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A resurgent spring refers to a type of spring that forms when groundwater flows to the surface due to pressure, often emerging from a hillside or cliff. This phenomenon typically occurs in karst landscapes, where soluble rock like limestone has been eroded to create underground channels. The term can also imply a seasonal revival of flora and fauna as ecosystems rejuvenate during springtime. Overall, resurgent springs are significant hydrological features that contribute to local water supplies and biodiversity.

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Resurgent Stream arise when the limestone is underlain by an impermeable rock, such as clay. this forces the water out into the open, forming a spring or resurgent stream.


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Resurgent Stream arise when the limestone is underlain by an impermeable rock, such as clay. this forces the water out into the open, forming a spring or resurgent stream.


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Why is a resurgent stream only formed in a limestone area?

A resurgent stream is formed when an underground river is forced to reappear when it reaches a layer of impermeable bedrock. For a river to become an underground river in the first place it must flow over an area of limestone rock. The mildly acidified river water (it is acidified by dissolved carbon dioxide which is present in rainwater) reacts with the limestone (which is 80% calcium carbonate) and dissolves it. This forms a swallow hole into which the river flows. The river then continues to chemically weather the limestone underground thus forming an underground river. The river is forced to reappear (in the form of a resurgent stream) on the surface when there is a change of rock type from permeable limestone to impermeable bedrock. Hence resurgent streams are typically only found in limestone areas.


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