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.
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