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Zungenbecken
A Zungenbecken, also called a tongue basin〔Kohl, Horst; Marcinek, Joachim and Nitz, Bernhard (1986). ''Geography of the German Democratic Republic'', VEB Hermann Haack, Gotha, p. 40. ISBN 978-3-7301-0522-1.〕 or tongue-basin,〔Dickinson, Robert E (1964). ''Germany: A regional and economic geography'' (2nd ed.). London: Methuen, p. 32. .〕 is part of a succession of ice age geological landforms, known as a glacial series. It is a hollow that is left behind by the ice mass, as the snout of the glacier (German: ''Gletscherzunge'') recedes, which initially fills with meltwater, forming a proglacial lake, and later may be filled with surface water from streams or precipitation. When the glacier has more fully retreated this produces a finger lake or glacial piedmont lake (German: ''Zungenbeckensee'', known as a ''Gletscherendsee'' of the glacial series in the Alpine Foreland). The term ''Zungenbecken'' is of German origin, but used in English language sources.〔Somme, Axel (1968). ''A geography of Norden: Denmark, Finland, Iceland, Norway, Sweden'', Heinemann p. 213. 〕〔Pfeil (1995). ''Quaternary field trips in Central Europe'', International Union for Quaternary Research, XIV International Congress, August 3-19, 1995, Berlin, Germany, Volume 2.〕〔Charlesworth, J.K. (1966). ''The Quaternary Era: With Special Reference to its Glaciation'', in Two Volumes (Volumes 1-2)〕
Examples are the Tegernsee, Ammersee, Starnberger See, Lake Constance, Chiemsee, Tollensesee and the Baltic Sea.
== See also ==
* Glacier
* Drumlin
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