Natural Hazards: Causes and Effects - Disaster Management Center ...
Natural Hazards: Causes and Effects - Disaster Management Center ... Natural Hazards: Causes and Effects - Disaster Management Center ...
The ultimate objective of this course, indeed the purpose of the Disaster Management Center at the University of Wisconsin, is to contribute to those objectives stated by Krimgold. An understanding of the nature of natural hazards is the first step in preparing for them. Being able to anticipate their consequences is a prerequisite not only to appropriate action following disaster events but also to prevention of them. The following lessons seek to provide an introduction to that process. Notes 1 Frederick C. Cuny, Disasters and Development, Oxford University Press, New York, 1983, p. 3. 2 Earthscan, Natural Disasters: Earthscan Press Briefing Document No. 39, International Institute for Environment and Development, London, 1984, p. 16. 3 Cuny, Disasters and Development. p. 14. 4 Earthscan, Natural Disasters, 1984. 5 Cuny, Disasters and Development. p. 39. 6 Ibid. p. 40. 7 Ibid. pp. 40-41. 8 see also J. Eugene Haas, Robert W. Kates, Martyn J. Bowden, Reconstruction Following Disasters, MIT Press, Cambridge, Massachusetts, 1977. 9 see also J. Eugene Haas, Robert W. Kates, Martyn J. Bowden, Reconstruction Following Disasters, MIT Press, Cambridge, Massachusetts, 1977. 10 Pan American Health Organization, A Guide to Emergency Health Management after Natural Disaster, Pan American Health Organization, Washington, D.C., 1981, pp. 3-4. 11 Cuny, Disasters and Development pp. 49-50. 12 Ibid pp. 44-56. 13 Frederick Krimgold, The Role of International Aid for Pre-disaster Planning in Developing Countries, audelringen for Arkitektur, KTH Stockholm, 1974, p. 65.
Chapter 2 Earthquakes Introduction Earthquakes are one of the most dangerous and destructive forms of natural hazards. They strike with sudden impact and little warning. They may occur at any time of day or on any day of the year. An earthquake can devastate an entire city or a region of hundreds of square kilometers. They can reduce buildings to a pile of rubble in seconds, killing and injuring their inhabitants. Earthquakes are caused by the movement of massive land areas, called plates, on the earth’s crust. Often covering areas larger than continents, these plates are in a constant state of motion. As the plates move relative to one another, stresses form and accumulate until a fracture or abrupt slippage occurs. This sudden release of stress is called an earthquake. Historical Examples Managua, Nicaragua, December 23, 1972 On December 23, 1972, a series of earthquakes shook the Central American nation of Nicaragua. The largest earthquake registered 6.2 on the Richter scale. The earthquake’s epicenter was located precisely at the capital city of Managua. The earthquake resulted in the destruction of the heavily populated central zone and damage to a total area of about 27 square kilometers (10 square miles). Subsequent fires blazed throughout the city, compounding the damages. In the wake of the disaster, at least 8,000 of Managua’s total population of 430,000 had died, 20,000 were injured, over 260,000 had fled the city, 50 percent of the employed were jobless, and 70 percent were left temporarily homeless. At least 10 percent of the nation’s industrial capacity, 50 percent of commercial property, and 70 percent of government facilities were rendered inoperative. Overall, the U.S. dollar damage was estimated at $845 million. 1 The city had been destroyed by previous earthquakes, but the capital was always rebuilt and expanded on the same location. It is, therefore, understandable that a major issue after the 1972 earthquake concerned future decentralization or relocation of the city. As is common in many developing countries, the capital is the focal point of the most productive activities, including those of trade, industry, and financial services, as well as the site of the central government. Thus, in addition to the loss of life and to property damage, the cost of temporary upsets in public administration and disruption of economic activity must be taken into account. The sectors that were hardest hit by the earthquake were housing, retail trade, and small manufacturing. These were concentrated in the over-crowded city-center closest to the epicenter of the earthquake. The massive destruction was due in part to their location, but also to inadequate building materials, structural deficiencies, and the absence of laws regulating construction. Although this earthquake was quite localized, it struck directly at the economic and administrative heart of Nicaragua and left its mark for years to come. The public sector entered
- Page 3 and 4: This publication was prepared by th
- Page 5 and 6: Introduction How to Get Started Thi
- Page 7 and 8: eruption may be the saturation of a
- Page 9 and 10: Course Objectives Lesson 1 Introduc
- Page 11 and 12: Lesson 1 - Introduction to Natural
- Page 13 and 14: _____ 9. The transitional period an
- Page 15 and 16: Lesson 2 - Self-Assessment Test Mul
- Page 17 and 18: Lesson 3 - Tsunamis Study Guide Ove
- Page 19 and 20: Lesson 4 - Volcanoes Study Guide Ov
- Page 21 and 22: a) frequency of tremors b) upward m
- Page 23 and 24: Lesson 5 - Self-Assessment Test Mul
- Page 25 and 26: ) two secondary responses handled b
- Page 27 and 28: Lesson 6 - Self-Assessment Test Mul
- Page 29 and 30: Lesson 7 - Drought Study Guide Over
- Page 31 and 32: ) often easier than implementing th
- Page 33 and 34: Lesson 8 - Self-Assessment Test Mul
- Page 35 and 36: Lesson 9 - Deforestation Study Guid
- Page 37 and 38: 10. One method holding great promis
- Page 39 and 40: Natural Hazards: Causes and Effects
- Page 41 and 42: Contents List of Figures List of Ta
- Page 43 and 44: Chapter 1 Introduction to Natural H
- Page 45 and 46: Type of Event Number of People Kill
- Page 47 and 48: Low-income Economy Afghanistan Bang
- Page 49 and 50: Phases of a Disaster Disaster speci
- Page 51 and 52: Effects of Disasters Each type of d
- Page 53: take steps to prevent the disaster,
- Page 57 and 58: Himalayan zone. Most earthquakes ap
- Page 59 and 60: The different rates of travel betwe
- Page 61 and 62: Modified Mercalli Intensity Scale o
- Page 63 and 64: Frequency of Earthquakes More than
- Page 65 and 66: How an earthquake damages a house F
- Page 67 and 68: Rupture Zones and Epicenters in Cen
- Page 69 and 70: of population from rural to urban a
- Page 71 and 72: In all emergency activities it is o
- Page 73 and 74: Notes 1 Rita Funaro-Curtis, Natural
- Page 75 and 76: foundations by the water buoyancy.
- Page 77 and 78: Impact on Natural and Built Environ
- Page 79 and 80: Disaster Mitigation The most system
- Page 81 and 82: - for tsunamis of local origin, pot
- Page 83 and 84: Chapter 4 Volcanoes Introduction Ov
- Page 85 and 86: production of sugar and cattle. Bec
- Page 87 and 88: lava is a thin fluid (not viscous),
- Page 89 and 90: then cool as thin, gently dipping s
- Page 91 and 92: drains, causing flooding during sub
- Page 93 and 94: then recognized, but today an incre
- Page 95 and 96: Volcanic Zoning and Risk Mapping Wi
- Page 97 and 98: 1. Environmental Effects Volcano Di
- Page 99 and 100: Altogether the combined disaster of
- Page 101 and 102: force caused by the earth’s rotat
- Page 103 and 104: An atmosphere disturbance forces wa
The ultimate objective of this course, indeed the purpose of the <strong>Disaster</strong> <strong>Management</strong> <strong>Center</strong> at<br />
the University of Wisconsin, is to contribute to those objectives stated by Krimgold. An<br />
underst<strong>and</strong>ing of the nature of natural hazards is the first step in preparing for them. Being able<br />
to anticipate their consequences is a prerequisite not only to appropriate action following<br />
disaster events but also to prevention of them. The following lessons seek to provide an<br />
introduction to that process.<br />
Notes<br />
1 Frederick C. Cuny, <strong>Disaster</strong>s <strong>and</strong> Development, Oxford University Press, New York, 1983, p. 3.<br />
2 Earthscan, <strong>Natural</strong> <strong>Disaster</strong>s: Earthscan Press Briefing Document No. 39, International Institute for Environment <strong>and</strong><br />
Development, London, 1984, p. 16.<br />
3 Cuny, <strong>Disaster</strong>s <strong>and</strong> Development. p. 14.<br />
4 Earthscan, <strong>Natural</strong> <strong>Disaster</strong>s, 1984.<br />
5 Cuny, <strong>Disaster</strong>s <strong>and</strong> Development. p. 39.<br />
6 Ibid. p. 40.<br />
7 Ibid. pp. 40-41.<br />
8 see also J. Eugene Haas, Robert W. Kates, Martyn J. Bowden, Reconstruction Following <strong>Disaster</strong>s, MIT Press, Cambridge,<br />
Massachusetts, 1977.<br />
9 see also J. Eugene Haas, Robert W. Kates, Martyn J. Bowden, Reconstruction Following <strong>Disaster</strong>s, MIT Press, Cambridge,<br />
Massachusetts, 1977.<br />
10 Pan American Health Organization, A Guide to Emergency Health <strong>Management</strong> after <strong>Natural</strong> <strong>Disaster</strong>, Pan American Health<br />
Organization, Washington, D.C., 1981, pp. 3-4.<br />
11 Cuny, <strong>Disaster</strong>s <strong>and</strong> Development pp. 49-50.<br />
12 Ibid pp. 44-56.<br />
13 Frederick Krimgold, The Role of International Aid for Pre-disaster Planning in Developing Countries, audelringen for<br />
Arkitektur, KTH Stockholm, 1974, p. 65.