buildings included 29‚500 structures in Miyagi Prefecture‚ 12‚500 in Iwate Prefecture and 2‚400 in Fukushima Prefecture. Three hundred hospitals with 20 beds or more in Tōhoku were damaged by the disaster‚ with 11 being completely destroyed. The earthquake and tsunami created an estimated 24-25 million tons of rubble and debris in Japan. An estimated 230‚000 automobiles and trucks were damaged or destroyed in the disaster. As of the end of May 2011‚ residents of Iwate‚ Miyagi‚ and Fukushima prefectures
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Earthquakes in Japan The Japan is located in an area where several continental and oceanic plates meet and create a major fault line; this is the cause of frequent earthquakes and the presence of many volcanoes and hot springs across Japan. If earthquakes occur below or close to the ocean‚ they may trigger tidal waves known as tsunami. Historic earthquakes Here is a brief history of earthquake in Japan. Many parts of this country have experienced devastating earthquakes and tidal waves in the
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JUSTUS-LIEBIGUNIVERSITÄT GIESSEN Andreas Bausch / Barbara E. Weißenberger / Marcus Blome Is market value-based residual income a superior performance measure compared to book value-based residual income? Working Paper 1 / 2003 – Arbeitspapiere Industrielles Management und Controlling – Herausgeber: Professur für Betriebswirtschaftslehre mit dem Schwerpunkt Industrielles Management und Controlling (Prof. Dr. Barbara E. Weißenberger) Justus-Liebig-Universität‚ Gießen http://wiwi
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Earthquakes in GCC An Earthquake known also as tremor is resulted from a sudden release of energy ‚which takes place in the earths crust‚ which then creates seismic waves. They are vibrations triggered by movement of rocks that have been strained (deformed) beyond their elastic limit. This activity called seismicity or seismism of an area refers to type ‚ size and frequency over a time period. Earthquakes are measured using many instruments ( up to atleast 20 different types
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Chile Earthquake Script Earthquake On February 27th 2010 at 3:34 an earthquake with a magnitude of 8.8 occurred in Chile. The earthquake lasted 90 seconds and affected a total of 6 Chilean regions but the earthquake mainly occurred offshore of Maule region. The earthquake left 93% of Chile’s population with no electricity. This earthquake not only damaged Chile but it has permanently shortened the length of our days by 1.26 microseconds and moved the earth’s axis by 8 centimetres. Tsunami
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Alaska earthquake http://www.iris.edu/hq/files/programs/education_and_outreach/aotm/31/Alaska1964EarthquakeCauses.mp4 A lot of excellent information is packed into this short video. 1. How many minutes did the shaking last? The shaking lasted 4.5 minutes. 2. What was the magnitude of the earthquake? The magnitude of the earthquake was 9.2. 3. This earthquake occurred just as geologists were figuring out plate tectonics. What principle of plate tectonics did the earthquake confirm
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FINANCIAL REPORTING RESEARCH REPORT MMPA 516 SUBMITTED BY Name: Rajat Chawla Student ID: 300256730 TABLE OF CONTENTS Executive Summary………………………………………………………………………….. i Table of Contents…………………………………………………………………………… ii Introduction Pros of SSP reporting Cons of SSP Reporting Conclusion Challenges communicated to Stakeholders What stakeholders are getting now? Stakeholders benefit from the changed reporting Recommendation
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San Francisco have all experienced a fault shift. In the case of Houston‚ the likelihood of an earthquake is extremely low. The instances of a fault shift on that area of the North American Plate don’t occur often. Earthquakes that occur are not by normal means of plates shifting but from the process of fluid extraction (Fehling 19). Seattle on the other hand has a very high probability of an earthquake occurring. There are three different types of quakes that the city experiences crustal quakes‚
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Gujarat earthquake The 2001 Gujarat earthquake occurred on January 26‚ 2001‚ at 03:17 UTC‚ and coincided with the 51st celebration of India’s Republic Day. The location of the epicentre was Bhuj (23.6° N 69.8° E) Gujarat‚ India. With a moment magnitude (Mw) of between 7.6 and 8.1‚ the quake killed more than 20‚000 people and injured another 167‚000 and destroyed near a million homes throughout Gujarat and parts of eastern Pakistan.[3] The earthquake is considered an intraplate earthquake because
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Prediction Why didn’t scientists know about the faults that caused the two earthquakes? Prior to September 4th‚ there were no surface signs of the Greendale Fault or the fault that generated the Lyttelton aftershock and there was no evidence for seismicity on these faults (i.e. ‘foreshocks’). Seismic surveys have located some ‘hidden’ faults across parts of the Canterbury Plains‚ but these particular regions had not been surveyed for this purpose. An oil-gas seismic survey had been carried out
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