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A hypothetical disaster scenario - Essay Example

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It was on Tuesday April 1st at 4:45 when an earthquake of about 8.2 magnitude hit the coast of Chile. The effect of this earthquake was felt when the ground shook at a distance of…
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A hypothetical disaster scenario
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However, there is no difference between this earthquake and the California earthquake. Data needs to be collected on the extension of the effects of the earthquake. The earthquake might have triggered other earthquakes or even tsunamis. Facts deploy that the crustal plates that compose the surface of the planet are seen moving all the time. They are identified moving at a rate that is equal to the development of fingernails. They are ought to be moving away from each other. This then leads to the oozing of the magma up which forms a new crust.

Therefore, they may slide past each other or even towards each other which makes the current crust to be destructed. The main thing that may make them stick together thus forcing a deformation when they continue their movement is through friction. The faults are subjected to breakage where seismic waves are when friction is by deformation. However, the divergent boundaries may occur at the mid-ocean ridges or even in the rift zones. This is where the new crust if formed. These regions are subjected to earthquakes of which they are not that hazardous in the part because they appear to be small and happen to be far away from people.

During the time when the plates are moving apart, the transform boundaries are the motion of strike slip of the San Andreas Fault. The earthquakes happening in these regions happen to be shallow and thus they produce moderate magnitude earthquakes. The convergent boundaries occur when there is a collision of the plates. If the plates are both continental plates, huge mountain ranges created by the crust that crumbles out in the process of formation just like the Himalayas. If the movement happens to be in between the continent and the ocean, the oceanic plate which is of high density, is sub ducted in the floating continental plate which happens to be of low density.

The regions where subduction takes place are always terrifying thus they occur infrequently in that the locals

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