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The Pindos foreland basin is an example of Tertiary turbidite basin fill, segmented during its evolution by propagating thrusts. The distribution of turbidite facies in the Pindos foreland and the palaeocurrent directions of submarine fan development show that the northe part of the Pindos foredeep, from the middle Eocene to the late Oligocene, was an example of underfilled foreland basin. Adjacent to the Pindos thrust front (inteal Ionian zone), during that period, in the northe part of the thrust, a valley was formed in which sediments concentrated from both the thrust .front and the peripheral bulge.