Karst Topography is a concoction response about the disintegration of layer.
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.
Karst Topography is a chemical reaction about the dissolution of layer(s) of soluble bedrock, clearly, carbonate rock like limestone or dolomite. Acidic water erodes the calcium in the bedrock, which is a main constituent of carbonate rocks in creating caverns. First tiny fractures/tunnels form in the rock and yet, with adequate time and dissolution, this acidic erosion can make huge caverns.
