For the Press‚ For the People‚ For your Life. Embedded Journalism Issue Paper [pic] Written by: Sabrina Browne A New Target of War Introduction Section Have you ever wondered what it was like to be a news reporter? Not just any reporter‚ but a war correspondent? To be in the middle of a war‚ watching it with your very own eyes? It sounds exciting‚ riveting in fact. Picture yourself‚ standing there with microphone in your hand‚ while gun shots and grenades are
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EMBEDDED JOURNALISM 1. In the realm of media-military relations‚ Operation Iraqi Freedom (OIF) has become synonymous with the concept of ‘embedding’. The Pentagon defines ‘embed’ “as a media representative remaining with a unit on an extended basis”[i] and OIF represents the single greatest instance of embedding. The Pentagon offered 920 embed spots‚ and‚ from 775 acceptances‚ eventually managed about 600 positions from more than 250 national and international media agencies[ii]. The British Ministry
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context. As evident from the above definition of e-learning‚ the Internet or Web is an integral part of the delivery of training and learning. With growing Internet speeds and decreasing hardware costs the Web is becoming a major part of every-day’s life. More recently‚ Web 2.0 has become a buzz-word in education and wider circles which has transformed the way people have used the Web‚ from passive to active users (Cleary‚ 2008). Although there is no clear definition of Web 2.0‚ it is considered as
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making it susceptible to earthquakes CONSTRUCTION OF EARTHQUAKE RESISTENT BUILDINGS IN SEISMIC ZONES OF INDIA Earthquakes occur due to movements along faults that have evolved through geological and tectonic processes. Often they occur without any prior warning and are‚ therefore‚ unpredictable. The large area of India is prone to earthquake. The construction of earthquake resistant building is the only solution for safeguarding our urban centres from the menace of earthquakes. On the basis of
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Underwater earthquake causing Tsunami. * The 2004 Indian Ocean earthquake was an undersea megathrust earthquake that occurred at 00:58:53UTC on Sunday‚ 26 December 2004‚ with an epicentre off the west coast of Sumatra‚ Indonesia. The quake itself is known by the scientific community as the Sumatra–Andaman earthquake. The resulting tsunami was given various names‚ including the 2004 Indian Ocean tsunami‚ South Asian tsunami‚ Indonesian tsunami‚ and the Boxing Day tsunami. * The earthquake was caused
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2013 a calamity so unexpected and tragic struck the islands in Central Visayas. Recorded as the deadliest earthquake that struck the Philippines in 23 years‚ fear‚ anxiety and panic were felt all throughout the area. Houses collapsed‚ buildings got destroyed and churches had fallen. More crucially‚ lives had been taken. Currently‚ we’re still within weeks after the 7.2 magnitude earthquake‚ hit into the peaceful surfaces of Bohol and Cebu. The destruction brought about by the quake is heartbreaking—over
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Earthquakes are one of the most destructive of natural hazards. Earthquake occurs due to sudden transient motion of the ground as a result of release of elastic energy in a matter of few seconds. The impact of the event is most traumatic because it affects large area‚ occurs all on a sudden and unpredictable. They can cause large scale loss of life and property and disrupts essential services such as water supply‚ sewerage systems‚ communication and power‚ transport etc. They not only destroy villages
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Earthquakes An earthquake is a shaking or trembling of the crust of the earth caused by underground volcanic action or by the breaking and shifting of rock beneath the surface. The volcanic action and shifting rocks create strain which continues to build to a sudden release of pressure resulting in a shock wave. The vibrations produced in the crust can vary from barely noticeable to enormously destructive. Shock waves can be classified into two broad categories. Waves that send particles oscillating
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2011 Christchurch earthquake From Wikipedia‚ the free encyclopedia Jump to: navigation‚ search "Christchurch earthquake" redirects here. For other uses‚ see Christchurch earthquake (disambiguation). For the 13 June 2011 aftershock‚ see June 2011 Christchurch earthquake. February 2011 Christchurch earthquake | ChristChurch Cathedral and the Cathedral Square | Quake epicentre | Date | 22 February 2011 (2011-02-22)‚ 12:51 pm NZDT | Magnitude | 6.3 ML[1] | Depth | 5 km (3.1 mi) | Epicenter
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INTRODUCTION 1 HOW EARTHQUAKES OCCUR 2 Fault types 3 Earthquake fault types 3 Different types of Faults 3 Tidal forces 5 Earthquake clusters 6 Aftershock 6 Earthquake swarm 6 Earthquake storm 6 METHODS USED IN MEASURING EARTHQUAKES 6 The Richter Scale 6 The Mercalli Scale 7 HAZARDS CONNECTED TO EARTHQUAKES 8 MEASURES TAKEN TO MINIMIZE EARTHQUAKES 9 BIBLIOGRAPHY 11 INTRODUCTION Earthquakes are caused by the movement of the earth’s tectonic plates. Earthquakes occur where the earth’s
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