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The Seerhein ("Lake Rhine") is a river about four kilometres long, in the basin of Lake Constance. It is the outflow of the Upper Lake Constance and the main tributary of the Lower Lake Constance. The water level of the lower lake is about 30 cm below the level of the Upper Lake. It is considered part of the Rhine, which flows into Lake Constance as the Alpine Rhine and flows out of the Lake as the High Rhine. The Seerhein arose after the last ice age (the Würm glaciation, about 9650 BCE). Some time after this period, the water level of Lake Constance gradually dropped by about ten metres and the shallow parts fell dry. Some parts of the Seerhein still have a character a bit like a lake.

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  • Seerhein (de)
  • Seerhein (fr)
  • Seerhein (en)
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  • Der Seerhein ist ein etwa vier Kilometer langer, im Bodenseebecken liegender Abschnitt des Flusses Rhein. Er ist der Abfluss des Obersees und Hauptzufluss des Untersees. Der Unterschied zwischen den Wasserspiegeln beider Seen beträgt im langjährigen Mittel der Jahresmittel genau 20 cm, in den langjährigen Mitteln der Monatsmittel zwischen 16 und 27 cm. Durch die Mitte des Seerheins verläuft teilweise die Grenze zwischen Deutschland und der Schweiz, größte Gemeinde an seinem Ufer ist Konstanz. Sein östlichster Punkt markiert zugleich den Beginn (km 0,0) der Rheinkilometrierung. (de)
  • Le Seerhein (littéralement « Rhin de lac ») est la portion du Rhin qui relie l'Obersee à l'Untersee, les deux composantes du lac de Constance. Long de 4,3 km, il traverse la ville de Constance, puis sert de frontière entre l'Allemagne (Bade-Wurtemberg) et la Suisse (Thurgovie). (fr)
  • The Seerhein ("Lake Rhine") is a river about four kilometres long, in the basin of Lake Constance. It is the outflow of the Upper Lake Constance and the main tributary of the Lower Lake Constance. The water level of the lower lake is about 30 cm below the level of the Upper Lake. It is considered part of the Rhine, which flows into Lake Constance as the Alpine Rhine and flows out of the Lake as the High Rhine. The Seerhein arose after the last ice age (the Würm glaciation, about 9650 BCE). Some time after this period, the water level of Lake Constance gradually dropped by about ten metres and the shallow parts fell dry. Some parts of the Seerhein still have a character a bit like a lake. (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Bodensee_satellit.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Konstanz_Blick_vom_Münsterturm.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Rheinkilometer_Loreley.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/SantaCruz-PeritoMoreno-P2140146b.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Konstanz_1553.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Konstanz_Rheintorturm.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Seerhein_02.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Wasserwunder_Konstanz.jpg
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