Extensive landscapes formed by the dissolution of limestone and other carbonate rock and characterized by pitted, bumpy surface topography, poor surface drainage, and well developed solutions channels are known as

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Karst topography is characterized by the dissolution of limestone and other carbonate rock, resulting in unique features such as sinkholes, caves, and pitted surface topography. Poor surface drainage and well-developed solution channels are also common in karst landscapes. Plains, basins, and high tablelands are not specific to the dissolution of carbonate rock and do not typically exhibit the same surface features as karst topography.

Extensive Landscapes Formed by the Dissolution of Limestone and Other