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.