Earthquakes Earths lithosphere is broken into a set of enormous jumpy fragments called plates. Interactions surrounded by these plate exit mainly on the edges, or coasts. There argon three different types of plate margins. These margins atomic number 18 determined by the types of interactions that advance between the plates. Divergent margins guide where 2 plates be moving aside from to separately one other, or diverging. This margin eject transcend in both Continental of oceanic crust. Convergent margins occurs where cardinal plates argon moving towards individually other. Different types of margins can occur here depending on the types of plates that argon interacting. A collision partition off occurs when two continents meet each other along a convergent margin. Here the plates pass on crumple upwardly and downwards as the lithosphere thickens, forming mountains. When the two plates meeting atomic number 18 both oceanic, one plate provide usually slopi ng trough underneath the other, usually resulting in volcanoes. The culture type of margin is a transform fault. This occurs where two plates are grinding their edges as they slide past each other. This causes the plates to fool very erose boundaries. An nationquake is the result of a fulminant release of capacity in the Earths crust that creates seismal waves. Earthquakes occur primarily along plate margins.

When two plates are attrition against each other, they irritate at the edges, but the rest of each plate is go along to move, so the fluctuate along the edges are distorted (strain). As this conti nues, pressure builds up to a layover where! the rock can no longer stand it, causation it to break. As the rock breaks, the energy radiates out as seismic waves and cause the earth to shake. The waves that are felt on the rebel of the Earth are Love waves and Rayleigh waves. Rayleigh waves, also known as anchor roll, trip like ocean waves along the come out of the cupboard of the Earth causing the footing surface to move up and down. Rayleigh waves cause most of the shaking that is felt at the ground during an earthquake....If you want to get a full essay, order it on our website:
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