Urstromtal in the context of Glacial series


Urstromtal in the context of Glacial series

⭐ Core Definition: Urstromtal

An urstromtal (plural: Urstromtäler) is a type of broad glacial valley, for example, in northern Central Europe, that appeared during the ice ages, or individual glacial periods of an ice age, at the edge of the Scandinavian ice sheet and was formed by meltwaters that flowed more or less parallel to the ice margin. Urstromtäler are an element of the glacial series. The term is German and means "ancient stream valley". Although often translated as "glacial valley", it should not be confused with a valley carved out by a glacier. More accurately some sources call them "meltwater valleys" or "ice-marginal valleys".

↓ Menu
HINT:

In this Dossier

Urstromtal in the context of Pomerania

Pomerania (Polish: Pomorze [pɔˈmɔʐɛ] ; German: Pommern [ˈpɔmɐn] ; Kashubian: Pòmòrskô; Swedish: Pommern) is a historical region on the southern shore of the Baltic Sea in Central Europe, split between Poland and Germany. The central and eastern part belongs to the West Pomeranian, Pomeranian and Kuyavian-Pomeranian voivodeships of Poland, while the western part belongs to the German states of Mecklenburg-Western Pomerania and Brandenburg.

Pomerania's historical border in the west is the Mecklenburg-Western Pomeranian border Urstromtal, which now constitutes the border between the Mecklenburgian and Pomeranian part of Mecklenburg-Western Pomerania, while it is bounded by the Vistula River in the east. The easternmost part of Pomerania is alternatively known as Pomerelia, consisting of four sub-regions: Kashubia inhabited by ethnic Kashubians, Kociewie, Tuchola Forest and Chełmno Land.

View the full Wikipedia page for Pomerania
↑ Return to Menu