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48. Agia Fotia Unconformity

Just after Agia Fotia, on the northern cliffs overlooking the country road, there are angled unconformities between the Pleistocene aeolianite sandstone on the Pliocene marl.

49. Agia Fotia Stratigraphy

50. Rousso Spasma

At the Rousso Spasma position, just to the north of Katsounaki beach, stratigraphic unconformity of Pleistocene rocks is observed in the natural walls of the bay, both in the Tripolitsa limestone, as well as in the Pliocene marl.

51. Asprougas Marls