Pondicherry, protected by seawalls relatively escaped unscathed in comparison to other areas in the state.[84]
At the same time, many villages from many districts at the state of Andhra Pradesh was destroyed. In the Krishna district, the tsunami created havoc in Manginapudi and on Machalipattanam Beach, which came like a running wall at the latter. The most affected was Prakasham District, recording 35 deaths, with maximum damage at Singraikonda, a beautiful beach hamlet.[84]
Given the enormous power of the tsunami, the fishing industry suffered the greatest. Moreover, the cost of damages in the transport sector was reported in the tens of thousands.[84] Many buildings and infrastructures near the coast were obliterated.
Conclusively, the tsunami effects varied greatly across different parts of the coast according to the number of waves experienced, the inundation distance and height of waves, and the population density of the area, as well as topological and geographical features that made some areas more vulnerable than others. Besides these factors, the number of lives lost was influenced by exposure to previous disasters and the local disaster management capability. Most of the people killed were members of the fishing community and, in some cases such as Marina Beach at Chennai and Velankanni in Nagapattinam, they were visitors on the beach.[84]
Maldives
The tsunami of 26 December 2004 severely affected the Maldives at a distance of 2,500 km (1553.4 miles) from the epicenter of the magnitude 9.0 earthquake. Identically to Sri Lanka, survivors reported three waves with the second wave being the most powerful.[75] Being rich in coral reefs, the Maldives provides an opportunity for scientists to assess the impact of a tsunami on coral atolls. The significantly lower tsunami impact on the Maldives compared to Sri Lanka is largely due to the topography and bathymetry of the atoll chain with offshore coral reefs, deep channels separating individual atolls and its arrival within low tide which decreased the power of the tsunami.[86]The largest tsunami wave measured was 4 m (13.1 ft) at Vilufushi Island (Thaa Atoll). The tsunami arrived approximately 2 hours after the earthquake.The greatest tsunami inundation occurred at North Male Atoll, Male island at 250 m (0.155 miles) along the streets.[75]
The Maldives tsunami wave analysis:[75]
• 1.3 m-2.4 m (4.27 ft-7.87 ft) at North Male Atoll, Male Island.
• 2 m (6.56 ft) at North Male Atoll, Huhule Island.
• 1.7 m-2.8 m (5.58 ft-9.2 ft) at South Male Atoll, Embudhu Finothu.
• 2.5 m-3.3 m (8.2 ft-10.8 ft) at Laamu Atoll, Fonadhoo Island.
• 2.2 m-2.9 m (7.2 ft-9.51 ft) at Laamu Atoll, Gan Island.
• 2.3 m-3 m (7.5 ft-9.8 ft) at North Male Atoll, Dhiffushi Island.
• 2.2 m-2.4 m (7.2 ft-7.87 ft) at North Male Atoll, Huraa Island.
• more than 1.5 m (4.92 ft) at North Male Atoll, Kuda Huraa Island.
Somalia
The tsunami spawned from the megathrust earthquake near Sumatra travelled 5000 km (3106.86 miles) west across the open ocean and ravaged the East African country of Somalia. Around 289 mortalities were reported in the Horn of Africa, drowned by four tsunami waves. The hardest hit was a 650 km (403.9 miles) stretch of the Somalia coastline between Garacad (Mudug region) and Xaafuun (Bari region), which forms part of the Puntland Province. Most of the victims were reported along the low-lying Xaafuun Peninsula.[87] The Puntland coast in northern Somalia was by far the area hardest hit by the waves to the west of the Indian subcontinent. The waves arrived around noon local time.[87]Consequently, tsunami runup heights vary from 5 m (16.4 ft) to 9 m (29.5 ft) with inundation distances varying from 44 m (0.027 miles) to 704 m (0.44 miles). The maximum runup height of almost 9 m (29.5 ft) was recorded in Bandarbeyla. An even higher runup point was measured on a cliff near the town of Eyl, solely on an eyewitness account.
The highest death toll was in Xaafuun, also known as Hafun, with 19 bodies and 160 people persumed missing out of its 5000 inhabitants, this amounts to the highest number of casualties in a single African town and the largest tsunami death toll in a single town to the west of the Indian subcontinent. In Xaafuun, small drawbacks were observed before the third and most powerful tsunami flood the town.[87]
Apart from lives and livelihood lost during the disaster, numerous fishing boats and buildings were devastated.
Elsewhere in the Indian Ocean
The tsunami also devastated Malaysia, mainly on the northern states such as Kedah, Perak, Selangor and Penang and on offshore islands such as Langkawi island. Peninsular Malaysia was shielded by the full fury of the tsunami due to the protection offered by the island of Sumatra, which lies just off the western coast.[88]
Tsunami flooding the streets of Tanjung Tokong, George Town, Penang.
The tsunami's immense power was even detected as far away as Africa, where rough seas were reported, specifically on the eastern and southern coasts that faces the Indian Ocean. Countries apart from Somalia that were majorly affected with deaths include South Africa (the furthest)- 2, Kenya- 1, The Seychelles- 3 and Tanzania- 10.[90][91]
Death toll and casualties
Chennai's Marina Beach after the tsunami.
The tsunami caused serious damage and deaths as far as the east coast of Africa, with the farthest recorded death due to the tsunami occurring at Rooi Els in South Africa, 8,000 km (5,000 mi) away from the epicentre. In total, eight people in South Africa died due to abnormally high sea levels and waves.
Relief agencies reported that one-third of the dead appeared to be children. This was a result of the high proportion of children in the populations of many of the affected regions and because children were the least able to resist being overcome by the surging waters. Oxfam went on to report that as many as four times more women than men were killed in some regions because they were waiting on the beach for the fishermen to return and looking after their children in the houses.[93]
In addition to the large number of local residents, up to 9,000 foreign tourists (mostly Europeans) enjoying the peak holiday travel season were among the dead or missing, especially people from the Nordic countries. The European nation hardest hit may have been Sweden, whose death toll was 543.[94]
States of emergency were declared in Sri Lanka, Indonesia, and the Maldives. The United Nations estimated at the outset that the relief operation would be the costliest in human history. Then-UN Secretary-General Kofi Annan stated that reconstruction would probably take between five and ten years. Governments and non-governmental organisations feared that the final death toll might double as a result of diseases, prompting a massive humanitarian response. In the end, this fear did not materialise.
Patong Beach, Thailand, after the tsunami
| Country where deaths occurred |
Confirmed | Estimated1 | Injured | Missing | Displaced |
|---|---|---|---|---|---|
| Indonesia | 130,736 | 167,799 | n/a | 37,063 | 500,000+[95] |
| Sri Lanka2 | 35,322[96] | 35,322 | 21,411[96] | n/a | 516,150[96] |
| India | 12,405 | 18,045 | n/a | 5,640 | 647,599 |
| Thailand | 5,3953[97] | 8,212 | 8,457[98] | 2,817[97] | 7,000 |
| Somalia | 78 | 289[99] | n/a | n/a | 5,000[100] |
| Myanmar (Burma) | 61 | 400–600[101] | 45 | 200[102] | 3,200 |
| Maldives | 82[103] | 108[104] | n/a | 26 | 15,000+ |
| Malaysia | 68[105] | 75 | 299[106] | 6 | 5,000+ |
| Tanzania | 10[107] | 13 | n/a | n/a | n/a |
| Seychelles | 3[108] | 3 | 57[108] | n/a | 200[109] |
| Bangladesh | 2 | 2 | n/a | n/a | n/a |
| South Africa | 24[110] | 2 | n/a | n/a | n/a |
| Yemen | 2[111] | 2 | n/a | n/a | n/a |
| Kenya | 1 | 1 | 2 | n/a | n/a |
| Madagascar | n/a | n/a | n/a | n/a | 1,000+[112] |
| Total | ~184,167 | ~230,273 | ~125,000 | ~45,752 | ~1.74 million |
1 Includes those reported under 'Confirmed'. If no
separate estimates are available, the number in this column is the same
as reported under 'Confirmed'.
2 Does not include approximately 19,000 missing people initially declared by Tamil Tiger authorities from regions under their control.
3 Data includes at least 2,464 foreigners.
4 Does not include South African citizens who died outside of South Africa (e.g., tourists in Thailand). For more information on those deaths, see this
2 Does not include approximately 19,000 missing people initially declared by Tamil Tiger authorities from regions under their control.
3 Data includes at least 2,464 foreigners.
4 Does not include South African citizens who died outside of South Africa (e.g., tourists in Thailand). For more information on those deaths, see this
Countries affected
Countries most affected by the tsunami, with the earthquake's epicenter.
Main article: Countries affected by the 2004 Indian Ocean earthquake
The earthquake and resulting tsunami affected many countries in Southeast Asia and beyond, including Indonesia, Sri Lanka, India, Thailand, the Maldives, Somalia, Myanmar, Malaysia, Seychelles
and others. Many other countries, especially Australia and those in
Europe, had large numbers of citizens traveling in the region on
holiday. Sweden lost 543 citizens in the disaster, while Germany had 539 identified victims.Event in historical context
The last major tsunami in the Indian Ocean was about A.D. 1400.[113][114] In 2008, a team of scientists working on Phra Thong, a barrier island along the hard-hit west coast of Thailand, reported evidence of at least three previous major tsunamis in the preceding 2,800 years, the most recent from about 700 years ago. A second team found similar evidence of previous tsunamis in Aceh, a province at the northern tip of Sumatra; radiocarbon dating of bark fragments in soil below the second sand layer led the scientists to estimate that the most recent predecessor to the 2004 tsunami probably occurred between A.D. 1300 and 1450.[115]The 2004 earthquake and tsunami combined are the world's deadliest natural disaster since the 1976 Tangshan earthquake. This earthquake was the third most powerful earthquake recorded since 1900. The deadliest known earthquake in history occurred in 1556 in Shaanxi, China, with an estimated death toll of 830,000, though figures from this period may not be as reliable.[116]
The 2004 tsunami is the deadliest in recorded history. Prior to 2004, the tsunami created in both Indian and Pacific Ocean waters by the 1883 eruption of Krakatoa, thought to have resulted in anywhere from 36,000 to 120,000 deaths, had probably been the deadliest in the region. In 1782 about 40,000 people are thought to have been killed by a tsunami (or a cyclone) in the South China Sea.[117] The most deadly tsunami prior to 2004 was Italy's 1908 Messina earthquake on the Mediterranean Sea where the earthquake and tsunami killed about 123,000.[118]
Impact
Humanitarian impact
German tsunami relief mission team members of AGSEP visiting tsunami-hit Mullaitivu in Northern Province, Sri Lanka in January 2005
Memorial dedicated to victims of the tsunami, Batticaloa, Eastern Province, Sri Lanka
There was also a great concern that the death toll could increase as disease and hunger spread. However, because of the initial quick response, this was minimized.[119]
In the days following the tsunami, significant effort was spent in burying bodies hurriedly due to fear of disease spreading. However, the public health risks may have been exaggerated, and therefore this may not have been the best way to allocate resources. The World Food Programme provided food aid to more than 1.3 million people affected by the tsunami.[120]
Further information: Health risks from dead bodies
Nations all over the world provided over US$14 billion in aid for damaged regions,[121] with the governments of Australia pledging US$819.9 million (including a US$760.6-million aid package for Indonesia), Germany offering US$660 million, Japan offering US$500 million, Canada offering US$343 million, Norway and the Netherlands offering both US$183 million, the United States offering US$35 million initially (increased to US$350 million), and the World Bank
offering US$250 million. Also Italy offered US$95 million, increased
later to US$113 million of which US$42 million was donated by the
population using the SMS system[122] According to USAID,
the US has pledged additional funds in long-term U.S. support to help
the tsunami victims rebuild their lives. On 9 February 2005, President
Bush asked Congress to increase the U.S. commitment to a total of US$950
million. Officials estimated that billions of dollars would be needed.
Bush also asked his father, former President George H. W. Bush, and
former President Bill Clinton to lead a U.S. effort to provide private
aid to the tsunami victims.[123]In mid-March the Asian Development Bank reported that over US$4 billion in aid promised by governments was behind schedule. Sri Lanka reported that it had received no foreign government aid, while foreign individuals had been generous.[124] Many charities were given considerable donations from the public. For example, in the United Kingdom the public donated roughly £330,000,000 sterling (nearly US$600,000,000). This considerably outweighed the donation by the government and came to an average of about £5.50 (US$10) donated by every citizen.
In August 2006, fifteen local aid staff working on post-tsunami rebuilding were found executed in northeast Sri Lanka after heavy fighting, the main umbrella body for aid agencies in the country said. There had been reports and rumors that the local aid workers had been killed.
Economic impacts
The level of damage to the economy resulting from the tsunami depends on the scale examined. While local economies were devastated, the overall impact to the national economies was minor. The two main occupations affected by the tsunami were fishing and tourism.[125] The impact on coastal fishing communities and the people living there, some of the poorest in the region, has been devastating with high losses of income earners as well as boats and fishing gear.[126] In Sri Lanka artisanal fishery, where the use of fish baskets, fishing traps, and spears are commonly used, is an important source of fish for local markets; industrial fishery is the major economic activity, providing direct employment to about 250,000 people. In recent years the fishery industry has emerged as a dynamic export-oriented sector, generating substantial foreign exchange earnings. Preliminary estimates indicate that 66% of the fishing fleet and industrial infrastructure in coastal regions have been destroyed by the wave surges, which will have adverse economic effects both at local and national levels.[127]While the tsunami destroyed many of the boats vital to Sri Lanka's fishing industry, it also created demand for fiberglass reinforced plastic catamarans in boatyards of Tamil Nadu. Since over 51,000 vessels were lost to the tsunami, the industry boomed. However, the huge demand has led to lower quality in the process, and some important materials were sacrificed to cut prices for those who were impoverished by the tsunami.[128]
But some economists believe that damage to the affected national economies will be minor because losses in the tourism and fishing industries are a relatively small percentage of the GDP. However, others caution that damage to infrastructure is an overriding factor. In some areas drinking water supplies and farm fields may have been contaminated for years by salt water from the ocean.[129] Even though only coastal regions were directly affected by the waters of the tsunami, the indirect effects have spread to inland provinces as well. Since the media coverage of the event was so extensive, many tourists cancelled vacations and trips to that part of the world, even though their travel destinations may not have been affected. This ripple effect could especially be felt in the inland provinces of Thailand, such as Krabi, which acted like a starting point for many other tourist destinations in Thailand.[130]
Both the earthquake and the tsunami may have affected shipping in the Malacca Straits, which separate Malaysia and the Indonesian island of Sumatra, by changing the depth of the seabed and by disturbing navigational buoys and old shipwrecks. In one area of the Strait, water depths were previously up to 4,000 feet (1,200 m), and are now only 100 feet (30 m) in some areas, making shipping impossible and dangerous. These problems also made the delivery of relief aid more challenging. Compiling new navigational charts may take months or years. However, officials hope that piracy in the region will drop off as a result of the tsunami.[131]
Countries in the region appealed to tourists to return, pointing out that most tourist infrastructure is undamaged. However, tourists were reluctant to do so for psychological reasons. Even beach resorts in parts of Thailand which were completely untouched by the tsunami were hit by cancellations.[132]
Environmental impact
According to specialists, the main effect is being caused by poisoning of the freshwater supplies and of the soil by saltwater infiltration and a deposit of a salt layer over arable land. It has been reported that in the Maldives, 16 to 17 coral reef atolls that were overcome by sea waves are completely without fresh water and could be rendered uninhabitable for decades. Uncountable wells that served communities were invaded by sea, sand, and earth; and aquifers were invaded through porous rock. Salted-over soil becomes sterile, and it is difficult and costly to restore for agriculture. It also causes the death of plants and important soil micro-organisms. Thousands of rice, mango, and banana plantations in Sri Lanka were destroyed almost entirely and will take years to recover. On the island's east coast, the tsunami contaminated wells on which many villagers relied for drinking water. The Colombo-based International Water Management Institute monitored the effects of saltwater and concluded that the wells recovered to pre-tsunami drinking water quality one and a half years after the event.[134] IWMI developed protocols for cleaning wells contaminated by saltwater; these were subsequently officially endorsed by the World Health Organization as part of its series of Emergency Guidelines.[135]
The United Nations Environment Programme (UNEP) is working with governments of the region in order to determine the severity of the ecological impact and how to address it.[needs update][136] UNEP has decided to earmark a US$1,000,000 emergency fund and to establish a Task Force to respond to requests for technical assistance from countries affected by the tsunami.[137] In response to a request from the Maldivian Government, the Australian Government sent ecological experts to help restore marine environments and coral reefs—the lifeblood of Maldivian tourism. Much of the ecological expertise has been rendered from work with the Great Barrier Reef, in Australia's northeastern waters.
Other effects
- Psychological trauma
- Conflicts and a cease-fire
The widespread devastation caused by the tsunami led the main rebel group GAM to declare a cease-fire on 28 December 2004 followed by the Indonesian government, and the two groups resumed long-stalled peace talks, which resulted in a peace agreement signed 15 August 2005. The agreement explicitly cites the tsunami as a justification.[140]
- Media coverage
- Fraud, false alarms, and panic
- Impact on Sweden
- Tsunami warning system
- Effect on the Earth
In popular culture
Apung 1
- Apung 1, a 2600-ton ship, was flung some 2–3 km inland by the tsunami, and has become a popular tourist attraction in Banda Aceh
Films and television
- Children of Tsunami: No More Tears (2005), a 24-minute documentary film
- Tsunami: The Aftermath (2006), a two-part television miniseries about its after-effects
- The Impossible (2012), an English-language Spanish film based on the story of María Belón and her family
- Dasavathaaram (2008), a Tamil disaster film which culminates with 2004 Tsunami
- Kayal (2015), a Tamil drama film which culminates with the 2004 Tsunami
- The Wave That Shook The World (2005), a PBS NOVA educational television-series documentary about the 2004 tsunami.
- Hereafter (2010), a main character's life is affected after surviving the tsunami while on vacation.
Museum
- Aceh Tsunami Museum, located in Banda Aceh, Indonesia, was designed as a symbolic reminder of the 2004 Indian Ocean earthquake and tsunami disaster, as well as an educational center and an emergency disaster shelter in case the area is ever hit by a tsunami again.
Rediscovery of Mahabalipuram
- Another result of the tsunami, respective of Indian culture, was the water that washed away centuries of sand from some of the ruins of a 1,200-year-old lost city at Mahabalipuram on the south coast of India. The site, containing such notable structures as a half-buried granite lion near a 7th-century Mahablipuram temple and a relic depicting an elephant, is part of what archaeologists believe to be an ancient port city that was swallowed by the sea hundreds of years ago.[149][150]
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