HOME

TheInfoList



OR:

A ''Zungenbecken'', also called a tongue basin or tongue-basin, is part of a succession of
ice age An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and gre ...
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 Meltwater is water released by the melting of snow or ice, including glacial ice, tabular icebergs and ice shelves over oceans. Meltwater is often found in the ablation zone of glaciers, where the rate of snow cover is reducing. Meltwater ca ...
, forming a
proglacial lake In geology, a proglacial lake is a lake formed either by the damming action of a moraine during the retreat of a melting glacier, a glacial ice dam, or by meltwater trapped against an ice sheet due to isostatic depression of the crust around th ...
, and later may be filled with
surface water Surface water is water located on top of land forming terrestrial (inland) waterbodies, and may also be referred to as ''blue water'', opposed to the seawater and waterbodies like the ocean. The vast majority of surface water is produced by pre ...
from streams or precipitation. When the glacier has more fully retreated this produces a
finger lake A finger lake, also known as a fjord lake or trough lake, is "a narrow linear body of water occupying a Overdeepening, glacially overdeepened valley and sometimes impounded by a Terminal moraine, morainic dam."Kotlyakov and Komarova (2007), 255. ...
or glacial piedmont lake (German: ''Zungenbeckensee'', known as a ''Gletscherendsee'' of the glacial series in the
Alpine Foreland The Alpine Foreland, less commonly called the Bavarian Foreland,Dickinson, Robert E (1964). ''Germany: A regional and economic geography'' (2nd ed.). London: Methuen, pp. 585-586. . Bavarian Plateau or Bavarian Alpine Foreland (german: Bayerisches ...
). The term ''Zungenbecken'' is of German origin, but used in English language sources.Charlesworth, J.K. (1966). ''The Quaternary Era: With Special Reference to its Glaciation'', in Two Volumes (Volumes 1–2) Examples are the
Tegernsee Tegernsee is a town in the Miesbach district of Bavaria, Germany. It is located on the shore of Lake Tegernsee, which is 747 m (2,451 ft) above sea level. A spa town, it is surrounded by an alpine landscape of Upper Bavaria, and has an ...
,
Ammersee Ammersee (English: Lake Ammer) is a Zungenbecken lake in Upper Bavaria, Germany, southwest of Munich between the towns of Herrsching and Dießen am Ammersee. With a surface area of approximately , it is the sixth largest lake in Germany. The la ...
,
Starnberger See Lake Starnberg, or ''Starnberger See'' ) — called Lake Würm, or ''Würmsee'' , until 1962 — is Germany's second-largest body of fresh water, having great depth, and fifth-largest lake by area. It and its surroundings lie in three different B ...
,
Lake Constance Lake Constance (german: Bodensee, ) refers to three bodies of water on the Rhine at the northern foot of the Alps: Upper Lake Constance (''Obersee''), Lower Lake Constance (''Untersee''), and a connecting stretch of the Rhine, called the Lak ...
,
Chiemsee Chiemsee () is a freshwater lake in Bavaria, Germany, near Rosenheim. It is often called "the Bavarian Sea". The rivers Tiroler Achen and Prien flow into the lake from the south, and the river Alz flows out towards the north. The Alz flows i ...
,
Tollensesee Tollensesee is a '' zungenbecken'' lake in Mecklenburg-Vorpommern, Germany. It belongs to the Mecklenburg Lake District. At an elevation of 14.8 m, its surface area is 17.4 km². Its maximum depth is about 33 m. The lake is 10.4 km lo ...
and the
Baltic Sea The Baltic Sea is an arm of the Atlantic Ocean that is enclosed by Denmark, Estonia, Finland, Germany, Latvia, Lithuania, Poland, Russia, Sweden and the North and Central European Plain. The sea stretches from 53°N to 66°N latitude and from ...
.


See also

*
Glacier A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such a ...
*
Drumlin A drumlin, from the Irish word ''droimnín'' ("littlest ridge"), first recorded in 1833, in the classical sense is an elongated hill in the shape of an inverted spoon or half-buried egg formed by glacial ice acting on underlying unconsolidated ...


References

{{topography-stub Glacial landforms