The December 26, 2004 M=9.1 Sumatra-Andaman earthquake occurred along a tectonic subduction zone in which the India Plate, an oceanic plate, is being subducted beneath the Burma micro-plate, part of the larger Sunda plate.. The earthquake was followed by a wide hazardous tsunami which intensified the catastrophic consequences of the disastrous earthquake.Since 1900, the 2004 Sumatra earthquake with magnitude of Mw=9.1 is considered as the third-largest earthquake ever recorded on a seismograph and had the longest duration of faulting ever observed, between 8.3 and 10 minutes. Stringer/Getty Images.
About 47,000 more people died, from Thailand to … A subduction earthquake, with a Richter magnitude of 9.3, occurred on December 26, 2004, off the coast of the Indonesian island of Sumatra, at 7:59 a.m. local time. He works as a research guide for the U.S. Geological Survey. The quake itself is known by the scientific community as the Sumatra-Andaman earthquake. The GSN data includes some eye-popping facts. The tsunami generated by the earthquake was recorded nearly world-wide and killed more people than any other tsunami in recorded history, almost 230,000 missing and presumed dead. Extensive seismic damage to engineering infrastructure occurred in northern and north-western Sumatra. The interface between the two plates results in a large fault, termed an interplate thrust or megathrust. On 26 December 2004, a magnitude 9.1 earthquake (3.316 N, 95.854 E, depth 30 km) occurred off the coast of northern Sumatra, Indonesia.
The Sumatra Earthquake of December 26, 2004 Share Flipboard Email Print Banda Aceh after the 2004 earthquake and five years later. The tsunami was caused by an underwater earthquake which measured 9.15 on the Richter scale.
This tsunami caused death of more than 230,000 people and is considered as Compare this to 1964, when the machines of the World Wide Standardized Seismic Network were knocked off scale for hours by the March 27 Alaskan quake. The tsunami heights in some places were extremely high. ThoughtCo uses cookies to provide you with a great user experience and for our Measuring Earthquake Intensities Using Seismic Scales (A startling De catastrofe wordt gezien als een van de ergste natuurrampen in de recente geschiedenis.
That was a scandal. IRIS, the Incorporated Research Institutions for Seismology, has compiled scientific results from the Sumatra earthquake on a
In addition, about 125,000 were injured, 45,752 were missed and more than 600,000 became homeless and displaced. Andrew Alden is a geologist based in Oakland, California. Just a video! A minute before 8 o'clock in the morning local time, a colossal On December 26, 2004, a large (magnitude 9.0) earthquake occurred off the western coast of Sumatra in the Indian Ocean. This pulse was detectable for several months afterward. At every spot on Earth, the ground was raised and lowered at least a full centimeter by the seismic waves from Sumatra. A powerful undersea earthquake that struck off the coast of Sumatra island, Indonesia, set off the 2004 Indian Ocean tsunami, also known as the Christmas or Boxing Day tsunami, on Sunday morning, Dec. 26, 2004. If each school in Sri Lanka, each mosque in Sumatra, each TV station in Thailand had shown such a video once in a while, what would the story have been instead that day? A magnitude 9.0 earthquake - the largest in 40 years - struck offshore of the Indonesian island of Sumatra on December 26, 2004. Amongst the affected countries was Somalia in Africa which is almost 3000 miles from the epicenter of the earthquake.Please donate £1 to help YPTE to continue its work of inspiring young people to look after our world.The Young People's Trust for the Environment is a charity which aims to encourage young people's understanding of the environment and the need for sustainability. The earthquake that generated the great Indian Ocean tsunami of 2004 was an undersea megathrust earthquake that occurred at 7:59 am local time on Sunday, 26 December 2004. In December 26, 2004, there were no tsunami warning systems in the Indian Ocean to detect tsunamis or to warn the general populace living around the ocean which could save many lives in the time interval between the earthquake and tsunami.The 2004 Indian Ocean earthquake was one of the deadliest natural disasters in recorded history, killing 230,000 people in 14 countries. The earthquake was caused by the release of stresses accumulated as the Burma tectonic plate overrides the India tectonic plate. The magnitude 9.1 quake ruptured a 900-mile stretch of fault line where the Indian and Australian tectonic plates meet. At the time, commentators from the scientific community decried the absence of a tsunami warning system in the Indian and Atlantic oceans, 40 years after the Pacific's system began. From the view point of seismology, the earthquake was caused by a subduction activity at a depth of 30 km below mean sea level. Seismic energy was released at such long wavelengths that they were a substantial fraction of the Earth's circumference. Sumatra, Indonesia Earthquake of 26 December 2004, Mw=9.1. More: Tsunami wave height as measured by satellites two hours and five minutes after the event. The earthquake triggered a series of devastating tsunamis along the coasts of most landmasses bordering the Indian Ocean, inundating coastal communities with waves up to 30 meters high. The epicenter of the earthquake was located in the Indian Ocean at the coordination of 3.295N and 95.982E. Over the next seven hours, a tsunami—a series of immense ocean waves—triggered by the quake reached out across the Indian Ocean, devastating coastal areas as far away as East Africa. A video about the 1998 New Guinea tsunami—was all it took to save the lives of a whole village in Vanuatu in 1999. Asian Tsunami in Sumatra, Indonesia - 26 December 2004. The tsunami generated by the earthquake was recorded nearly world-wide and killed more people than any other tsunami in recorded history, almost 230,000 missing and presumed dead.
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