An ''urstromtal'' (plural: ''Urstromtäler'') is a type of broad glacial
valley
A valley is an elongated low area often running between hills or mountains and typically containing a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over ...
, for example, in northern
Central Europe
Central Europe is a geographical region of Europe between Eastern Europe, Eastern, Southern Europe, Southern, Western Europe, Western and Northern Europe, Northern Europe. Central Europe is known for its cultural diversity; however, countries in ...
, that appeared during the
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 g ...
s, or individual
glacial period
A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate betw ...
s of an ice age, at the edge of the Scandinavian
ice sheet
In glaciology, an ice sheet, also known as a continental glacier, is a mass of glacier, glacial ice that covers surrounding terrain and is greater than . The only current ice sheets are the Antarctic ice sheet and the Greenland ice sheet. Ice s ...
and was formed by meltwaters that flowed more or less parallel to the ice margin. ''Urstromtäler'' are an element of the
glacial series
The glacial series refers to a particular sequence of landforms in Central Europe that were formed during the Last glacial period, Pleistocene glaciation beneath the ice sheets, along their margins and on their forelands during each glacial advance ...
. 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".
Emergence and structure

Important for the emergence of the ''Urstromtäler'' is the fact that the general lie of the land on the
North German Plain
The North German Plain or Northern Lowland () is one of the major geographical regions of Germany. It is the German part of the North European Plain. The region is bounded by the coasts of the North Sea and the Baltic Sea to the north, Germany's ...
and in
Poland
Poland, officially the Republic of Poland, is a country in Central Europe. It extends from the Baltic Sea in the north to the Sudetes and Carpathian Mountains in the south, bordered by Lithuania and Russia to the northeast, Belarus and Ukrai ...
slopes down from south to north. Thus the ice sheet that advanced from Scandinavia flowed into a rising terrain. The meltwaters could therefore only flow for a short distance southwards over the
sandurs (outwash plains) before having to find a way to the
North Sea
The North Sea lies between Great Britain, Denmark, Norway, Germany, the Netherlands, Belgium, and France. A sea on the European continental shelf, it connects to the Atlantic Ocean through the English Channel in the south and the Norwegian Se ...
basin that was parallel to the ice margin. At that time, the area that is now the North Sea was dry as a result of the low level of the sea.
As elements of the glacial series, ''Urstromtäler'' are intermeshed with sandur areas for long stretches along their northern perimeters. It was over these outwash plains that the meltwaters poured into them. ''Urstromtäler'' are relatively uniformly composed of
sand
Sand is a granular material composed of finely divided mineral particles. Sand has various compositions but is usually defined by its grain size. Sand grains are smaller than gravel and coarser than silt. Sand can also refer to a textural ...
s and
gravel
Gravel () is a loose aggregation of rock fragments. Gravel occurs naturally on Earth as a result of sedimentation, sedimentary and erosion, erosive geological processes; it is also produced in large quantities commercially as crushed stone.
Gr ...
s; the grain size can vary considerably, however. Fine sand dominates especially in the upper sections of the ''Urstromtal'' sediments. The thickness of the ''Urstromtal'' sediments also varies a great deal, but is mostly well over ten metres.
''Urstromtäler'' have wide and very flat valley bottoms that are between 1.5 and 20 kilometres wide. The valley sides, by contrast are only a few to a few dozen metres high. The bottom and the edges of an ''Urstromtal'' may have been significantly altered by more recent processes, especially the thawing of
dead ice blocks or the accumulation of
sand dune
A dune is a landform composed of wind- or water-driven sand. It typically takes the form of a mound, ridge, or hill. An area with dunes is called a dune system or a dune complex. A large dune complex is called a dune field, while broad, flat ...
s. In the
post-glacial period, many ''Urstromtäler'' became bogs due to their low lying situation and the high water table.
Central Europe

In
Central Europe
Central Europe is a geographical region of Europe between Eastern Europe, Eastern, Southern Europe, Southern, Western Europe, Western and Northern Europe, Northern Europe. Central Europe is known for its cultural diversity; however, countries in ...
, there are several ''Urstromtäler'' from various periods.
* Breslau-Magdeburg-Bremen ''Urstromtal''; (
Poland
Poland, officially the Republic of Poland, is a country in Central Europe. It extends from the Baltic Sea in the north to the Sudetes and Carpathian Mountains in the south, bordered by Lithuania and Russia to the northeast, Belarus and Ukrai ...
,
Germany
Germany, officially the Federal Republic of Germany, is a country in Central Europe. It lies between the Baltic Sea and the North Sea to the north and the Alps to the south. Its sixteen States of Germany, constituent states have a total popu ...
); formed during the
Saale glaciation
* Glogau-Baruth ''Urstromtal''; (Poland, Germany); formed during the
Weichselian
* Warsaw-Berlin ''Urstromtal''; (Poland, Germany); formed during the Weichselian
* Thorn-Eberswalde ''Urstromtal''; (Poland, Germany); formed during the Weichselian
* The term
Elbe ''Urstromtal'' refers to the
Elbe valley roughly at the height of
Genthin to the Elbe estuary at
Cuxhaven
Cuxhaven (; ) is a town and seat of the Cuxhaven district, in Lower Saxony, Germany. The town includes the northernmost point of Lower Saxony. It is situated on the shore of the North Sea at the mouth of the Elbe River. Cuxhaven has a footprint o ...
. The meltwaters of the three above-mentioned Weichselian ''Urstromtäler'' flowed successively through this valley towards the North Sea basin.
* The term Rhine ''Urstromtal'' for the
Rhine
The Rhine ( ) is one of the List of rivers of Europe, major rivers in Europe. The river begins in the Swiss canton of Graubünden in the southeastern Swiss Alps. It forms part of the Swiss-Liechtenstein border, then part of the Austria–Swit ...
valley from
Düsseldorf
Düsseldorf is the capital city of North Rhine-Westphalia, the most populous state of Germany. It is the second-largest city in the state after Cologne and the List of cities in Germany with more than 100,000 inhabitants, seventh-largest city ...
to its mouth on the North Sea is disputed. The Rhine was certainly a route for meltwaters during the Saale glaciation. The structure of the valley is however clearly older and was formed by recent
tectonics
Tectonics ( via Latin ) are the processes that result in the structure and properties of the Earth's crust and its evolution through time. The field of ''planetary tectonics'' extends the concept to other planets and moons.
These processes ...
.
* In the
Alpine glaciation zone of Central Europe the term ''Urstromtal'' is not used. In this region, the
Danube
The Danube ( ; see also #Names and etymology, other names) is the List of rivers of Europe#Longest rivers, second-longest river in Europe, after the Volga in Russia. It flows through Central and Southeastern Europe, from the Black Forest sou ...
and, periodically, the
Rhine
The Rhine ( ) is one of the List of rivers of Europe, major rivers in Europe. The river begins in the Swiss canton of Graubünden in the southeastern Swiss Alps. It forms part of the Swiss-Liechtenstein border, then part of the Austria–Swit ...
carried the meltwaters away.
Some sections of the aforementioned main valleys have been given their own names. The Lusatian ''Urstromtal'' and the Aller ''Urstromtal'' are parts of the Breslau-Magdeburg-Bremen ''Urstromtal''. The Baruth, Berlin and Eberswalde ''Urstromtäler'' are common short names for the associated sections of the ''Urstromtal'' in
Brandenburg
Brandenburg, officially the State of Brandenburg, is a States of Germany, state in northeastern Germany. Brandenburg borders Poland and the states of Berlin, Mecklenburg-Vorpommern, Lower Saxony, Saxony-Anhalt, and Saxony. It is the List of Ger ...
.
In addition to the large main valleys there are also numerous smaller meltwater valleys (''Urstromtalungen''). Their appearance is similar to that of the great ''Urstromtäler'', but they are considerably shorter. They are also not linked to a sandur and a
terminal moraine
A terminal moraine, also called an end moraine, is a type of moraine that forms at the terminal (edge) of a glacier, marking its maximum advance. At this point, debris that has accumulated by plucking and abrasion, has been pushed by the front e ...
.
''Urstromtäler'' of Central Europe (Poland, Germany and Denmark especially) were directly connected to the North Atlantic Ocean, via the
Channel River, during Pleistocene maximum glaciations, i.e. at times of confluence of the British and Fennoscandian ice-sheets in the intervening North Sea.
Features
''Urstromtäler'' should not be confused with
tunnel valleys. The latter are formed beneath, not in front of, the ice mass. In addition most tunnel valleys run from north to south. The principal direction of ''Urstromtäler'' is from east to west. Today ''Urstromtäler'' are only partly used by rivers, because the majority have found shorter routes to the sea (like the
Oder
The Oder ( ; Czech and ) is a river in Central Europe. It is Poland's second-longest river and third-longest within its borders after the Vistula and its largest tributary the Warta. The Oder rises in the Czech Republic and flows through wes ...
and
Vistula
The Vistula (; ) is the longest river in Poland and the ninth-longest in Europe, at in length. Its drainage basin, extending into three other countries apart from Poland, covers , of which is in Poland.
The Vistula rises at Barania Góra i ...
). The straight troughs of the ''Urstromtäler'' between the rivers were used for canal routes due to their low gradient, for example for the
Elbe–Havel Canal or the
Oder–Havel Canal.
Because the land in
North America
North America is a continent in the Northern Hemisphere, Northern and Western Hemisphere, Western hemispheres. North America is bordered to the north by the Arctic Ocean, to the east by the Atlantic Ocean, to the southeast by South Ameri ...
and on the
Russian Plain tilts towards the south, the formation of ''Urstromtäler'' there during the ice age did not take place. The
Mississippi River
The Mississippi River is the main stem, primary river of the largest drainage basin in the United States. It is the second-longest river in the United States, behind only the Missouri River, Missouri. From its traditional source of Lake Ita ...
and its tributaries carried the meltwaters of the North American ice sheet away. In Eastern Europe the meltwaters flowed down the river basins of the
Dnieper
The Dnieper or Dnepr ( ), also called Dnipro ( ), is one of the major transboundary rivers of Europe, rising in the Valdai Hills near Smolensk, Russia, before flowing through Belarus and Ukraine to the Black Sea. Approximately long, with ...
,
Don and
Volga
The Volga (, ) is the longest river in Europe and the longest endorheic basin river in the world. Situated in Russia, it flows through Central Russia to Southern Russia and into the Caspian Sea. The Volga has a length of , and a catchment ...
.
''Urstromtäler'', whether sandy or boggy, posed considerable obstacles to movement in the
Middle Ages
In the history of Europe, the Middle Ages or medieval period lasted approximately from the 5th to the late 15th centuries, similarly to the post-classical period of global history. It began with the fall of the Western Roman Empire and ...
. As a result, the
trade routes
A trade route is a Logistics, logistical network identified as a series of pathways and stoppages used for the commercial transport of cargo. The term can also be used to refer to trade over land or water. Allowing Good (economics and accounting ...
converged on points where the valley could be crossed comparatively easily. These hubs thus became favourite sites for the founding of towns or castles. Examples from the German state of Brandenburg include
Berlin
Berlin ( ; ) is the Capital of Germany, capital and largest city of Germany, by both area and List of cities in Germany by population, population. With 3.7 million inhabitants, it has the List of cities in the European Union by population withi ...
,
Fürstenwalde,
Luckenwalde
Luckenwalde (; Upper Sorbian language, Upper and , , ) is the capital of the Teltow-Fläming district in the state of Brandenburg in eastern Germany. It is situated on the Nuthe river north of the Fläming Heath, at the eastern rim of the Nuthe-Ni ...
and
Baruth/Mark
Baruth/Mark () is a town in the Teltow-Fläming district of Brandenburg, Germany. It is situated 24 km east of Luckenwalde, and 53 km south of Berlin.
Geography
Baruth/Mark is structured in the following parts of town,Main constituti ...
, and from Lower Saxony the town of
Vorsfelde and
Wolfsburg Castle.
See also
*
Strath
*
Urstrom The Urstrom is a geologists' name for a great glacial age river of the Polish and north German plain, which drained the combined melt-waters from the northern headwaters of the Alps and the southern part of the Scandinavian ice during the Devens ...
References
Literature
* H. Liedtke: ''Die nordischen Vereisungen in Mitteleuropa''. 2nd ed., Trier 1981, , 307 p.
* H. Liedtke, J. Marcinek (ed.): ''Physische Geographie Germanys''. 3rd ed., Gotha 2002, , 786 p.
* Johannes H. Schroeder (ed.): ''Führer zur Geologie von Berlin und Brandenburg, No. 2, Bad Freienwalde – Parsteiner See''. 2nd improved edition. Geowissenschaftler in Berlin und Brandenburg e. V., Selbstverlag, Berlin 1994, ,
* Johannes H. Schroeder (ed.): ''Führer zur Geologie von Berlin und Brandenburg, No. 5, Nordwestlicher Barnim – Eberswalder Urstromtal''. Geowissenschaftler in Berlin und Brandenburg e. V., Selbstverlag, Berlin 2004, ,
* Johannes H. Schroeder (ed.): ''Führer zur Geologie von Berlin und Brandenburg, No. 9, Oderbruch – Märkische Schweiz – Östlicher Barnim''. Geowissenschaftler in Berlin und Brandenburg e. V., Selbstverlag, Berlin 2003, ,
{{Authority control
*
Glaciology