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Variations in weathering on a local scale are influenced by several factors, including climate, rock type, topography, and soil moisture. For instance, areas with high rainfall and warmer temperatures typically experience more chemical weathering, while colder regions may see more physical weathering due to freeze-thaw cycles. Additionally, the mineral composition of rocks affects their susceptibility to weathering processes, and topographical factors can determine the drainage and exposure to elements. Local vegetation also plays a role, as roots can break down rocks and organic acids from decomposing material enhance chemical weathering.

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