The Earth resurfaces itself through a process known as the rock cycle, which involves the continuous transformation of rocks from one type to another. This cycle includes processes such as weathering and erosion, which break down rocks, and volcanic activity, which can create new landforms. Additionally, tectonic activity, including plate movements, can uplift, fold, or subduct rocks, further reshaping the Earth's surface. Over geological time, these processes contribute to the dynamic and ever-changing nature of the planet's crust.
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