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Freeze-thaw is the most common form of mechanical weathering that causes rocks to break into smaller pieces. Water enters cracks in rocks and freezes, expanding the cracks and breaking the rocks apart over time. Chemical weathering like carbonation occurs when acid rain forms from carbon dioxide in the air and water, dissolving rocks like limestone. This creates karst landscapes with features like grikes, clints, and caves formed by underground rivers dissolving the limestone further with carbonic acid in a

Author

Don Musoga

Language

EN