GUJARAT EARTHQUAKE MORE DESTRUCTIVE THAN THE SAN FRANCISCO EARTHQUAKE? In 1989 an earthquake hit San Francisco‚ on the west coast of USA‚ killing around 63 people. Twelve years later an earthquake hit Gujarat‚ in India. This time it killed approximately 20‚000 people. In this report I will be comparing the two earthquakes‚ giving reasons why the Gujarat earthquake was so much more destructive than the one in San Francisco. An earthquake is a movement or tremor in the earth’s crust. Earthquakes happen
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12 7.0 Conclusion 13 8.0 Reference 14 The effect of earthquake on buildings in Japan 1.0 Abstract The country of Japan is an island. The population in Japan is considered quite high‚ about 127‚817‚277 people in this small country. Therefore‚ this has made Japan became one of the most tightly populated country in the world‚ ranking the 36th placing. Earthquakes are very common in Japan. In fact‚ Japan had suffered more earthquakes compared to other. Therefore‚ engineers have put in a lot of
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EARTHQUAKE ENGINEERING IN AUSTRALIA BEFORE MECKERING AND AFTER NEWCASTLE by Charles Bubb BE‚ DIC (Eng. Seis.)‚ FIEAust‚ CPEng SUMMARY Earthquake Engineering in Australia‚ as elsewhere‚ has been formulated in the aftermath of damaging earthquakes. The first Australian Code AS2121-1979 was written and published after the 1968 Meckering WA earthquake. The second AS1170.4 1993 was published after the 1989 Newcastle NSW earthquake. Good quality Building Codes are a necessary basis for sound earthquake
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Investigations of past and recent earthquake damage have illustrated that the building structures are vulnerable to severe damage and/or collapse during moderate to strong ground motion. Among the possible structural damages‚ seismic induced pounding has been commonly observed in several earthquakes. A parametric study on buildings pounding response as well as proper seismic hazard mitigation practice for adjacent buildings is carried out. Three categories of recorded earthquake excitation are used for input
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Loma Prieta Earthquake Story Teller By: Kavita Butani There is a lot that happens around the world we cannot control. We cannot stop earthquakes‚ we cannot prevent droughts‚ and we cannot prevent conflict. Earthquakes and the damages they bring have affected the lives of many people around the world forever. As our community grows so does the danger caused by these quakes also increases by mass. Earthquakes can affect our lives in many ways; this type of natural disaster can upset everything from
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1)Abstract 2)Introduction 3)Causes of earthquakes 4)Basic terminology: a)Hypocentre‚ b)Epicentre c)Focal depth 5)Earthquake size a)Magnitude b)Intensity 6) Earthquake hazard a)Primary effects b)Secondary effects 7)Earthquake loads on buildings 8)How Buildings Respond to Earthquakes 9)Common Modes of Failure a)Structural
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EARTHQUAKE An earthquake (also known as a tremor‚ temblor or seismic activity) is the result of a sudden release of energy in the earth’s crust that creates SEISMIC WAVES. Earthquakes are measured with a seismometer; a device which also records is known as a seismograph. SEISMIC DEFORMATION When an earthquake fault ruptures‚ it causes two types of deformation: static; and dynamic. Static deformation is the permanent displacement of the ground due to the event. The earthquake cycle progresses
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deadliest earthquake in history killed 840‚000 people‚ But many other earthquake have caused the dead of more than 100‚000 people and isn’t unusual‚ even in modern times‚ for an earthquake death toll to reach 20‚000 to 20‚000 people with hundreds of thousands left homeless. There are four factors that affect the casualty rate and economic impact of earthquake: magnitude‚ location‚ quality of construction of building‚ and timing. Magnitude The magnitude‚ or strength‚ of an earthquake is measured
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2010 Haiti Earthquake - Case Study Location A 7.0 magnitude earthquake strikes Haiti on Tuesday‚ 12th of January 2010 at 16.53 local time (21.53 GMT). The earthquake occurred in Port-au-Prince‚ the capital city of Haiti. The focus of the earthquake was 13 km below the surface of the earth. Causes The earthquake was caused by the North American Plate sliding past the Caribbean Plate at a conservative plate margin. Both plates moved in the same direction‚ but on plate moves
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Impact Approximately 57 deaths‚ about $1.1 billion in property damage; caused a partial collapse of the volcano’s flank‚ deposited ash in eleven states and five Canadian provinces. With no immediate precursors‚ a magnitude 5.1 earthquake occurred and was accompanied by a rapid series of events. Mount St. Helens produces small to large explosive eruptions‚ which send varying quantities of ash and tephra into the atmosphere Tephra (rock fragments and particles ejected by a volcanic eruption
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