The two correct examples of chemical weathering are:
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Oxidation of certain metals in rock - This process involves a chemical reaction where oxygen reacts with minerals in the rock, altering their composition and weakening the rock structure.
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Acid rain breaking down compounds in rock statues - Acid rain contains acidic compounds that can chemically react with the minerals in rocks, leading to their breakdown.
Other options, such as physical processes (like temperature-induced cracking or rock slides) and biological processes (like insects digging), do not qualify as chemical weathering.