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  • Studies in the periglacial environment: a review of geomorphodynamic, cryopedological and Quaternary research in Germany
  • Geomorphodynamics, sea-level applied to coastal management of the lagoon.
  • energy of surface runoff. Occasionally wind may contribute additional energy but even then it is mainly propagated through the water. This contribution to microgeomorphology and to geomorphodynamics sheds new light on the genesis of sliding tracks
  • The fluvial geomorphodynamic of the Danube during the late Pleistocene and Holocene is rather thought to be the result of a self-control mechanism independent from the climatic rhythm. Changes of either internal and/or external factors therefore
  • necessarily affect valley floors different in river morphology and parts of the fluvial systems of different sensitivity which produce different geomorphodynamic reactions.