Rudower Fliess
| Rudower Fliess | ||
 Rudower Fliess |
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| Data | ||
| location | Großziethen , Berlin | |
| Beginning | Kleinziethener Rieselfelder 52 ° 22 ′ 23 ″ N , 13 ° 26 ′ 35 ″ E |
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| muzzle |
Teltow Canal at the Rudow tank farm Coordinates: 52 ° 26 ′ 1 ″ N , 13 ° 29 ′ 46 ″ E 52 ° 26 ′ 1 ″ N , 13 ° 29 ′ 46 ″ E
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| Big cities | Berlin | |
The Rudower Fließ is a 9.2 kilometer long sand-shaped lowland stream in the Berlin district of Rudow in the Neukölln district . It is also known as Rudow's tear gland due to its formation as an Ice Age meltwater channel .
course
The flow begins in the Kleinziethener Rieselfeldern and is fed in its course to the northeast by irrigation ditches and the Waßmannsdorf sewage treatment plant . It runs as a deep, wide ditch parallel to Rudower Damm, the former road from Kleinziethen to Rudow, to the Berlin Wall Trail . After flowing through a long culvert , the river crosses the border with Berlin. Here the landscape of the Rudower Fließ changes significantly: Dense trees and aquatic plants mark the further course. After crossing under the poultry walkway, there are small floodplains and bogs , which offer an ideal habitat for pond rails. Here the short Meskengraben flows into the Rudower Fließ. It crosses under the Groß-Ziethener-Chaussee and maintains its north-eastern course. It flows through another moor before it turns north-east just before Neuköllner Straße and the last meters above ground are already canalised. Immediately in front of the Sculptor's Path, the flow disappears into an underground channel. This runs in a north-easterly direction below the Ehrenpreisweg and Stubenrauchstrasse to the Rudow tank farm . This is crossed under, where the water finally pours into the Teltow Canal .
history
The channel was formed around 12,000 years ago during the last Glaciation of the Vistula . The rise in temperatures caused snow and ice to melt; the resulting meltwater collected in depressions that formed into a channel. The stream that was created in this way was spared human interference for many centuries. Between the First and Second World War , the section between Neuköllner Straße and Teltow Canal was channeled and laid underground as part of the development of the settlements in northern Rudow. After the end of the Second World War, there was a further denaturation : residents straightened the bank and built structures near it. The sewage treatment plant in Waßmannsdorf also used the stream as a receiving water for the Berlin Rieselfelder . The Senate Administration therefore had the river bed straightened and lined with concrete shells so that the polluted wastewater could drain away more quickly. In the 1980s, it was carefully dismantled. The concrete shells were largely removed, the river bed was stretched and widened in a serpentine fashion, and bank plants were settled on the banks and bushes and trees were planted.
Web links
Individual evidence
- ↑ Rudower Fließ (flowing waters - identifier: DE_RW_DEBB58382_1737) , water body profile surface water body of the 2nd management plan according to the Water Framework Directive, accessed on March 18, 2018.
- ↑ Route 5 Rudow - Rudower Fließ and Meskengraben , website of the Gartenkulturpfads Neukölln, accessed on November 18, 2015.
- ↑ Walk to the “tear gland” and view of the village in Rudow . In: Berliner Morgenpost , December 30, 2012, accessed on November 18, 2015.
- ↑ Archived copy ( memento of the original from November 19, 2015 in the Internet Archive ) Info: The archive link was inserted automatically and has not yet been checked. Please check the original and archive link according to the instructions and then remove this notice. Christian Klingenfuß, Diana Möller, Christian Heller, Tina Thrum, Jutta Zeitz: Rudower Fließ , work for the Humboldt University in Berlin, June 2015, (PDF), website Berliner Moorboden im Klimawandel of the HU, accessed on November 18, 2015.
- ^ Rivers and lakes in Germany (The great ADAC travel and leisure guide), Munich / Stuttgart 1988, p. 112 f. ISBN 3-87003-299-5
