Explanation:
Karst topography is a type of topography that is formed by the dissolution of soluble rocks such as limestone or dolomite.
Karst landscapes are characterized by features such as caves, sinkholes, underground rivers, and rocky outcrops. These features are formed through the chemical weathering and erosion of soluble rocks over time.
The dissolution process often leads to the formation of underground drainage systems, which can further enhance the development of karst topography.
