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Limestone generally weathers and erodes at a moderate pace, influenced by factors such as the presence of water, acidity, and environmental conditions. Carbonic acid, formed when rainwater mixes with carbon dioxide, can accelerate the chemical weathering of limestone. While it may not erode as quickly as softer rocks, its dissolution can lead to significant geological features over time, like karst landscapes. Thus, while the process can be gradual, it can still lead to notable changes over thousands to millions of years.

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6d ago

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