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The Ranzano Sandstone Late Eocene to Oligocene) above and Montepiano marl (Lower Upper Eocene) below are part of Epiligurian Succession, a piggy back basin in the Nirthern Appeninies. It is located northward adjoining the coeval successions of the Tertiary Piedmont Basin of which the Epiligurian Succession would represent the less proximal facies. PhotoID812

The Ranzano Sandstone Late Eocene to Oligocene) above and Montepiano marl (Lower Upper Eocene) below are part of Epiligurian Succession, a piggy back basin in the Nirthern Appeninies. It is located northward adjoining the coeval successions of the Tertiary Piedmont Basin of which the Epiligurian Succession would represent the less proximal facies. PhotoID812

Photograph: Marco Mazzotta