+The Earth's structure refers to the planet's distinct internal layers, from the fragile outer [Crust](/wiki/crust) to the superheated inner [Core](/wiki/core). Between these lies the thick [Mantle](/wiki/mantle), where slow convection currents drive immense geological change. These layers, each with unique composition and properties, are fundamental to understanding Earth's dynamic processes.
+## See also
+- [Plate Tectonics](/wiki/plate_tectonics)
+- [Geology](/wiki/geology)
+- [Earth](/wiki/earth)
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