Karst topography

- Karst topography, is a distinctive landscape characterized by unique landforms and geological features.
- Karst landscapes develop in areas with soluble bedrock, primarily limestone, dolomite, or gypsum, and are shaped by the dissolution of these rocks by natural processes
Solution
- Solution is a dominant geological process in the development of landforms in karst regions.
- Solution processes involve the chemical dissolution of soluble rocks, such as limestone, dolomite, or gypsum, by acidic groundwater.
- Over time, as water percolates through the rock, it gradually dissolves it, creating a variety of unique and distinctive landforms.
Here while both statements are true, they are not directly related or explaining each other.
The formation of stalactites and stalagmites is a specific result of solution processes in karst regions, but the reason is not providing a direct explanation for this particular formation.