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1981, Petar T. Milanović, Karst hydrogeology, page 168:
As long as the total capacity q of the spring is smaller than the total capacity q2 of the ponor, no flooding of the polje will occur.
2004, John Gunn, Encyclopedia of Caves and Karst Science, page 1283:
The only permanent sea ponor in the world is the sea mill of Argostoli, located on Kefalonia Island in the Ionian Sea (Greece) (Glanz, 1965).
2004, Petar Milanovic, Water Resources Engineering in Karst, page 22:
Ponors are one of the symbol features of karst regions, and crucial features from a hydrogeological and geotechnical point of view.
2018, Márton Veress, Glaciokarsts, page 203:
The characteristic features of the ponors of glaciokarst mainly manifest in the fact that they were mostly formed in karstic depressions or in glacial erosional depressions.