Karst topography forms primarily through the dissolution of soluble bedrock, such as limestone, gypsum, or salt, by natural acidic water, often from rain or groundwater. This process requires a combination of geological conditions, including the presence of these soluble rocks, adequate rainfall, and a landscape that facilitates water movement. Over time, the dissolution creates distinctive features like sinkholes, caves, and underground rivers. Additionally, vegetation can play a role by enhancing the acidity of the water through organic decay.
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