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An example of weathering in the rock cycle is the process of granite breaking down into smaller particles due to exposure to water and temperature changes. Over time, rainwater can seep into cracks in the granite, causing it to expand and contract, leading to the formation of smaller rock fragments. This mechanical weathering, coupled with chemical processes such as acid rain reacting with the minerals, contributes to the gradual breakdown of the rock. Ultimately, these weathered materials can then be transported and deposited, further contributing to the rock cycle.

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