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Centimetre-scale reverse faults cross-cutting alternating dolomites and silica layers of the Plattenkalk nappe. Faults (photo) and asymmetric south-verging folds reflect Oligocene compression and are exposed in the Samaria Gorge, which developed as a result of contemporaneous (Pleistocene) continent uplift and erosion.

Approximate location of the outcrop

Centimetre-scale reverse faults cross-cutting alternating dolomites and silica layers of the Plattenkalk nappe. Faults (photo) and asymmetric south-verging folds reflect Oligocene compression and are exposed in the Samaria Gorge, which developed as a result of contemporaneous (Pleistocene) continent uplift and erosion.

Approximate location of the outcrop

Photograph: Koen Van Noten

Reference: Fassoulas C. (2004). Field Guide to the Geology of Crete. Natural History Museum of Crete, Publ., 104p, Heraklio (3th edition)