The term karst describes a distinctive topography where the dissolution (or chemical solution) of underlying soluble rocks by ground water has occurred. Although commonly associated with carbonate rocks like limestone and dolomite, other highly soluble rocks such as can be sculpted into karst terrain. About 15% of the surface of the United States (and 10% of the earth’s land) consists of soluble limestone, which can be easily dissolved by the weak solution of carbonic acid found in underground water.
As rain falls through the atmosphere, it picks up carbon dioxide and forms carbonic acid. Carbonic acid seeps into the bedrock and creates slow-moving groundwater. The combination of carbonic acid and groundwater erodes the landscape and creates karst topography. The underground water of karst topography carves impressive channels and caves that are susceptible to collapse from the surface. When enough limestone is eroded from underground, a sinkhole may develop. This geological process of erosion can take thousands of years to form karst topography.
Sinkholes can range in size from a few feet to over 300 feet deep. They’ve been known to “swallow” cars, homes, businesses, and other structures. Sinkholes are especially common in Florida where they’re often caused by the loss of groundwater from things such as pumping.
Karst topography is also responsible for some of the most stunning sites on Earth: karst caves. Inside karst caves, it is easy to find a wide range of structures created by the deposition of slowly dripping calcium carbonate solutions. Dripstones provide the point where slowly dripping water turns into stalactites. Those are structures which hang from the ceilings of cave. Over thousands of years, the slowly dripping water will form stalagmites. Those are structures which rise up from the floors of caves. Tourists from all over the world flock to caverns to view beautiful displays of stalactites and stalagmites. In fact, the world’s longest cave system – the 350 mile long Mammoth Cave system of Kentucky – was formed by karst topography.