Jordanbach
Jordanbach | ||
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Data | ||
location | City of Walsrode , Heidekreis district , Lower Saxony | |
River system | Weser | |
Drain over | Böhme → Aller → Weser → North Sea | |
source | in Vehmsmoor 52 ° 51 ′ 3 ″ N , 9 ° 29 ′ 47 ″ E |
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Source height | 63 m above sea level NN | |
muzzle | southwest of Altenboitzen in the Bohemia Coordinates: 52 ° 48 ′ 7 " N , 9 ° 29 ′ 51" E 52 ° 48 ′ 7 " N , 9 ° 29 ′ 51" E |
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Mouth height | 22 m above sea level NN | |
Height difference | 41 m | |
Bottom slope | 5.3 ‰ | |
length | 7.7 km | |
Catchment area | 15.6 km² | |
Discharge at the mouth of the A Eo : 15.6 km² |
MQ Mq |
120 l / s 7.7 l / (s km²) |
The Jordanbach is a right tributary of the Böhme (southwestern Lüneburg Heath ). It flows exclusively in the area of the Lower Saxon city of Walsrode in the Heidekreis district .
The headwaters of the seven-kilometer-long stream lies in the Vehmsmoor , the western half of which it drains. The moor lies on a gently undulating plateau of the Walsroder loam geest, which is known as the natural area . It breaks little south suddenly and up to 40 meters deep the Aller glacial valley from. The Jordanbach flowing in a southerly direction cuts noticeably into this edge of the Geest plateau and then emerges at Altenboitzen into the grassland-shaped valley floodplain of the Böhme. It then follows the foot of the slope to the southwest and finally flows into the Böhme, which also flows southwest to the Aller .
The Jordanbach is the namesake for a railway line between Bomlitz and Altenboitzen, which today only serves tourist purposes and on which the Arbeitsgemeinschaft Verkehrsfreunde Lüneburg e. V. carries out individual special trips with the Heideexpress . From a section of the railway line Verden -Walsrode of Verden Walsroder railway (since 1910) and the Bomlitz-Walsrode railway (since 1915) existing connection is occasionally Jordan Bomlitz train called because it from the valley of the Jordan creek into Bomlitztal leads.
swell
- ↑ a b Measurement in TK 25
- ↑ The drainage of the catchment area is derived from the similarly structured adjacent intermediate catchment area of the Brock and Hollige an der Böhme gauges and Westerharl an der Bomlitz (7.7 l / s km²)