2010 chile earthquake

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The rupture began deep beneath the coast and spread into western, northern and southern directions. Both geological and socio-political reasons can be cited. The 2010 Chile earthquake was caused by the movement of convergent plate boundaries.

At first, its magnitude was reported to be between 8.3 and 8.5 on the Moment magnitude scale, but this was later corrected upwards, to be at 8.8 of that scale. Nevertheless, the International Charter “Space and Major Disasters” (http://www.disasterscharter.org) was activated. En tant que membres du Mouvement international de la Croix-Rouge et du Croissant-Rouge, nous sommes guidés dans notre travail par sept Principes fondamentaux: humanité, impartialité, neutralité, indépendance, volontariat, unité et universalité. The effects were far more strongly felt in the cities of Conception (Chile’s second city) and Chillan, both about 100 km away. She also confirmed the deaths of at least 795 people.[8][9]. It was the 5th strongest earthquake ever recorded, and has been followed by numerous aftershocks, some as high as magnitude 6.9 (for comparison: the January earthquake in Haiti had a magnitude of 7.0). Chile is largely located on the boarders of the oceanic Nazca plate and the continental South American plate. During the twentieth century, Chile has been struck by twenty-eight major earthquakes, all with a force greater than 6.9 on the Richter scale. This time the Pacific Tsunami Warning System functioned very well. Chile had learnt from previous large earthquakes, such as the magnitude 9.5 earthquake in 1960, for example implementing strict building codes for shake-resistant buildings, and preparing its population on how to behave during and after a large quake. Just south of Concepción, the source of this years 2010 earthquake adjoins a fault rupture nearly 1,000 km long that produced the largest 20th-century earthquake worldwide – the giant 1960 earthquake of magnitude 9.5, the largest earthquake ever recorded. How can this be explained? The two plates are converging at roughly 7 to 10 meters per century. This includes teaching how to use spatial data to assess hazard and risk, as well as risk mitigation, and disaster preparedness and management approaches. Although there are different theories as to why this was the case, the most convincing is the fact that the earthquake had its largest stress release in relatively shallower waters compared to the other two tsunami generating events. It was MW 6,9 in the Richter scale. From Simple English Wikipedia, the free encyclopedia, For a list of earthquakes in 2010 in Chile, see, Subsecretaría del Interior de Chile (31 January 2011). The epicenter was located at 35.909°S, 72.733°W (just offshore), at a depth of about 35 km. This is when 2 tectonic plates converge, move towards each other, and depending on the nature and type of plate, it is classified as either a subduction or collision boundary. The sudden vertical movement of the ocean floor also caused a tsunami along the fault-rupture area. [4] It was the strongest earthquake in Chile since the magnitude 9.5 1960 Valdivia earthquake, and the strongest earthquake worldwide since the 2004 Indian Ocean earthquake. The event was felt as far away as Southern Peru, Bolivia and Buenos Aires (Argentina), and lasted up to 30 seconds. This large displaced water column turns into a large tsunami wave when approaching the coast, entering into shallow coastal waters, leading to increased wave heights. In Figure 4 examples are shown of the diverse mapping carried out following the Chile earthquake (click for larger versions). These waves affect the whole column of water between the surface and the sea floor as they move, from the region of origin in the middle of the sea, towards the coast. This subduction of the Nazca plate beneath the South American plate is causing high stress beneath Chile, making the country highly prone to large magnitude earthquakes. meant that many fatalities can be attributed to help coming too late. No coordinated warnings were issued, many coastal regions never received any warning, and in those who did, communities had little to no idea what to do with the warning. [1], The earthquake was also felt in the Chilean capital Santiago as well as in some Argentinean cities. La Fédération internationale des Sociétés de la Croix-Rouge et du Croissant-Rouge est le plus vaste réseau humanitaire au monde. Pour le tremblement de terre de 2014, voir 2014 tremblement de terre Iquique. The 1960 earthquake in Chile happened in much deeper water, therefore, replacing a much larger water column. ITC also carries out research, such as on modelling the actual local site effects and seismic amplifications, or on how to use remote sensing data to map structural damage. ITC does not engage in rapid damage mapping or in-field support following disasters.
Other cities exposed to Mercalli intensity scale intensity VIII (Destructive) shaking were Arauco, Lota and Constitución. An estimated 1,600 lives were lost to the 1960 earthquake and tsunami in Chile, with the tsunami also taking over 200 lives after reaching Japan, Hawaii, and the Philippines. The earthquake, which has gained wide acceptance as one of the most powerful to ever have occurred in all of history, had its epicenter off the Coast of the Chilean town of Pelluhue. [7] Tsunami warnings were issued in 53 countries. The 2010 Cauquenes earthquake was an earthquake that happened off the coast of Maule region of Chile, near Cauquenes, on February 27, 2010, at 3:34 local time (6:34 UTC). According to the United States Geological Survey (USGS) the Chile earthquake released about 500 times more energy than the 7.0 earthquake that struck Haiti in January.

Risk is seen as a combination of hazard (the seismic potential, or the expected local shaking intensity), and the value and vulnerability of the so-called elements at risk in the area to be affected. The process of subduction boundary that resulted in the massive 8.8 earthquake of Chile in 2010. The capital, Santiago, lies some 330 km NNE, too far to be strongly affected. In addition a number of other organisations has joint disaster mapping efforts in recent years, such as ITHACA (Information Technology for Humanitarian Assistance, Cooperation and Action, http://www.ithaca.polito.it/), USAID (http://www.usaid.gov/), the Joint Research Centers (JRC) of the European Commission (http://ec.europa.eu/dgs/jrc/index.cfm), or G-MOSAIC (http://www.gmes-gmosaic.eu/), an European Commission GMES (Global Monitoring for Environment and Security) service. Most of Chile is located on the border between the oceanic Nazca Plate and the continental South American Plate. Satellite images are obtained on a priority basis, and processed by one of several organisations – typically UNOSAT, the Center for Crisis Information of the German Space Agency (DLR-ZKI), or SERTIT, based at the University of Strasbourg. The structural damage and number of people killed, injured or made homeless are still not clear.

That after 30 hours it turned out that the tsunami was not that strong is only a relief but it was a very strong improvement with respect to earlier events. Although this earthquake was one of the largest that ever happened it only created a relatively small tsunami. Envoyer comme e-card. This was not the case in Haiti, in part due to the long time since the last strong earthquake, the limited financial means of the national economy, and the poorly functioning government. Copyright 2020 - International Federation of Red Cross and Red Crescent Societies - Legal Disclaimer, Pourquoi travailler pour la Fédération internationale, Préparation communautaire aux épidémies et aux pandémies, National Society Preparedness for Effective Response. 2010 Earthquake in Chile by Claudio Nunez. training students (largely from economically less developed countries) on how to use geoinformation science tools and methods for disaster risk management. But also location was important. 2010 tremblement de terre du Chili - 2010 Chile earthquake. US scientists have measured with GPS that the city of Concepcion has moved more than 3 meters to the west.


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