- Any underground lake. The water can be in a partially drained phreatic cave, and may then be the entrance to a sump, or it can be open over its entire surface. In vadose caves lakes are most commonly formed by ponding behind banks of sediment or, in rarer cases, behind very large gour barriers .
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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