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Tongue Basin
A ''Zungenbecken'', also called a tongue basin or tongue-basin, 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.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 A drumlin, from the Iri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tegernsee (lake)
The Tegernsee is a ''Zungenbecken'' lake in the Bavarian Alps in southern Germany. The lake is the centre of a popular recreation area south-east of Munich. Resorts on the lake include the eponymous Tegernsee, as well as Bad Wiessee, Kreuth, Gmund, and Rottach-Egern. The lake is some in length, with a width of and an area of . It reaches a maximum depth of , with an average depth of , and the normal water level is above sea level. The lake flows into the River Mangfall, a tributary of the River Inn and thence the River Danube. The buildings of the former Benedictine monastery of Tegernsee Abbey lie on the banks of the lake. Now in private hands, they are now known as ''Schloss Tegernsee''. The area around the lake is linked to Munich by rail through trains of the Bayerische Oberlandbahn, which, in the final part of their journey, travel over the tracks of the privately owned Tegernsee-Bahn. Pleasure boat services serve several points on the lake, and are operated by boat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 10°E to 30°E longitude. A marginal sea of the Atlantic, with limited water exchange between the two water bodies, the Baltic Sea drains through the Danish Straits into the Kattegat by way of the Øresund, Great Belt and Little Belt. It includes the Gulf of Bothnia, the Bay of Bothnia, the Gulf of Finland, the Gulf of Riga and the Bay of Gdańsk. The " Baltic Proper" is bordered on its northern edge, at latitude 60°N, by Åland and the Gulf of Bothnia, on its northeastern edge by the Gulf of Finland, on its eastern edge by the Gulf of Riga, and in the west by the Swedish part of the southern Scandinavian Peninsula. The Baltic Sea is connected by artificial waterways to the White Sea via the White Sea–Baltic Canal and to the German ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 long and between 1.5 and 2.5 km wide. The entire lake lies within the administrative area of the city of Neubrandenburg. In the south part of the lake there is island Fischerinsel Fischerinsel (, ''Fisher Island'') is the southern part of the island in the River Spree which was formerly the location of the city of Cölln and is now part of central Berlin. The northern part of the island is known as Museum Island. Fischerinse .... See also * External links * * Lakes of Mecklenburg-Western Pomerania Neubrandenburg LTollensesee {{Neubrandenburg-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 into the Inn which then merges with the Danube. The Chiemsee is divided into the bigger, north section, in the northeast, called , and the , in the southwest. The Chiemgau, the region surrounding the Chiemsee, is a popular recreation area. Origin The Chiemsee was formed, like many other pre-alpine lakes, at the end of the last ice age about 10,000 years ago from a hollow carved out by a glacier (a ). Originally the lake covered an area of almost , which is about three times its present area. Within 10,000 years its area had shrunk to around . Before 1904 the water level was lowered by about a metre. As a result, large areas of dry land were reclaimed. Islands There are three main islands on the lake: Herreninsel ("gentlemen's island" ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Constance
Lake Constance (german: Bodensee, ) refers to three Body of water, 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 Seerhein, Lake Rhine (''Seerhein''). These waterbodies lie within the Lake Constance Basin () in the Alpine Foreland through which the Rhine flows. The lake is situated where Germany, Switzerland, and Austria meet. Its shorelines lie in the German states of Baden-Württemberg and Bavaria, the Swiss cantons of Canton of St. Gallen, St. Gallen, Canton of Thurgau, Thurgau, and Canton of Schaffhausen, Schaffhausen, and the Austrian state of Vorarlberg. The actual location of the border Lake_Constance#International_borders, is disputed. The Alpine Rhine forms in its original course the Austro-Swiss border and flows into the lake from the south. The High Rhine flows westbound out of the lake and forms (with the exception of the Canton ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Bavarian districts, or ''Landkreise''. The lake is property of the state and accordingly managed by the Bavarian Administration of State-Owned Palaces, Gardens and Lakes. Located in southern Bavaria southwest of Munich, Lake Starnberg is a popular recreation area for the city and, since 1976, one of the wetlands of international importance protected by the Ramsar Convention. The small town of Berg is famous as the site where King Ludwig II of Bavaria was found dead in the lake in 1886. Because of its associations with the Wittelsbach royal family, the lake is also known as Fürstensee (Prince's Lake). It is also mentioned in T. S. Eliot's poem ''The Waste Land''. Overview The lake, lying in a ''zungenbecken'' or glacial hollow, was create ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 lake is at an elevation of , and has a maximum depth of . Like other Bavarian lakes, Ammersee developed as a result of the ice age glaciers melting. Ammersee is fed by the River Ammer, which flows as the Amper out of the lake. Like neighbouring Lake Starnberg - deeper, bigger in surface area, similar in shape - it is a popular location for watersports. Ammersee and the Amper are part of the ancient Celtic amber trading route leading to the Brenner Pass. The word ''Ammer'' is a 13th-century form of ''Amper'', the Celtic ''*ambra'', deriving from the Indo-European ''*ombh-, *mbh-'' "wet, Water". Passenger services have operated on the lake since 1879. Today they are operated by the Bayerische Seenschifffahrt company, using a mixture of histor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Alpenvorland), refers to a triangular region of plateau and rolling foothills in Southern Germany, stretching from Lake Constance in the west to beyond Linz on the Danube in the east, with the Bavarian Alps forming its south boundary and the Danube its northern extent. Geography The Alpine Foreland has been shaped under the influence of the ice ages and has a rich variety of landforms. A molasse basin of extensive Tertiary and Quaternary sediments —silt and clay, sand and sedimentary rocks from Alpine erosion— overlay the Alpine nappes. Features such as the morainic hills, gravel sandar and lakes have left a record of various glaciation stages in this region. The Alpine Foreland is crossed by the rivers Iller, Wertach, Lech, Isar a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Map Ammersee
A map is a symbolic depiction emphasizing relationships between elements of some space, such as objects, regions, or themes. Many maps are static, fixed to paper or some other durable medium, while others are dynamic or interactive. Although most commonly used to depict geography, maps may represent any space, real or fictional, without regard to context or scale, such as in brain mapping, DNA mapping, or computer network topology mapping. The space being mapped may be two dimensional, such as the surface of the earth, three dimensional, such as the interior of the earth, or even more abstract spaces of any dimension, such as arise in modeling phenomena having many independent variables. Although the earliest maps known are of the heavens, geographic maps of territory have a very long tradition and exist from ancient times. The word "map" comes from the , wherein ''mappa'' meant 'napkin' or 'cloth' and ''mundi'' 'the world'. Thus, "map" became a shortened term referring to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Finger Lake
A finger lake, also known as a fjord lake or trough lake, is "a narrow linear body of water occupying a glacially overdeepened valley and sometimes impounded by a morainic dam."Kotlyakov and Komarova (2007), 255. Where one end of a finger lake is drowned by the sea, it becomes a fjord or sea-loch. Examples New Zealand * Lake Wakatipu, Otago, South Island. United Kingdom England * Many of the lakes of the Lake District are finger lakes. Scotland * Many lochs of Scotland are finger lakes. Some like Loch Broom and Loch Maree form fjord and finger lake systems. Wales * Many of the Welsh llyns. United States * Finger Lakes, New York State See also * ''Zungenbecken A ''Zungenbecken'', also called a tongue basin or tongue-basin, 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: ''Glets ...'' * References Literature *Hamblin, P.F ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
