PPT-Earthquake Hazards in the Central U.S.
Author : liane-varnes | Published Date : 2017-08-31
Brian Blake Central US Earthquake Consortium MEMA SAR Planning Meeting July 24 2013 Senatobia Mississippi Overview of CUSEC Formed in 1983 Result of a growing
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Earthquake Hazards in the Central U.S.: Transcript
Brian Blake Central US Earthquake Consortium MEMA SAR Planning Meeting July 24 2013 Senatobia Mississippi Overview of CUSEC Formed in 1983 Result of a growing body of research Partnership effort between State and Federal Government. Are You Prepared To Ride It Out? We have heard it so many times –the “big one” is coming. In our lifetime, we still haven’t seen or felt that huge earthquake. That shouldn’t stop us from preparing. Magnitude 2.9 LOUGHBOROUGH, LEICS, UK . Friday, 18 January, 2013 at 05:20:44 UTC. The earthquake was felt in the towns of . Loughborough. , Derby, Nottingham and Leicester. Shaking was felt as far away as Buxton and Warwick.. Hazard . Prediction Based on Seismicity . Simulation. . Shiyong. Zhou Russell Robinson . Xiaofei. Chen . M. Jiang . X. . Jin. . B. Gao . :. Analyzing Tweets for Real-Time Event Detection. Takehi. . Sakaki. Makoto Okazaki Yutaka Matsuo. @. tksakaki. @okazaki117 @. ymatsuo. . the University of Tokyo. Introduction. Occurred just before midday on 25 April 2015. 7.8 Magnitude at a depth of around 15 . kilometres. The . epicentre. was the village of . Barpak. in the . Gorkha. district. The tremors were felt as far away as India, Pakistan and Bhutan.. Tectonic activity and hazards. PowerPoint presentation by . Médecins Sans Frontières / Doctors Without Borders (MSF)UK. Schools Team: Mary Doherty and Severa von . Wentzel. March 2013. . MSF. Geography Working Group. Hazards are produced from the response of energy released. Amount and duration are related to the amount of energy released. Which hazards do you know?. Earthquake Hazards. Tsunami: displacement of a large volume of water. Briefly, “explain” the intent of this cartoon. Why do earthquakes occur?. Which of the following diagrams represents a normal fault? What is your evidence? . A.. B. .. TPS – What is going on here?. Tectonic plates are huge rock pieces within the earth’s crust. The plates are usually marked by fractures or fault lines formed when the plates tear apart or slide or collide past each other. This results in a change of the earth’s interior masses which send out powerful shock waves with enough force to alter the surface of the earth. The shock waves can thrust up cliffs and open huge cracks on the ground leading to an earthquake event. Earthquake Risk. Earthquakes are likely wherever plate movement stores energy in the rock along faults.. Geologists can determine earthquake risk by locating where faults are active and where past earthquakes have occurred.. So you think you have a safe office job.. You spend most of your day sitting in a chair. What could go wrong? The National Safety Council says employees are two-and-a-half times more likely to suffer a disabling fall in an office setting than anywhere else. How to avoid them?. Earthquake Country Alliance. Cisco, San Jose, March 1. , 2018. SAFRR: Science Application for Risk Reduction. SAFRR: Science Application for Risk Reduction …. NATURAL HAZARDS MISSION AREA Earthquake Hazards Program. (Lesson 22). ENQUIRY QUESTION 3:. How successful is the . management. of tectonic hazards and disasters?. H/W :TASK 4. Read the information . (Hodder page 90 in this booklet) . about two recent tectonic mega disasters : . Earthquakes. Earthquakes occur throughout the world but predominately on. plate boundaries. . For example the San Andreas Fault, a conservative plate margin. Furthermore, earthquakes also occur on the constructive plate boundaries of the Mid- Atlantic Ridge, although these are not as severe.
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