Chemical weathering is a natural process that involves the breakdown and alteration of rocks and minerals due to chemical reactions. This type of weathering occurs when rainwater, which is slightly acidic due to dissolved carbon dioxide, interacts with minerals in rocks, leading to chemical changes. For example, it can cause limestone to dissolve. Factors such as temperature, moisture, and vegetation can affect the rate of chemical weathering. This process is crucial in shaping landscapes and contributes to soil formation, playing an important role in the rock cycle.
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