vízkáraktól
Vízikarakto is a Hungarian term that translates to "water karst" in English. It refers to karst landforms that have developed and are actively influenced by water, particularly in areas where the bedrock is soluble, such as limestone or dolomite. Unlike dry karst, which is shaped primarily by dissolution in the vadose zone (the unsaturated zone above the water table), vizikaraft involves the interaction of groundwater with the rock.
This process leads to the formation of various underground features like caves, conduits, and large dissolution
The study of vizikaraft is important for understanding groundwater resources, hydrogeology, and the stability of underground