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  • This study examines, in the eastern Harz Foreland, the initiation and evolution of forms caused by subsurface erosion using aerial photographs taken between 1964 and 1993. The subsurface erosion processes occur in a Pleistocene depression filled
  • The development of the Fischland-Darss-Zingst spit was reconstructed for different times after the beginning of the Litorina transgression. Especially the processes of an accelerated straightening of the coast is taken into account