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Karst terrain lacks surface streams and lakes due to disappearing streams flowing into sinkholes. Dissolved limestone forms distinctive features like sinkholes and caverns.
Karst terrain is characterized by disappearing streams where surface streams can enter sinkholes and flow underground, resulting in an absence of surface streams and lakes. The dissolved limestone creates features like sinkholes, caverns, disappearing streams, and towers. Living in karst regions presents challenges due to features like sinkholes that can appear rapidly.
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