What are tsunamis‚ and how can we decrease deaths among the human population? Tsunamis are created when underwater tectonic plates rub up against each other creating potential energy and then when they shift‚ the potential energy turns into kinetic energy which create a very fast wave. Geoscience helps us to better understand them through many ways. Once a tsunami starts‚ they won’t stop because of all the energy but there are ways to warn people about them through the uses of geoscience. First
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TSUNAMI Tsunami is a series of water waves caused by the displacement of a large volume of a body of water‚ typically an ocean or a large lake. Earthquakes‚ volcanic eruptions and other underwater explosions (including detonations of underwater nuclear devices)‚ landslides‚ glacier calving’s meteorite impacts and other disturbances above or below water all have the potential to generate a tsunami. The effects of a tsunami are devastating. They are one of the world’s worst natural disasters that
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when plates collide or move away from one another thus they are usually found at the edge of tectonic plates .Volcanoes can also occur in the interior of plates‚ these volcanoes are commonly known hotspots. MOVEMENT OF TECTONIC PLATES 2. Tsunamis can be formed by : Underwater earthquakes Underwater earthquakes are the most common cause of tsunami’s .If an underwater earthquake is large enough‚ significant movements will be made by the ocean floor‚ pushing up the ocean water upward causing
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How tsunamis occur. As one plate subducts below another (moves underneath)‚ pressure builds for many years resulting in a section of the mega-thrust giving away. As this section gives away‚ it ruptures the ocean floor‚ resulting in a massive displacement of water‚ causing a tsunami. Tsunamis are barely felt as a ripple on the ocean’s surface‚ but as the waves reach land‚ they increase in size as the water becomes shallower. Japan earthquake and tsunami At 2:46pm Japanese time‚ on March 11th
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Creative Destruction and the Aftermath of the Tsunami: Recovery of Southern Sri Lankan Small Business in the Face of Inertia Dr. C. Travis A. Perera Senior Consultant‚ Entrepreneurship‚ Business Development & Operations Management Postgraduate Institute of Management‚ Sri Lanka Telephone number: 94-777 756 109 Fax number: 94-11-2689643 Email: drtravisperera@gmail.com Paper Presented At the 5th International Entrepreneurship Forum held in Cape Town‚ South Africa from September 07-09-2005
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THE AFTERMATH OF THE TSUNAMI AND CONSEQUENTIAL POVERTY SUBJECT: LAW AND POVERTY SUBMITTED BY: NISHANT K PRASAD 2010-50 SUBMITTED TO: PROFESSOR AMITADHANDA DEAN(ACADEMICS) NALSAR UNIVERSITY OF LAW‚ HYDERABAD A large number of people to the extent of 220‚000 people were killed in the tsunami which hit South Asia in 2004. There were disastrous consequences of this natural calamity. Loss of millions
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Japan Earthquake and Tsunami 2011 After doing research on significant events that occurred in the past 12 months within the Pacific Rim‚ the topic I finally decided to do my research report on was the recent earthquake and tsunami that devastated Japan’s many cities. I chose this topic because I was really interested about learning more about the issue and how significant
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2004 Boxing Day Tsunami | Source 1 | Source 2 | Source 3 | Source 4 | Name of Topic | Tsunami Flash | The Tsunami Page | The Boxing Day 2006 Tsunami | 2004 Tsunami Disaster | Name of Author | The Age | Dr George P.C | Phil Cummins | Matthew Clieok | Address | http://www.theage.com.au/tsunamiflash/ | http://www.drgeorgepc.com/Tsunami2004Indonesia.html | http://www.ga.gov.au/ausgeonews/ausgeonews200503/tsunami.jsp | http://www.ciolek.com/WWWVLPages/AsiaPages/Tsunami-Analyses.html | Notes
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4038600-137160How Are Tsunami’s Made -Initiation The sea floor rises and drops suddenly creating large columns of water -Split ddsddsThe initial tsunami then splits into two‚ one heads further into sea another heads towards shore -Amplification As the wave appdsroaches shore‚ the height of the wave is amplified as the wave gathers energy as approaches shore -Run Up The leading wave is steepened‚ the wave does not break at this point‚ instead it acts like a wall of water smashing everything
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GAC013 Assessment Event2: Case Study Investigation Compare and Contrast Tsunamis and Volcanic Eruption Forecasting Student’s Name: Sissy Wang Student ID#: SHSA16374 Teacher: Kenny Due Date: 14th December 2011 Word Count: 1‚194 Table of Contents 1. Abstract Page 2 2. Introduction Page 2 3. Methodology Page 4 4. Finding Page 4 5. Discussion Page 6 6. Conclusions and Recommendations Page 6 7. Reference Page 7 Abstract With the development of science
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