Plate divergence is a tectonic phenomenon in which lithospheric plates move apart along divergent plate boundaries, driven primarily by mantle convection, slab pull, and ridge push forces. This separation promotes decompression melting of the underlying asthenosphere, generating mafic magmas that ascend to form new oceanic crust at mid-ocean ridges or intraplate rift systems on continents. The process is characterized by extensional stress fields, normal faulting, and symmetric seafloor spreading, often accompanied by linear volcanic and seismic activity. Plate divergence plays a central role in lithosphere recycling, global heat loss, and the long-term evolution of ocean basins and continental configurations.
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