Rodenberger Aue
Rodenberger Aue Aue |
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Rodenberger Aue in Rodenberg |
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Data | ||
Water code | DE : 48884 | |
location | In the Schaumburg and Hameln-Pyrmont districts and the Hanover region | |
River system | Weser | |
Drain over | Westaue → Leine → Aller → Weser → North Sea | |
source | Near Kessiehausen am Süntel | |
Source height | approx. 190 m above sea level NN | |
muzzle | At Auhagen in the Westaue coordinates: 52 ° 24 '22 " N , 9 ° 19' 22" E 52 ° 24 '22 " N , 9 ° 19' 22" E |
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Mouth height | 49 m above sea level NN | |
Height difference | approx. 140 m | |
Bottom slope | approx. 5 ‰ | |
length | 28 km | |
Catchment area | 170 km² | |
Left tributaries | Pohler Bach, Riesbach, Salzbach | |
Right tributaries | Eimbeckhäuser Bach |
The Rodenberger Aue is the 28 km long right tributary of the Westaue in Lower Saxony , in the districts of Hameln-Pyrmont , Schaumburg and the Hanover region , the border of which it forms in the lower reaches. It flows through the Deister-Süntel valley and the bordering landscape of the Bückeberg foreland below Rodenberg .
course
The Rodenberger Aue rises as a meadow near Kessiehausen, above Bakede am Süntel , approx. 190 m above sea level. NN . It drains the eastern Süntel, the western Deister and the northeastern part of the Bückeberg , a total of 170 square kilometers. In its course it absorbs the water of numerous low mountain streams, is dammed by weirs in Rodenberg , Horsten and Rehren , crosses the BAB 2 behind Lauenau , the B 65 near Bad Nenndorf , the Hanover – Minden railway line and the Mittelland Canal before Auhagen .
Between the Mittelland Canal and its mouth, the Rodenberger Aue has been extensively renatured since 1990 , as it is part of the Lower Saxony river protection system as one of the representatives of a typical Bördebach. Characteristic here are steep bank breaks, which can result in a breeding habitat for the kingfisher .
At Sachsenhagen -Auhagen it joins the Sachsenhäger Aue to form the Westaue , which soon afterwards flows into the Leine at Wunstorf -Liethe .
The floodplain, which is rarely more than 2 meters wide, flows through the Deister-Süntel valley from southeast to northwest and thus follows one of the pre-glacial courses of the Weser , which today bends west in front of this valley.
In earlier times the floodplain was used to operate a few mills. Today it is occasionally used to train canoeists .
Bigger places on the river
Tributaries
The floodplain takes in numerous low mountain streams from Deister, Süntel and Bückeberg:
- Flöttenbach (Deister)
- Eimbeckhäuser Dorfbach (Deister)
- Walterbach or Waltershagener Bach (Deister)
- Hülseder Bach (Süntel)
- Meinser Bach (Süntel)
- Riesbach (Bückeberg)
- Pohler Bach (Süntel)
- Altenhäger Bach (Deister)
- Blumenhäger Bach (Deister)
- Schlierbach (Deister)
- Salzbach (Bückeberg)
- Ackersbeeke (Deister)
- Rodebach (Deister)
- Rieper Flahbach (Bückeberg)