File:Katavothra-Feneos ponor karst-depression Peloponnese Feneos mit katavothre.jpg

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Ελληνικά: καταβόθρα, καρστικο φαινομένων στη λεκάνη / οροπέδιο Φενεού, Πελοπόννησος, Ελλάδα. Καθε 4-5 χρονια, οταν οι μεγαλες ποσοτητες νερού συσσωρευτηκαν η μπλοκαριστηκαν, υπηρχε κατακρατηση νερού. Οταν η ποσοτητα του νερού, ηταν πολυ μεγαλη, διμιουργηθηκαν λιμνες.

English: One of 3 Ponors in the southern part of the polje Feneos, Corinthia, Peloponnese.

When precipitation of winters is exceptionally rich, parts of the polje become flooded even nowadays; until the second half of the 19th century there was even an almost permanent lake. Marks of the watertable at the bottom of the slopes are still visible. Construction of a system of draining ditches reduced floods.

By hydrogeological tracertests in 1984 subsurface drainage through the surrounding limestone mountains emerged in a karst spring of river Ladonas, 15 km south east.
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