Earthquakes often occur near volcanic regions due to the movement of tectonic plates and the dynamics of magma beneath the Earth's surface. As magma rises, it creates pressure and can cause the surrounding rocks to fracture, resulting in seismic activity. Additionally, tectonic activity associated with volcanic regions can lead to faulting and the release of stress accumulated in the Earth's crust, further increasing the likelihood of earthquakes. This interplay between volcanic activity and tectonic forces creates a seismically active environment.
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