Chemical weathering quick check

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Chemical weathering refers to the breakdown of rocks and minerals through chemical reactions. This process occurs when minerals in rocks react with water, oxygen, or acids to form new compounds. Some examples of chemical weathering include the dissolution of limestone by acid rain, the oxidation of iron minerals in rocks, and the hydrolysis of feldspar minerals in granite. Chemical weathering is a slow but continuous process that can alter the physical and chemical properties of rocks over time.
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