- 1. Subsurface conduit water that has been driven back up into older, higher karst levels and into the surrounding rock matrix during a high flow period.2. River water that has infiltrated river banks during a high flow period and being retained in temporary storage .
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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