Answer:
Karst Topography is a concoction response about the disintegration of layer.
Step-by-step explanation:
solvent bedrock, plainly, carbonate shake like limestone or dolomite. Acidic water dissolves the calcium in the bedrock, which is a primary constituent of carbonate shakes in making natural hollows. First modest breaks/burrows frame in the stone but then, with sufficient time and disintegration, this acidic disintegration can make gigantic caves.