Karst topography is a type of landscape formed from the dissolution of soluble rocks, such as limestone, gypsum, or salt. This process creates unique features like sinkholes, caves, and underground rivers. The water, often slightly acidic, erodes the rock over time, leading to the characteristic rugged terrain. In areas with karst topography, the surface can appear uneven and pockmarked due to the presence of these features. This landscape is important for groundwater systems, as it can influence water flow and storage. Additionally, karst regions often support diverse ecosystems and unique geological formations.