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  2. Oder - Wikipedia

    en.wikipedia.org/wiki/Oder

    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 ]

  3. Stream order - Wikipedia

    en.wikipedia.org/wiki/Stream_order

    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 ...

  4. Oder (Harz) - Wikipedia

    en.wikipedia.org/wiki/Oder_(Harz)

    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."

  5. Oder–Neisse line - Wikipedia

    en.wikipedia.org/wiki/Oder–Neisse_line

    The Oder–Neisse line (German: Oder-Neiße-Grenze, Polish: granica na Odrze i Nysie Łużyckiej) is an unofficial term for the modern border between Germany and Poland. The line generally follows the Oder and Lusatian Neisse rivers, meeting the Baltic Sea in the north.

  6. Bóbr - Wikipedia

    en.wikipedia.org/wiki/Bóbr

    The Bóbr has a length of 279 kilometres (173 mi) (3 in Czech Republic, 276 in Poland, 10th longest Polish river) and a basin area of 5,874 square kilometres (2,268 sq mi) (44 in Czech Republic and 5,830 in Poland). [2] It originates on a slope of the Rýchory mountains in the southeast of the Krkonoše range.

  7. River morphology - Wikipedia

    en.wikipedia.org/wiki/River_morphology

    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 ...

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  9. Body of water - Wikipedia

    en.wikipedia.org/wiki/Body_of_water

    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