A spring may be the result of
karst topography where surface water has infiltrated the
Earth's surface (recharge area), becoming part of the area
groundwater. The groundwater then travels through a network of cracks and fissure—openings ranging from intergranular spaces to large
caves. The water eventually emerges from below the surface, in the form of a
The forcing of the spring to the surface can be the result of a confined
aquifer in which the recharge area of the spring water table rests at a higher elevation than that of the outlet. Spring water forced to the surface by elevated sources are
artesian wells. This is possible even if the outlet is in the form of a 300-foot-deep (91 m) cave. In this case the cave is used like a hose by the higher elevated recharge area of groundwater to exit through the lower elevation opening.
Non-artesian springs may simply flow from a higher elevation through the earth to a lower elevation and exit in the form of a spring, using the ground like a drainage pipe.
Still other springs are the result of pressure from an underground source in the earth, in the form of
volcanic activity. The result can be water at elevated temperature such as a
The action of the groundwater continually dissolves permeable bedrock such as
dolomite, creating vast cave systems.
Seepage or filtration spring. The term seep refers to springs with small flow rates in which the source water has filtered through permeable earth.
- Fracture springs, discharge from faults, joints, or fissures in the earth, in which springs have followed a natural course of voids or weaknesses in the bedrock.
- Tubular springs, in which the water flows from underground caverns.