Sulz (Altmuehl)
Sulz | ||
The Sulz spring on the Tyrolsberg |
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Data | ||
Water code | DE : 13862, DE : 13854 | |
location |
Bavaria
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|
River system | Danube | |
Drain over | Altmühl → Danube → Black Sea | |
source | northwest of Berngau 49 ° 15 ′ 57 ″ N , 11 ° 22 ′ 40 ″ E |
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Source height | approx. 445 m | |
muzzle | in Beilngries from the left into the Altmühl coordinates: 49 ° 1 '40 " N , 11 ° 28' 53" E 49 ° 1 '40 " N , 11 ° 28' 53" E |
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Mouth height | 363 m | |
Height difference | approx. 82 m | |
Bottom slope | approx. 2.7 ‰ | |
length | 30.6 km |
The Sulz is a left tributary of the Altmühl mainly in the district of Neumarkt in the Upper Palatinate in Bavaria , which flows from the left into the lower course of the town of Beilngries in the neighboring district of Eichstätt . The predominantly southern to southeastern course of the approximately 30 km Sulz River was interrupted several times by the construction of the Main-Danube Canal on the lower course, which uses its valley channel .
geography
course
The Sulz rises officially Sulzquelle to about 517 m above sea level. NHN a little north of the settlement boundary of the village of Tyrolsberg in the municipality of Berngau in the forest on the Tyrolsberg. It then has an open run less than 200 meters long, after which it disappears underground at the roadside in Tyrolsberg.
Only almost one and a half kilometers southwest of it is there another open run in the so-called Kindlesgraben , which is about 445 m above sea level. NHN sets in, here the Sulz continues to feed a chain of ponds in a southerly direction and then moves west past the main town of Berngau. It passes two districts of the municipality and then changes to the area of the city of Freystadt , where the village of Sondersfeld is on the left side of the river.
It turns to the southeast in the area of the municipality Mühlhausen , some of which are located on the waterfront. In between, the municipality of Sengenthal borders here , of which only the Braunmühle is located in a certain river proximity. There the Wiefelsbach flows from the left and north, its largest natural tributary, and it now turns consistently to the south in its direction and digs an ever deeper Jura valley.
Then it flows through Mühlhausen itself and changes over to the area of the town of Berching , where the Main-Danube Canal swings into the valley a little below the Pollanten district and now accompanies Sulz to the right. Still in her own bed, she crosses Berching itself and then flows a little below the town limits and the Berching lock of the canal towards it.
After its crossing into the area of the town of Beilngries , which is located in the district of Eichstätt , there is first to the right of the canal, then to the left of it both times under two kilometers long, strongly meandering residual water that drains it off. Shortly before Beilngries itself, where the canal bends to the east, the Sulz is diverted southward from it. It flows for about three kilometers on a south-easterly path through the settlement area of the central city, passes the old town center on the right and then flows out at about 363 m above sea level. NHN from the left into the lower Altmühl .
The mountain and town of Sulzbürg derive their name from the small, leisurely flowing body of water.
The once meandering Sulz operated many mills, of which the Gösselthalmühle in Gösselthal is reminiscent of the relevant place names listed in the → Places section .
Near the so-called lock 25 there is an introduction of the Sulz into the historic Ludwig-Danube-Main Canal , the smaller forerunner of today's Main-Danube Canal , which also ran in the Jura valley of the Sulz and of which several sections have been preserved. Such structures were built to compensate for water loss through sluice, seepage and evaporation. If necessary, part of the water was diverted into the canal. In addition to other discharges, the Sulz serves to supply a six-kilometer-long vertex post . At the head of the lock 25 there is a compulsory relief that drains over the Entenbach into the Sulz during high water.
Tributaries
From the source to the mouth. Selection.
- Frauengraben , from the right to Berngau-Mittelricht
- Wiefelsbach , from the left n before Mühlhausen-Belzlmühle
- Entenbach , from the left across from southern Mühlhausen
- Gänsgraben , from the left at Berching-Grubmühle
(Start of the running gap)
- Trout stream , from the right at Beilngries-Biberbach into a residual water on the right of the Main-Danube Canal
- (Residual water to the left of the Main-Danube Canal), near Beilngries-Gösselthal
(End of the running gap)
- (Hangbach), from the right in Beilngries in front of the sports boat harbor on the Main-Danube Canal
- (Hangbach), from the right in Beilngries to the sports boat harbor on the Main-Danube Canal
- Wertbach , from the left in Beilngries
places
Places on the Sulz from the source to the mouth with the district and community affiliations. Only the entries with the lowest nesting level are resident.
District of Neumarkt in the Upper Palatinate
- community Berngau
- Allershofen (hamlet, left)
- Mittelricht (Kirchdorf, some distance to the right)
- City of Freystadt
- Sondersfeld (parish village, some distance to the left)
- community Muehlhausen
- Wettenhofen (village, right)
- Rocksdorf (Kirchdorf, mostly on the right)
- Community Sengenthal
- Braunmühle (hamlet, some distance to the left)
- Mühlhausen community
- Belzlmühle (wasteland, right)
- Ellmannsdorf (hamlet, right)
- Aumühle (wasteland)
- Sand mill (wasteland, right)
- Mühlhausen (parish village)
- Reismühle (wasteland, enclave of Berching, right)
- City of Berching
- Pollanten (parish village, left at the foot of the slope beyond the Ludwig-Danube-Main Canal)
- Breitenfurt (wasteland, left)
- Rapperdorf (village, left at the foot of the slope beyond the Ludwig-Donau-Main Canal)
- Grubmühle (wasteland, right)
- Sollngriesbach (Kirchdorf, right at the foot of the slope beyond the Main-Danube Canal)
- Berching (main town)
start of the running gap - Eglasmühle (village, in the area of the running gap mainly to the right of the former course and today's Main-Danube Canal)
- Plankstetten (parish village, in the area of the passage mainly to the right of the former course and today's Main-Danube Canal)
- City of Beilngries
- Biberbach (Kirchdorf, to the right of a residual Sulz watercourse to the right of the Main-Danube Canal at the foot of the slope)
-
Gösselthal (hamlet, on a residual Sulz water body to the left of the Main-Danube Canal, predominantly on the left at the foot of the slope)
end of the running gap - Beilngries (main town)
See also
literature
- Johann Kaspar Bundschuh : Sulz . In: Geographical Statistical-Topographical Lexicon of Franconia . tape 5 : S-U . Verlag der Stettinische Buchhandlung, Ulm 1802, DNB 790364328 , OCLC 833753112 , Sp. 490 ( digitized version ).
- ↑ Location lock 25 and hydraulic structures in the BayernAtlas (accessed on March 8, 2019)
Web links
- Upper course of the Sulz on the BayernAtlas.