Stege and Waidbach
| Waidbach | ||
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| Data | ||
| Water code | DE : 96486 | |
| location | Germany , Mecklenburg-Western Pomerania | |
| River system | Warnow | |
| Drain over | Beke → Warnow → Baltic Sea | |
| Origin: pseudobifurcation | Bridge between Konow u. Wilsen 54 ° 3 ′ 33 " N , 11 ° 59 ′ 33" E |
|
| Source height | 24 m above sea level NHN | |
| muzzle | at the Dachsberg in the Beke coordinates: 53 ° 58 '36 " N , 12 ° 0' 46" E 53 ° 58 '36 " N , 12 ° 0' 46" E |
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| Mouth height | 3 m above sea level NHN | |
| Height difference | 21 m | |
| Bottom slope | 1.8 ‰ | |
| length | 11.4 km | |
| Bridges | |
| Water code |
DE / 9638 (together with the lower course of the Mühlenfließ), 963812 (top water ), 96388 (old lower course) |
| location | Germany , Mecklenburg-Western Pomerania |
| River system | originally own, now Mühlenfließ |
| Drain over | (Mühlenfließ) → Baltic Sea |
| source | Dänenberg near Hanstorf 54 ° 3 ′ 15 ″ N, 11 ° 56 ′ 59 ″ E |
| Source height | 76 m above sea level NHN |
| Mouth | Originally at Heiligendamm 53 ° 58 '36 "N, 11 ° 52' 8" E now in Bad Doberan 54 ° 6 '58 "N, 11 ° 55' 0" E |
| Mouth height | 0 m above sea level NHN |
| Height difference | 76 m |
| length | hydrological 21 km, nominally 5.3 - 14.7 km |
| Flowing lakes | Conventer See (old lower reaches) |
| Small towns | Bad Doberan |
The brooks Stege and Waidbach in the Rostock district in Mecklenburg-Western Pomerania form with their common source brooks one of the numerous pseudobifurcations in northeast Germany.
Spring streams
The source streams, all of which are not classified, come from valleys in the vicinity of the 93 m high Dänenberg on the east side of the eastern part of the cooling , the Ivendorfer Heights south of Bad Doberan , and form three groups:
- The northern group consists of a spring 73 m above sea level, the brook of which flows south around the 60.6 m high Kreigenberg and a tributary of about the same length north of this hill promontory.
- Next south there is a single inlet that seeps south of the Vossberg twice before it reaches the bottom of the valley.
- The source streams of the southern group unite at the Hanstorf district of Konow . From there a part flows entirely above ground to the north, and a body of water fed by underground branches to the northeast. The latter may temporarily have flowed off towards Waidbach. The westernmost of these springs is the one with the longest stretch of water to the confluence of Stege and Mühlenfließ at the Jemnitz lock.
Apex area
The natural watershed that can be derived from the contour lines is likely to have been between (east of) Neuhof and (east of) Konow. The map display from 1900 clearly shows where the water flowed south, but no flow arrows to the north. However, the river bed between Parkentin and Konow has been artificially deepened. The maintenance by the water and soil association aims at a flow limit under the way from Konow to Wilsen. The waterway indicators are also based on this. Nevertheless, individual maps let the Waidbach begin one kilometer further north.
Drains
Waidbach
To the south the Waidbach flows through a meadow valley to the west past Stäbelow and the Fahrenholzer Wald nature reserve . After about eight kilometers, the Waidbach is crossed by the Bundesautobahn 20 with a valley bridge. After another four kilometers it flows southeast of the Satow district of Matersen or southwest of Ziesendorf at 3.3 m above sea level. NHN in the Beke , which reaches the Warnow after about twelve more river kilometers in Schwaan .
Bridges
The northern outflow is called the footbridges. It runs through Parkentin and Bartenshagen and joins the Rotbäk (or Rotbach ) after eight kilometers . Just 80 meters behind the junction there is another branch : the greater part of the water is directed to the west as a footbridge (formerly part of the Rotbach) and after two kilometers on the northern edge of Bad Doberan it reaches the Mühlenfließ , which flows into the Baltic Sea northeast of Heiligendamm . The mill flow below the confluence of the Stegekanal is classified as the same river as the Stege. The smaller part of the water is let through a sluice in the flood dam of the Rotbach or Stegekanals and flows as footbridges north of the aforementioned watercourse through fields and meadows of the Conventer Niederung into the Conventer See, which is surrounded by moor . It has an area of a good one square kilometer and is separated from the seashore by a land bridge less than half a kilometer wide, the Holy Dam , after which the seaside resort is named. Its course flows together with the mill flow through the Jemnitz lock into the Baltic Sea. Until the early 1960s, the connection to the mill flow in Doberan did not exist. Thus the footbridges including the Konventer See and its connection with the Baltic Sea, called Jemnitz , measured about 18 km, including the longest source brook even 21 km. Nowadays it is 300 meters more from the farthest spring over the Mühlenfließ to the mouth.
Lengths of the river sections, each up to their mouth:
- 3.51 km - unclassified source stream
- GWK 963812, peak waters
- 2.0 km - from the Konow - Wilsen bridge
- 1.05 km - from the confluence of the Quellbach
- GWK 9638, Stege - Stegekanal (lower Rotbach) - Mühlenfließ
- 16.2 km - from classified origin
- 13.9 km - from the confluence of the top water
- 8.6 km - at the junction of the old Stege lower course
- 8.3 km - GWK 96388, old lower course of the Stege - Conventer See - Jemnitz
natural reserve
The Waidbach is part of the Fahrenholzer Wald nature reserve . There is a high population of frog and tailed amphibians in its catchment area. Many endangered and endangered plant species as well as a valuable insect population are also at home here. The old lower course of the footbridges flows through the Conventer See nature reserve .
literature
- Topographic map 1: 100,000, edition 1999, sheets C 1934, C 1938 and C2338.
Web links
- Mecklenburg-Western Pomerania Geoportal
- Map portal environment of the State Office for the Environment, Nature Conservation and Geology Mecklenburg-Western Pomerania ( information ) with geodata
Individual evidence
- ↑ Mes table sheet No. 1837 Doberan from 1911 ( Memento of the original from May 11, 2013 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.
- ↑ GPS track based on aerial photo and open street map
