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The forces inside the Earth, primarily driven by mantle convection, generate heat and pressure that lead to processes like magma formation and plate tectonics. At the surface, weathering, erosion, and sedimentation continuously alter the landscape and rock formations. Together, these internal and external forces create a dynamic rock cycle, where rocks are formed, broken down, and transformed over geological time. This cycle is essential for the recycling of materials and the evolution of the Earth's crust.

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