Trebel
| Trebel | ||
 The Trebel with tributaries |
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| Data | ||
| Water code | DE : 9666 (with Poggendorfer Trebel) | |
| location | Mecklenburg-Western Pomerania , Germany | |
| River system | Peene | |
| Drain over | Peene → Baltic Sea | |
| River basin district | Warnow / Peene | |
| source | near Zarnewanz, municipality of Süderholz 54 ° 3 ′ 35 ″ N , 13 ° 11 ′ 55 ″ E |
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| Source height | 22.5 m above sea level NHN | |
| muzzle | in the Peene coordinates: 53 ° 54 '52 " N , 13 ° 1' 11" E 53 ° 54 '52 " N , 13 ° 1' 11" E |
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| Mouth height | 0.1 m above sea level NHN | |
| Height difference | 22.4 m | |
| Bottom slope | 0.26 ‰ | |
| length | 87 km with Poggendorfer Tr., 69.5 km from the junction of Poggendorfer and Kronshorster Trebel | |
| Catchment area | 956 km² | |
| Left tributaries | Red moat | |
| Right tributaries | Kronhorster Trebel , Blinde Trebel , Warbel | |
| Small towns | Tribsees , Grimmen | |
 Trebel near Nehringen |
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The Trebel is a 70 km long river in Mecklenburg-Western Pomerania , with its longest source stream almost 87 km long . The name comes from Slavic and means something like river through Rodeland . The Trebel is mentioned for the first time when the city of Tribsees was granted by Wizlaw II in 1285.
Since there are numerous glacial valleys in Western Pomerania between Stralsund , Tribsees , Demmin and Greifswald , the Trebel is connected to several other bodies of water by ditches and streams.
The Poggendorfer Trebel , the longest spring stream, rises in Zarnewanz 22.5 meters above sea level. The Kronhorster Trebel as another source river, rises southeast of Franzburg . Both unite 3.8 meters above sea level in Grimmen .
From Grimmen, the Trebel first flows past Quitzin towards the west. About three kilometers after the Blinde Trebel empties from Franzburg to the north at 0.8 meters above sea level , it turns west around Tribsees to the south. Until the beginning of the 20th century there was a small shipping canal to Bad Sülze an der Recknitz, 6 km away . From the beginning of the Trebelbogen just above Tribsees to the confluence of the Peene in the Peene stream near Demmin , the river bed is consistently below sea level, as in the Recknitz from Bad Sülze.
From Tribsees to shortly before Demmin, the Trebel is the historical border between Mecklenburg and Pomerania. The old border line has been partially preserved to this day as the southern border of the Vorpommern-Rügen district . In the 1950s, however, a piece of the natural river below Tribsees was replaced by the Trebel Canal . After the confluence of the Warbel near Bassendorf (to Deyelsdorf ), the Trebel flows increasingly southeast. In the triangle bounded to the north and south-west of the course of the Trebel there is a complicated network of ditches with different directions of flow, which are connected to each other and connect to Trebel and Peene at several points. These include Ibitzgraben and Ibitzbach between Siemersdorf (to Tribsees) an der Trebel and Loitz an der Peene and the Rote Brückengraben between Ibitzgraben and Nehringen (to Grammendorf ) an der Trebel. In Demmin it flows into the Peene , 0.1 meters above sea level.
The river is a well-known and popular water hiking and fishing area. There are resting places for water hikers in Nehringen and Tribsees .
In the years 1998 to 2001, extensive renaturation measures were carried out in the border valley moor to Bassendorf as part of a LIFE project , with the aim of preserving natural water conditions and rewetting the drained moors.
Web links
literature
- Topographic maps 1: 100,000 C 1942 “Stralsund” and C 2342 “Demmin”, State Surveying Office Mecklenburg-Western Pomerania
Individual evidence
- ↑ a b c Geodata viewer of the Office for Geoinformation, Surveying and Cadastre of Mecklenburg-Western Pomerania ( information ) Topics: Water (with all classified waters) u. topographical background
- ↑ 2004 inventory according to the Water Framework Directive in the Warnow / Peene river basin district, published by the State Office for the Environment, Nature Conservation and Geology Mecklenburg-Vorpommern, Güstrow 2005, p. 4
- ↑ renaturation of the Flusstalmoore Recknitz and the average Cernosin (PDF; 340 kB) - Characteristics for WFD conversion was