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During physical weathering, rock structures break down into smaller pieces without altering their chemical composition, often due to temperature changes, freeze-thaw cycles, or abrasion. In chemical weathering, the minerals within the rock undergo chemical reactions, leading to alterations in their structure and composition, such as dissolution or oxidation. Metamorphism involves intense heat and pressure, transforming the existing rock into a new type with a different mineral structure and texture, often resulting in foliation or banding. Lastly, during sedimentation, weathered rock fragments are transported and deposited, eventually compacting and cementing into sedimentary rock.

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