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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 ]
Fierljeppen in Linschoten Newsreel footage of the 1961 Fierljeppen Championships in Winsum. Fierljeppen (West-Frisian compound of fier—"far" and ljeppen—"leaping") or polsstokverspringen is a traditional sport of the West Frisian people in the Dutch province of Fryslân.
A site along the route of a stream or river, used for reference marking or water monitoring. [34] Thalweg The river's longitudinal section, or the line joining the deepest point in the channel at each stage from source to mouth. Watercourse The channel followed by a stream (a flowing body of water) [36] or the stream itself.
The river Warta (/ ˈ v ɑːr t ə / VAR-tə, Polish: ⓘ; German: Warthe ⓘ; Latin: Varta) rises in central Poland and meanders greatly through the Polish Plain in a north-westerly direction to flow into the Oder at Kostrzyn nad Odrą on Poland's border with Germany.
A river is a natural freshwater stream that flows on land or inside caves towards another body of water at a lower elevation, such as an ocean, lake, or another river. A river may run dry before reaching the end of its course if it runs out of water, or only flow during certain seasons.
the location where a river flows into an ocean, sea, estuary, lake, or reservoir. Distributary or distributary channel: a stream that branches off and flows away from the main stream channel. Drainage basin: a region of land where water from rain or snowmelt drains downhill into another body of water, such as a river, lake, or reservoir. Draw
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 ...
Water chemistry in river ecosystems varies depending on which dissolved solutes and gases are present in the water column of the stream. Specifically river water can include, apart from the water itself, [citation needed] dissolved inorganic matter and major ions (calcium, sodium, magnesium, potassium, bicarbonate, sulphide, chloride)
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