Uffe (Wieda)
Uffe Sachsengraben (in Thuringia) |
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Run the Uffe right through Bad Sachsa . |
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Data | ||
Water code | DE : 5648228 | |
location | Districts of Göttingen and Nordhausen ; Lower Saxony and Thuringia ( Germany ) | |
River system | Elbe | |
Drain over | Wieda → Zorge → Helme → Unstrut → Saale → Elbe → North Sea | |
source | in the Harz at the Großer Bockstalskopf 51 ° 37 '37 " N , 10 ° 32" 28 " E |
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Source height | approx. 580 m above sea level NHN | |
muzzle | behind Obersachswerfen in the Wieda coordinates: 51 ° 33 '14 " N , 10 ° 39' 21" E 51 ° 33 '14 " N , 10 ° 39' 21" E |
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Mouth height | approx. 236 m above sea level NHN | |
Height difference | approx. 344 m | |
Bottom slope | approx. 23 ‰ | |
length | approx. 15 km | |
The Uffe, known here in Branderode as the Sachsengraben. |
The Uffe , called Sachsengraben in Thuringia , is a western and orographically right tributary of the Wieda in the Harz in the Lower Saxony district of Göttingen and in the Thuringian district of Nordhausen .
course
The Uffe has its source in the southern Harz region of Lower Saxony in the Harz Nature Park . Its source is in the community-free Harz region of the Göttingen district at around 580 m above sea level. NHN on the southern slope of the Großer Bockstalskopf ( 630 m ), a secondary peak of the Ravensberg ( 659 m ). Near the source, the Uffe is fed by a trickle coming from a height of about 610 m .
Initially the Uffe flows south through the Harz Mountains. Then it runs southeast through the core town of Bad Sachsa . Below the village, to the west, it passes the Sachsenstein, a former coral reef of the Zechstein Sea . There, at the cut of the Northeim – Nordhausen railway line crossed by the Uffe, is the ruin of Sachsenstein Castle (Sachsenburg) .
The Uffe then reaches the village of Neuhof , which belongs to Bad Sachsa , from where the brook - from the transition from the Lower Saxon Harz Nature Park to the Thuringian Südharz Nature Park - flows further south-east as the Sachsengraben. It flows through the villages of Branderode and Obersachswerfen, which are part of the Hohenstein community . As a rule, the stream seeps into the gypsum karst there before it can reach the Wieda tributary of the Zorge at a height of around 236 m below Obersachswerfen
Klettenberger Mühlgraben
In the 17th century, the Klettenberger Mühlgraben branching off from the brook axis (Uffe-Sachsengraben) that branches off from the brook axis flowing to the Wieda was created below Neuhof by means of a weir built there . The weir used to branch off was near the former inner-German border , which is why it was abandoned in 1961 and the Mühlgraben was robbed of its function; there is a sewage treatment plant near the weir . It originally led over to the Uffe, which flows into the Ichte, and crossed the watershed of both rivers in a north-south direction. With the help of a water art, the mill ditch was used to supply Klettenberg and Klettenberg Castle , which are located in the southern Harz gypsum karst landscape, and to operate more than ten water mills . Almost nothing remains of the mill moat and the water art.
Water quality
In Thuringia, the Uffe (Sachsengraben ) is rated as "moderately polluted" ( water quality class II).
References and comments
- ↑ a b c d Map services of the Federal Agency for Nature Conservation ( information )
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↑ a b Memory of an almost forgotten medieval engineering achievement , from October 25, 2012, accessed on March 16, 2015, on walkenrieder-nachrichten.com
compare with:
Heimatkunde der Stadt Nordhausen, p. 24, E. Haacke's Buchhandlung, Nordhausen 1904:
A water flows into the Ichte from Klettenberg and Holbach, which branches off from the Uffe and the Sachsengraben at Branderode and Neuhof. This creates a fork in the Uffe, in which a part continues to flow to the Wieda and a part to the Ichte. - ↑ Water quality, flowing waters 2006 , on tlug-jena.de (PDF; 412.7 kB)
Web links
- Unknown sinkholes on the southern Harz , with information on gypsum karst and water shrinkage, on karstwanderweg.de