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The Oder (/ ˈ oʊ d ər / OH-dər, German: ⓘ; Czech, Lower Sorbian and Polish: Odra; [a] Upper Sorbian: Wódra) 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 . [ 1 ]
The stream order or waterbody order is a positive whole number used in geomorphology and hydrology to indicate the level of branching in a river system.. There are various approaches [1] to the topological ordering of rivers or sections of rivers based on their distance from the source ("top down" [2]) or from the confluence (the point where two rivers merge) or river mouth ("bottom up" [3 ...
The Oder rises in the district of Goslar in the heart of the Harz Mountains. Its source is located in the southern part of the Brockenfeld about 1.3 km (0.81 mi) north of the Achtermannshöhe . The river's source is called the Odersprung or "Oder Leap."
West Oder (Polish: Odra Zachodnia) is the western arm of the lower Oder near Szczecin, Poland along the border with Germany.It flows into the Oder Lagoon.. The river flows through the Lower Oder Valley forming, along with the Eastern Oder (Polish: Odra Wschodnia), an area called Międzyodrze, part of the Lower Odra Valley Landscape Park.
It flows through Skośnica canal into West Oder and through Regalica into Dąbie Lake in the delta of the Oder river. The river flows through the Lower Oder Valley forming, along with the Western Oder (Polish: Odra Zachodnia), an area called Międzyodrze, part of the Lower Odra Valley Landscape Park. Międzyodrze area is traversed by a network ...
Channel patterns are found in rivers, streams, and other bodies of water that transport water from one place to another.Systems of branching river channels dissect most of the sub-aerial landscape, each in a valley proportioned to its size.
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The terms river morphology and its synonym stream morphology are used to describe the shapes of river channels and how they change in shape and direction over time. The morphology of a river channel is a function of a number of processes and environmental conditions, including the composition and erodibility of the bed and banks (e.g., sand, clay, bedrock); erosion comes from the power and ...