Some information on EARTH QUAKE
Method of information
1. Introduction
2. Causes - List ---->> Point wise
3. Case Study
4. Mitigation
5. Conclusion
6. Source [ from where u collected the information ]
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- Earthquake is the sudden and violent shaking of the ground caused by the release of energy in earth 's crust that generates seismic waves.
- Plate movement and volcanic activities are the major causes for release of energy. Collision between plates or subsidence caused by their movement away from each other generate waves of energy.
- Focus- It is the point of origin of earthquake where the energy is released.
- Epicentre- The point on the earth 's surface directly above the focus is known as the epicentre of the earthquake.
- The fastest of the three waves and the one that is first detected by seismographs is the P wave or primary wave. The P waves can move through both liquid and solid rock. P waves compress and expand matter as they move through it.
- S waves, or secondary waves, are the waves directly following the P waves. S waves cannot travel through liquid.. S waves are larger than P waves and are more dangerous they and generate vertical and horizontal motion in the ground surface.
- Surface waves move close to or on the outside surface of the ground. This the slowest of all the earthquake waves.
- The earthquake with the largest recorded magnitude of 9.5 occurred at Valdivia in Chile on May 22nd 1960. Its epicenter was near Lumaco.
- engineers have constructed skyscrapers that float on systems of ball bearings, springs and padded cylinders. Acting like shock absorbers in a car, these systems allow the building to be decoupled from the shaking of the ground.
- Another technique to dampen the swaying of a tall building is to build in a large (several tons) mass that can sway at the top of the building in opposition to the building sway. Known as “tuned mass dampers”, these devices can reduce the sway of a building up to 30 to 40 percent.