Figure 5.19 The mortar in unreinforced masonry walls such as these in Iran‚1990(A) can easily fail during an earthquake. Oftentimes the entire structure crumbles‚ leaving a pile of rubble in which survive. Shown in(B) is one of the many masonry homes to collapse during the 1988 Armenia earthquake (M6.9)‚ claiming nearly 25‚000 lives. The failure is called soft-story collapse. Soft-story collapse is a common problem in commercial building where the first floor has considerable open space for
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QUARTER EARTHQUAKE DRILL I. INTRODUCTION Having experienced the recent 7.2 magnitude earthquake some Boholanos are already nervous and uneasy every time there is news about the said calamity. Thus‚ they became very eager to undergo drills and listen to some orientations and preparations in responding calamities in order for them to be prepared for the future calamities. Public awareness is very much necessary to obtain and improve the people’s preparedness and mitigation. Thus this earthquake preparedness
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legend of the Earthquake Once upon a time‚ it was a dark and ominous day and trouble was arising in the underworld. Shiva the goddess of death and destruction had finally finished her mighty plans to take back what was rightfully hers. her plan was to swoop in from behind the city of peace ‚ and raid the museum of everything sweet and sour and steel the orb of tranquillity. Though to her surprise when she arose from the cavern of raw meat‚ Their awaited Johnny Mon Soony and Snoop Dogg. The most
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Relieving Chile and Haiti Many earthquakes strike different countries and very often‚ and they face efforts to rebuild the nation. Some countries do it better than others and some are more effective. But‚ this does not only apply to earthquakes but also to other natural disasters such as floods and droughts. In such situations‚ humanitarian and development aid rush in from different corners of the world and from the countries government. The aid that is received goes into the relief efforts of the
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2011) (Wdowinski‚ Tsukanov‚ Hong‚ & Amelung‚ 2010). Coincidentally‚ prior to the earthquake‚ Haiti experienced two tropical storms and a major hurricane in 2010; which may corroborate geologists’ assertion that increased soil erosion from these extreme weather events may have triggered the 2010 earthquake in Haiti (Ader‚ 2011) (Wdowinski‚ Tsukanov‚ Hong‚ & Amelung‚ 2010). Relative Risk & Vulnerability The 2010 earthquake disaster damaged over 30‚000 buildings including the parliament building‚ Presidential
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Earthquakes and Logarithms Earthquakes are responsible for a wast majority of natural hazards on our planet. This natural geological phenomena are almost impossible to predict‚ and they occur usually in zones of the planet that are prone to movement in the uppermost crust of the earth. Certain areas are more likely to experience earthquakes‚ and also the aftermath of the earthquakes can be just as destructive or sometimes even more. Different methods of measuring earthquakes have been implemented
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powerful earthquake in half a century. The 7.9 magnitude earthquake killed as many as 2‚000‚ injured at least 2‚000‚ and left 4‚000 missing. Most of the missing are thought to be buried under rubble‚ and rescue workers dug frantically with bulldozers‚ shovels‚ sticks -- even bare hands -- trying to find them. India’s Earthquake -- Residents in the Gujarat State of western India spent the night outside Friday‚ too fearful to go back into their damaged homes after India’s most powerful earthquake in half
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Northridge Earthquake Contents Chapter One Introduction Chapter Two Earthquake Chapter Three Aftermath Chapter Four Conclusion Introduction What makes the Northridge Earthquake so remarkable is that it is one of the few earthquakes that ever really erupted in a suburban area‚ the most money was put into repairs and reconstruction‚ it happened in a place such as America in an area with a huge population and the Earthquake affected many areas of American
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Effects of earthquakes Shaking and ground rupture Shaking and ground rupture are the main effects created by earthquakes‚ principally resulting in more or less severe damage to buildings and other rigid structures. The severity of the local effects depends on the complex combination of the earthquake magnitude‚ the distance from the epicenter‚ and the local geological and geomorphological conditions‚ which may amplify or reduce wave propagation.[44] The ground-shaking is measured by ground acceleration
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One of the strongest earthquakes in Mexico history struck the country’s southern coast. It happened later on a Thursday night. The earthquake destroyed hundreds of buildings. Panicked people ran into the streets in the middle of the night. About 90 people died. The earthquake hit minutes before midnight and caused buildings to sway violently in Mexico City. The capital of Mexico is more than 650 miles away from where the earthquake had struck. Beds were banging against walls. People still wearing
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