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Palaeogeographic maps of the lacustrine Miocene and Pliocene have been   constructed according to all the known geological data. The Lakes of the   Balkan Land, depending on the tectonics, migrated due to causes from the deep   subsurface. There are several phases of the Miocene lakes: the lowermost   Miocene transiting from marine Oligocene, Lower, Middle, Upper Miocene   covering, in patches, the main part of the Land. The Pliocene lakes spread   mostly to the north of the Balkan Land and covered only its marginal parts.   Other lake-like sediments, in fact freshened parts of the Black Sea   Kuialnician (Upper Pliocene), stretched along the middle and southern   portions of the Balkan Peninsula (to the south of the Balkan Mt.).   Subsequently, the Balkan Peninsula was formed

The Neogene lakes on the Balkan land