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  1. Convergent plate boundaries: Where two tectonic plates collide, one plate is forced beneath the other, creating intense heat and pressure that leads to volcanic activity.
  2. Divergent plate boundaries: Where two tectonic plates move apart, magma rises to fill the gap, creating new volcanic activity along the boundary.
  3. Hot spots: Areas where magma plumes rise from deep within the mantle, creating isolated volcanic activity away from tectonic plate boundaries, such as the Hawaiian Islands.
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