karst aquifers

Karst aquifers are underground water systems formed in limestone and other soluble rocks. Over time, rainwater, slightly acidic from carbon dioxide, dissolves the rock, creating features like caves, sinkholes, and underground rivers. This process leads to unique landscapes and influences how groundwater flows. Karst aquifers are crucial for providing fresh water, but they can be vulnerable to pollution since the water moves quickly through these systems. Understanding karst aquifers is essential for water resource management and environmental protection, especially in areas where they serve as a primary water supply.