The Baltic Sea area, as defined by its catchment and body of water, because of its recent geological development and its presently occuring changes is both an evolving and a responding conservative cellular, complementary geosystem.
Geological, geomorphological, archaeological and historical records allow a reconstruction of the hydrological development of Lake Müritz (Mecklenburg-Vorpommern, Northeast-Germany) in the Late Quaternary. After a very high lake-level