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Sendai earthquake 2011 case study

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As of , a majority of the mega projects that involved restoration actions have been completed, which indicates a more effective rate of completion compared with the MLIT projects performed in normal non-disaster situations. This short article explains the management process of the recovery and reconstruction utilized by the TRB—an inter-organizational process—from a business process management BPM perspective and creates a simple organization construction diagram of the entire process. The study focused on the transactions and actor roles to identify their strengths. The findings indicate the utilization of different operational procedures in some parts of the process, the importance of liaison role, as well as some obstacles.
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Response to the 2011 Great East Japan Earthquake and Tsunami disaster

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Japan Earthquake - Internet Geography

This earthquake caused 60 deaths, 9, people injured. What was actually the main cause of the Northridge earthquake? Why did the Northridge earthquake caused so many destruction? The earthquake happened because of the movement from the San Andreas Fault u-s-history.
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Japan earthquake 2011 Case Study

Please join StudyMode to read the full document. I chose this topic because I was really interested about learning more about the issue and how significant it actually was. My purpose in writing this research essay is simply to explore and explain in detail where and why these natural disasters occurred, the background history of the issue, and how Japan has been affected environmentally, socially, and economically by these events.
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Researchers at the Institute of Geomatics -- Research Centre of the Polytechnic University of Catalonia UPC and the Government of Catalonia -- have estimated the ground deformation suffered in the area of Sendai, Japan, as a consequence of the earthquake of March 11, and its aftershocks. The estimate was derived from radar observations acquired by the Envisat satellite of the European Space Agency. According to this estimate, obtained over an area of approximately x km around the city of Sendai, the terrain has suffered a co-seismic deformation -- permanent deformation of Earth's surface -- associated with the earthquake of up to 1. The estimated value of 1. The minimum distance from the epicentre to the study area is km approximately.
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