In geography, tectonic plates are classified into three main types based on their interactions and boundaries: divergent, convergent, and transform plates. Divergent plates move apart from each other, creating new crust as magma rises to the surface, as seen at mid-ocean ridges. Convergent plates collide, leading to subduction or mountain building, which can result in earthquakes and volcanic activity. Transform plates slide past one another horizontally, causing friction and earthquakes along faults like the San Andreas Fault.
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