Thursday, June 20, 2019
A hypothetical disaster scenario Essay Example | Topics and Well Written Essays - 1000 words
A hypothetical disaster scenario - Essay ExampleHowever, there is no passing 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 compeer to the development of fingernails. They are ought to be moving away from individually 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 consequently 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 go on 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 humble and authorize 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, big 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 terrif ying thus they occur infrequently in that the locals
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