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The Karst Landforms and Cycle of Erosion

Karst landforms are shaped by the dissolution of soluble rocks like limestone, gypsum, and dolomite. Common features include sinkholes, caves, and underground rivers. The karst cycle of erosion begins with water seeping into cracks, dissolving the rock, and expanding cavities over time. This process creates distinctive landscapes with collapsed surfaces and intricate cave systems. The cycle evolves from early surface erosion to mature underground drainage networks, and eventually, land collapse or landscape leveling.