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Geology Journal

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September 24 2013 Earthquake

U.S Geological Survey

A magnitude 7.7 earthquake hit Awaran, Pakistan due to a strike-slip occurring between the plates. The plates collided between the transition zone between the northward subduction of the Arabic plate beneath the Eurasia plate. The epicenter of the event occurred 69km north of the Awaran, Pakistan border. The earthquake killed at least 825 people and injured hundred of others. The Balochistan government estimated that the earthquake had destroyed at least 21,000 homes. In the past 40 years, only one significant earthquake had injured humans in that area. The earthquake occurred along the two plate boundaries of the region, the area where typically most earthquakes occur due to collision of plates by convergent or transform boundaries. Due to the poor economic area in which the earthquake took place, many homes collapsed easily as many were not reinforced like many buildings are now in the United States. As the location of the city was so close to the epicenter, the city felt a high intensity level. The reason for the creation of the earthquake deals with the Elastic Rebound Theory that states crust bends as strains builds up until the earthquake occurs making bent crust snap back into place. While detection devices have been created such as seismograph, many devices to forewarn individuals of future earthquakes have still not been created. Spatial trends have been one concept in preparing individuals for upcoming earthquakes for looking for gaps between seismic activities over a period of time. A reoccurrence method is also a possible predictor as it predicts future earthquakes based off intervals of earthquake activity over the years. Both systems have flaws and would not be able to perfectly predict future seismic activity. Actions to mitigate the damages would have been a faster response to the event.

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