The origin of the man at the Earth is directly associated with the determination of directions of the flow distribution of the ancient man migration to adjacent territories. In such studies traditionally mainly landscape and climatological changes are considered. We suggest that along with the above factors, regional tectonic-geodynamic factors played a dominant role in the character of migration. The considered African-Levantine-Caucasian region is one of the most complex regions of the world, where collisional and spreading processes of geodynamics converge. First is determined an essential influence of the Akchagylian hydrospheric maximum (about 200 m above the mean sea level) limiting the ancient men migration from Africa to Eurasia. We propose that the Levantine Corridor emerged after the end of the Akchagylian transgression and landscape forming in the Eastern Mediterranean. This corridor location was formed by the movements between the Dead Sea Transform and the boundary of the carbonate platform of the Mesozoic Terrane Belt. Further landscape evolution was largely determined by the geodynamic behavior of the deep mantle rotating structure occurring below the central part of the region under study. All the mentioned events around and in the Levantine Corridor have been studied in detail on the basis of the combined geodynamic, paleogeographic, and paleomagnetic analyzes performed in northern Israel (Carmel uplift and Galilee plateau). Careful studies of the Evron quarry geological section indicate that it is a unique one for the dating of the marine and continental archaeological sequences and sheds light on the movement of the ancient man along the Levantine Corridor.