karst processes

Karst processes refer to the natural formation of landscapes shaped by the dissolution of soluble rocks like limestone, gypsum, and dolomite. When rainwater, which is slightly acidic, seeps into the ground, it chemically reacts with these rocks, gradually dissolving them. Over time, this creates distinctive features such as caves, sinkholes, underground rivers, and rugged surface terrain. These processes occur slowly but continually, transforming the landscape and creating unique geological formations. Karst regions are important for their unique ecosystems, water resources, and geological interest.