+Seafloor spreading is the silent forge beneath the oceans, where new [oceanic crust](/wiki/oceanic_crust) is born. Magma rises from the depths, through [volcanic activity](/wiki/volcanic_activity) at rifts, pushing ancient seafloor aside in a slow, grand expansion. This continuous renewal is a vital part of [plate tectonics](/wiki/plate_tectonics).
+## See also
+- [Mid-ocean Ridge](/wiki/mid-ocean_ridge)
+- [Subduction](/wiki/subduction)
+- [Continental Drift](/wiki/continental_drift)
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