Ein neues Modell des würmzeitlichen Inn-Chiemseegletschers: Überschiebungen des Inngletschers über den Tiroler Achengletscher bis in die Bereiche des heutigen Chiemsees

Klaus Hormann
One problem of glacial geomorphology in Southern Bavaria is, whether the different glaciers spreading over the foreland of the Alpes advanced and retreated nearly simultanously or whether they acted more individually. The Inn-Chiemsee-glacier gives a fascinating example for individual behaviour. The limit between his two components, the Inn-glacier and the Chiemsee-glacier, was difficult to be determined, as in some areas terminal moraine structures belonging to both glaciers can be observed (crossing each other). The best...