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When it rains in the Yucatán Peninsula, the limestone bedrock undergoes chemical weathering due to the reaction of rainwater, which is slightly acidic, with the calcium carbonate in the limestone. This process leads to the dissolution of the rock, creating features such as sinkholes and underground rivers. Over time, this can significantly alter the landscape, contributing to the region's unique geological formations and karst topography. Additionally, the water can erode and transport limestone particles, further shaping the environment.
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