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Sagot :
Because the plates collide at different depths along their leading edges, earthquakes happen in subduction zones. One plate to some extent floats above the other as a result of this.
The two plates rub against one another in ways that are frequently earthquakes considerably more irregular than other fault lines are because there is material being rolled and spun around within the area of friction when pressure is released along the fault line. The resulting increased subduction zones trembling may cause some portions of the fault line to be pushed higher by the force of the fault collision.
The upward pushing also generates its own shock waves, which could earthquakes go in a different direction and increase the amount of damage. Because the plates collide at different depths along their leading edges, subduction zones earthquakes happen in subduction zones.
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