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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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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EARTHQUAKES DHORI: Cracks on a salt marsh can be seen on this aerial view of the epicentre of the recent earthquake near Dhori village some 20 km. (12 miles) from Bhuj in the western Indian state of Gujarat‚ Saturday Feb. 3‚ 2001. (AP Photo/Enric Marti) AHMEDABAD: Residents of Ahmedabad‚ India‚ survey earthquake damage Saturday‚ Jan. 27‚ 2001. Officials predicted as many as 6‚000 may have been killed in the 7.9 magnitude earthquake in western India on Friday.(AP Photo/Saurabh Das) The 2001 Gujarat
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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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Gujarat’s Vulnerability to Earthquake 10. Case Study: Bhuj Earthquake 2 11. Drawbacks of the Bhuj earthquake 12. Gujarat State Disaster Management Authority (GSDMA) 13. Data Analysis 14. Conclusion 15. Bibliography ABSTRACT India has been traditionally vulnerable to natural disasters on account of its unique geo-climatic conditions. Floods‚ droughts‚ cyclones‚ earthquakes and landslides have been recurrent phenomena. About 60% of the landmass is prone to earthquakes of various intensities;
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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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faults lead to be a lot more destruction. Earthquakes are a trembling or shaking of the ground caused by a sudden release of energy stored in rocks beneath earths surface. Earthquakes appear all over the planet‚ and there are many different sizes. Some earthquakes destroy entire cities while others only shake the ground for a moment. Faults are one of the causes of earthquakes‚ which I will tell about soon as well as the hazards and benefits they give. Earthquakes can be caused in many ways‚ some even
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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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Definition: An earthquake is the result of a sudden release of energy in the Earth’s crust that creates seismic waves.TThe recent earthquake In India on September 18 ‚ 2011 compelled me to write an essay about earthquake. In this essay many things related to earthquake will be discussed.e seismicity or seismic activity of an area refers to the frequency‚ type and size of earthquakes experienced over a period of time. Measurement: Earthquakes are measured with the help of seismometers. The moment
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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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