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An angular unconformity between folded Jurassic chert and chertly limestone beds of the Pindos Nappe (below) and Pliocene coastal deposits (above); the unconformity level is about 4m above the present day sea level (Kythira Island). Photo ID 614

An angular unconformity between folded Jurassic chert and chertly limestone beds of the Pindos Nappe (below) and Pliocene coastal deposits (above); the unconformity level is about 4m above the present day sea level (Kythira Island). Photo ID 614

Photograph: Paris Xypolias

Reference: Xypolias, P., Koukouvelas, I., Zulauf, G. 2008. Cenozoic tectonic evolution of northeastern Apulia: insights from a key area in the Hellenides (Kythira, Greece). Zeitschrift der Deutschen Gesellschaft für Geowissenschaften, 159, 439-455.