Answer:
Earthquakes occur when there is a sudden release of energy in the Earth's crust or upper mantle, typically along fault lines. The majority of earthquakes occur along the boundaries of tectonic plates, where the plates are either moving away from each other (divergent boundaries), moving towards each other (convergent boundaries), or sliding past each other (transform boundaries).
In contrast, the centers of tectonic plates are characterized by relatively stable and uniform conditions. The rocks in these areas are not subjected to the same level of stress and strain as those at plate boundaries, as the plate is not being deformed or bent in any particular direction.
This lack of significant deformation and stress makes it less likely for an earthquake to occur at the centers of plates. However, it is important to note that earthquakes can still occur in these regions, although they are typically much less frequent and less intense than those occurring at plate boundaries.
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