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The Oder (/ ˈ oʊ d ər / OH-dər [a]; Czech and Polish: Odra [b]) 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 ...
River name Emptying into Total length Length in Poland Total basin area Basin area in Poland km mi km mi km 2 sq mi km 2 sq mi; Vistula: Baltic Sea: 1,022 635 1,022 635 193,690 74,780 168,868 65,200 Oder: Baltic Sea: 840 520 726 451 119,074 45,975 106,043 40,943 Warta: Oder: 795 494 795 494 54,520 21,050 54,520 21,050 Bug: Narew: 774 481 590 ...
Many atmospheric river events are weak. But the powerful ones can transport extraordinary amounts of moisture. Studies have shown that they can carry seven to 15 times the average amount of water discharged daily by the Mississippi River, according to the U.S. Geological Survey. What happens when an atmospheric river reaches land?
branch of river Oder (from Oder Lagoon) Świna/Swine (in Świnoujście, Poland) Uecker (into Oder Lagoon in Ueckermünde) Oder (into Oder Lagoon near Szczecin, Poland) Lusatian Neisse (Lausitzer Neiße) (near Eisenhüttenstadt)
what is an atmospheric river? Atmospheric rivers are long and relatively narrow bands of water vapor that form over an ocean and flow through the sky, transporting much of the moisture from the ...
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.
Formation of a river anticline by river erosion and the associated isostatic rebound. As the river erodes the overlying material, the underlying rocks will rebound up, like a block in water if you remove a weight from on top of it, forming an antiformal structure. (Image created by Michael Stevens)