- A point where water exists from an underground drainage route or aquifer. An obvious output point is a surface resurgence or exsurgence, where drainage emerges from a conduit system. Less obvious are points where drainage leaves a carbonate aquifer and enters an adjacent non-carbonate bed, such as a sandstone aquifer .
A Lexicon of Cave and Karst Terminology with Special Reference to Environmental Karst Hydrology. Courtesy of the author & The Karst Waters Institute. 2002.
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