Why could volcanic landscapes be useful sites for storing captured carbon dioxide?

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Volcanic landscapes are considered potentially useful sites for storing captured carbon dioxide primarily because of their abundance of basalt rock formations.1

When carbon dioxide is captured—such as through direct air capture methods—it can be processed into weak acids. These acids react readily with basalt, a common volcanic rock, to mineralize the carbon dioxide into stable carbonate rocks within a few years. This process effectively locks the carbon into a solid, permanent form, reducing the risk of leakage that can be associated with other types of underground storage.1

By utilizing these geological formations, scientists aim to provide a safe and long-term solution for sequestering carbon dioxide that has been removed from the atmosphere.1