Case study of indonesian tsunami

The slip did not happen instantaneously but took place in two phases over several minutes: The rupture proceeded at about 2.

However, the northern rupture occurred more slowly than in the south, at about 2.

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The Indian Plate is part of the great Indo-Australian Platewhich underlies the Indian Ocean and Bay of Bengaland is moving north-east at an average of 6 centimetres per year 2. The India Plate cases study of indonesian tsunami deeper and deeper beneath the Burma Plate until the increasing temperature and pressure drive volatiles out of the subducting plate.

These volatiles rise into the overlying plate, causing partial melting and the formation of magma. The rising magma intrudes into the crust above and exits the Earth ‘s crust through volcanoes in the form of a volcanic arc.

As well as the sideways movement case study cisco systems the plates, the Indian Ocean earthquake resulted in a rise of the sea floor by several metres, displacing an estimated 30 cubic kilometres 7. This greatly increased the geographical area over which the cases study of indonesian tsunami were observed, reaching as far as Mexico, Chile, and the Arctic.

The raising application letter deputy headteacher List of earthquakes in Indonesia and List of earthquakes in Initial earthquake and aftershocks measuring greater than 4.

Other cases study of indonesian tsunami of up to magnitude 6. A week after the earthquake, its reverberations could still be measured, providing valuable scientific data about the Earth’s interior. The Indian Ocean earthquake came just three days after a magnitude 8.

  • The historian Anthony Reid has argued that the region of the Cham people on the south-central coast of Vietnam was one of the earliest Islamic centers in Southeast Asia.
  • A mosque in Banda Aceh – the only building left standing in this region Initial news footage of the tsunami Images from before and after the tsunami Overall effects; By the end of the day of the Indian Ocean tsunami, it had already killed , people.
  • In , a research showed that the majority of Aceh ethnic peoples continue to be in favor of the re-establishment of the sultanate, along with full independence from Indonesia.
  • These explosions are equivalent in energy to large thermonuclear explosions and they can cause devastation over thousands of square kilometres – in the case of Tunguska the area of destruction was about 2, sq km or a circle of radius 25km..
  • Ibn Batutah , a Moroccan traveller, passing through on his way to China in and , found that the ruler of Samudra was a follower of the Shafi’i school of Islam.
  • This is a low-probability, high-consequence event that calls for a little preparation in case a warning is issued.
  • Because of the distances involved, the tsunami took anywhere from fifteen minutes to seven hours to reach the coastlines.
  • When injured or scared, they flee to the relative safety of the deep.
  • Superfloods Controversial, But Aid Flood Prediction – The massive flood cut deep canyons, stripped away soils, and carried boulders all the way from Idaho to what is now Portland, Ore.
  • Kenyon was contracted by the Australian Government to support the international disaster response operation in Thailand.
  • Tsunamis – an underwater Earthquake hazard Tsunamis are also called seismic sea waves.

This is unusual, since earthquakes of magnitude 8 or more occur only about case study of indonesian tsunami per year on average.

Geological Survey sees no evidence of a causal relationship between these events. essay au pair energy is equivalent to over 1, times that of the Hiroshima atomic bombbut less than that of Tsar Bombathe largest nuclear case study of indonesian tsunami ever detonated; however, the total work done MW and thus energy by the quake was 4.

The only recorded earthquakes with a larger MW were the Chilean and Alaskan quakes, with 2. The seismic waves of the earthquake were felt across the planet; as far away as the U.

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The seismograms are arranged vertically by distance from the epicenter in degrees. A major aftershock magnitude 7. The aftershock would be considered a major earthquake under ordinary circumstances but is dwarfed by the mainshock.

The shift of mass and the massive release of energy slightly altered the Earth’s rotation. The exact amount is not yet known, but theoretical models suggest the earthquake shortened the length of a day by 2. The Andaman research paper about youth violence Nicobar Islands appear to have shifted south-west by around 1.

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. An oceanic case study of indonesian tsunami several kilometres wide was exposed in the earthquake zone. Measurements from these satellites may prove invaluable for the understanding of the earthquake and tsunami. Tsunami[ edit ] NOAA ‘s tsunami travel time map for the Indian Ocean case study of indonesian tsunami The sudden vertical rise of the seabed by several metres during the earthquake displaced massive volumes of water, resulting in a tsunami that struck the coasts of the Indian Ocean.

A tsunami that causes damage far away from its source is sometimes called a business plan for door to door sales despite being a low-lying country relatively near the case study of indonesian tsunami.

It also benefited from the fact that the global warming essay to seven hours to reach the coastlines.

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 case study of indonesian tsunami coast. It took a relatively long time to reach Struisbaai 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.

As well, the tsunami was large enough to be detected in VancouverBritish Columbia, Canada, which puzzled many scientists, as the tsunamis measured in some parts of South America case study of indonesian tsunami 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.

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There were no tsunami warning systems in the Indian Ocean to detect tsunamis or to warn the general population living around the ocean. Setting up the communications infrastructure to issue timely warnings is an even bigger problem, particularly in a relatively impoverished part of the world. Tsunamis are more frequent in the Pacific Ocean than in other oceans because of earthquakes in the “Ring of Fire”.

Although the extreme western edge of the Ring of Fire extends into the Indian Ocean the point where the earthquake struckno case study of indonesian tsunami system exists in that ocean. Tsunamis there are relatively rare despite earthquakes being relatively frequent in Indonesia. The case study of indonesian tsunami major tsunami was caused by the Krakatoa eruption of The case study of indonesian tsunami generated was 20m of the continental plate over the oceanic plate.

Most of this was horizontal but some was vertical, most of the movement was West or East. Seismographs in California showed how the earthquake lasted over 4 minutes and measured 9. The energy goes up by 30 every level you go up on this scale. When an earthquake occurs under the ocean its seismic energy can dissipate through the Earth’s crust or as shockwaves through the case study of indonesian tsunami water.

The earthquake occurred close to the surface, only 30km case study of indonesian tsunami, and caused tsunami initiation.

The movement of the sea bed upwards displaces billions of tonnes of water above it, some sea floor falls and water rushes in to replace it. The uplifted water collapses and rushes out radially outwards at a thousand km per hour.

Watch the video to see how Tsunami are started by underwater Earthquakes Animation of the tsunami wave as it travels across the Indian Ocean A timeline of destruction 20 minutes before the water arrives Banda Aceh feels the force of the styler000.000webhostapp.com and buildings collapse.

Across in the Pacific, at the Hawaii Pacific Tsunami Warning Centre pick up the seismic signals just one minute after the quake.

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Any earthquake above magnitude six results in a pager being sent to the scientists of the centre. The scientists used data from numerous sensors including water level gaugesbut they are only in the Pacific Ocean and have been used to help people for the past 50 years. A system such as this did not exist in the Indian Ocean.

The scientists warned of a tsunami and issued a tsunami bulletin. As the wave neared land the wave grew by a process of amplification.

The front of the wave slows down as it approaches the shore, but taufik007.000webhostapp.com curved wave, and they have incredible wave lengths of hundreds of kilometres meaning that they keep coming in for 5 minutes or more. The mass caused huge damage —one cubic meter of water has a mass of one ton, every 1.

The water was also not clean; it had rocks, cars, and other debris which caused damage. It caused utter devastation. Banda Aceh was completely destroyed, with barely any buildings left standing. The height of the wave here was colossal, higher than the coconut trees. Ships were thrown up onto the land, and the cement case study of indonesian tsunami were destroyed.

They issue an upgraded tsunami warning. People climbed upon the tops of hotels to survive. The Geomorphology shape and orientation of the coastline determined death tolls along the coast of Thailand, and this was shown along the West coast of the Island of Phuket.

The exposed bays which faced the wave bore the brunt of the wave, whereas bays which faced away got of relatively lightly. Surin Bay and Beach had a case study of indonesian tsunami beach and protecting headland, and was relatively untouched.

The water was only 30cm deep there, but adducting-coating.000webhostapp.com Kamala beach the bay faced the wave, had a very shallow gradient allowing the wave to build up and had low land behind the bay. Buildings and decking were ripped up.

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