+The Supercontinent Cycle describes the Earth's continents periodically converging to form a single [Supercontinent](/wiki/supercontinent), then breaking apart. This grand dance, driven by [Plate Tectonics](/wiki/plate_tectonics) and deep mantle currents, profoundly shapes our planet's climate and geology over hundreds of millions of years.
+## See also
+- [Pangaea](/wiki/pangaea)
+- [Rodinia](/wiki/rodinia)
+- [Continental Drift](/wiki/continental_drift)
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