Karst Aquifer

A karst aquifer is a type of underground water reservoir formed in soluble rocks like limestone or gypsum. Over time, water dissolves these rocks, creating a network of caves, cracks, and sinkholes. This process results in highly permeable pathways that store and transmit large amounts of freshwater. Karst aquifers are important sources of drinking water and support ecosystems, but their complex structure can make water quality and flow unpredictable. These aquifers are often characterized by rapid flow channels and underground channels that replenish surface water sources.