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Final answer:
Groundwater and carbon dioxide interact to shape karst topography through dissolution and deposition processes.
Explanation:
Formation of Karst Topography by Water and Carbon Dioxide
Groundwater containing CO2 dissolves limestone deposits over time, forming caves through a process of dissolution and deposition. Water droplets forming stalactites and stalagmites illustrate this process. Karst topography results from chemical weathering of limestone by water, creating sinkholes and caves.
Learn more about Karst Topography here:
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