The distribution of earthquake epicenters often aligns with the boundaries of tectonic plates, where continents are located. These boundaries can be convergent, divergent, or transform, influencing the shape and location of landmasses. As tectonic plates interact, they can cause earthquakes, which tend to occur along the edges of continents rather than in their interiors. Consequently, the pattern of earthquakes reflects the geological processes that shape the continents over time.
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