South Carolina has many springs which serve as important indicators of groundwater health and hold historical significance to its citizens.
Overview 
Springs naturally flow to the surface and can have a pipe added to them to access the water more easily. Springs of most interest are those that flow out of rock or the ground in amounts that are useful or noticeable. H. Lee Mitchell of the SCDNR located and researched 458 springs across South Carolina during the 1990s and 2000s, with particular interest in the history of springs. This work was the first and most expansive study of South Carolina's springs and served as the basis for another study undertaken from Fall 2025 to Summer 2026, which focused on spring water quality for a subset of Mitchell's original sites.
Springs come in four main types:
Depression springs
Contact springs
Fault springs
Sinkhole (or solution) springs
A handout with figures of the four spring types with additional information can be downloaded here.
The type of sediment in an area affects the type of spring that one would find. For example, depression springs are found where there is a depression in the permeable land surface that intersects the water table, then a spring forms. A contact spring forms where water from an aquifer meets an impermeable layer, such as clay, and flows out at the surface. Fault springs, which can be hot or cold in temperature, occur when water flows from the aquifer through a fracture to the land surface. If the aquifer has an underlying magma chamber, the water will heat up and any flowing water at the surface could form a hot spring. Lastly, sinkhole (or solution) springs occur when water that naturally moves through the ground dissolves minerals (for example limestone) and forms solution cavities. If the land surface collapses above a solution cavity, this forms a sinkhole and where the water meets the surface, a spring is formed (Mitchell 2004).
Reports
2025-2026 South Carolina Springs Assessment, Modzelesky, et. al. 2026
Springs of South Carolina, Mitchell. 2004





































