The breach
Phorkys, that lies between two points that break the line of the sea and shut the harbour in.
Around 40 m east of the in-situ beachrock ruin of the Plaka, we found a ridge made out of isolated beachrock fragments at 2.5-3.2 m water depth. The rubble ridge is up to 0.9 m thick..... .......The ridge structure is completely separated from the Plaka and its components lie on top of or are partly embedded in sandy deposits. Approaching the Plaka, numerous large beachrock blocks lie in extraordinarily disordered positions completely detached from the in-situ beachrock ruin at 2.9-4.6 m water depth.
The oldest dated tsunami which affected the Lagoon of Aghios Nikolaos and its shores occurred in the
3rd millennium BC.
3rd millennium BC.
Displacement and breach
Odussey Book 13 line 95-96 Samuel Butler