Karst topography forms through the dissolution of soluble rocks like limestone, primarily driven by rainwater and carbon dioxide. Rainwater becomes acidic as it absorbs carbon dioxide, enabling it to erode these rocks over time. This process results in features such as sinkholes and caves in the landscape. ;
Karst topography forms through the dissolution of soluble rocks like limestone, driven mainly by acidic rainwater and carbon dioxide. Rainwater absorbs carbon dioxide, which enhances its ability to dissolve limestone, leading to features like caves and sinkholes over long periods. This geological process creates unique landscapes found in various parts of the world, showcasing the effects of water and carbon dioxide on rock formations.
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