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Nesse (Hörsel)

The Nesse is a 54.5-kilometre-long (33.9 mi)[1] tributary of the Hörsel in the southern Thuringia. Strictly speaking, it represents a second, right main branch of the Hörsel, which brings about as much water to join the Hörsel as the Hörsel itself and drains an even larger catchment area.

Nesse
Location
CountryGermany
StateThuringia
Physical characteristics
Source 
 • elevation295 m (968 ft)
Mouth 
 • location
Hörsel
 • coordinates
50°58′48″N 10°20′24″E / 50.9799°N 10.3399°E / 50.9799; 10.3399
 • elevation
215 m (705 ft)
Basin features
ProgressionHörselWerraWeserNorth Sea

The Nesse is a typical lowland river with an average bed gradient of only about 1.5 ‰. According to the Thuringia Water Act it has the status of a first order watercourse and is therefore under the maintenance obligation of the Free State of Thuringia.

Origin edit

The Nesse was formed at the end of the last ice age, geologists assume that a dammed lake with meltwater forced the breakthrough to the west. Neighbouring rivers belong to the Elbe river basin, the watershed of both rivers runs over Alacher Höhe and Bienstädter Höhe.[2]

Course edit

 
The County of Thuringia around 1645 (after Blaeu, detail)

Source area and upper cours edit

The Nesse river is created by the confluence of several drainage and spring ditches at 295 m (968 ft) above about 7 km (4.3 mi) west of Erfurt in the district Alach, not far from Erfurt Airport, and then flows in a westerly direction through the north of the district of Gotha. In Nottleben, the Mollbach, its first bigger tributary flows from the right, further right tributaries of the upper course flowing further below come from the Fahnersche Höhe.

Lower course edit

At the former railway station of Wangenheim the Wilder Graben (Nesse), which is fed in particular by the Leinakanal, flows into the Nesse from Gotha or coming from the left. Here ends the upper course of the Nesse, which up to now has been classified as a water body of 2nd class according to § 3 of the Thuringian Water Act. Up to the estuary the Nesse is a watercourse of the 1st class. About 1 kilometre (0.62 mi) to the west of Wangenheim is the Talsperre Tüngeda/Wangenheim, which is fed by the Mittagswassergraben from the direction Tüngeda and drains about 2 km (1.2 mi) southeast into the Nesse. The Wangenheimer See existed in its place until the 18th century. This is the first inflow from the Hainich. At Sonneborn, 2.5 km (1.6 mi) further on, the Arzbach flows from the left, and another Hainich tributary flows another 4 km (2.5 mi) below at Friedrichswerth with the Bieberbach from the right.

Directly at the district border of the district of Gotha with the Wartburgkreis, the 380 m (420 yd) long Talbrücke Nessetal of the Bundesautobahn 4 spans the water since 2009. On the left side the river approaches the Hörselberge, from which, however, only very short streams come. Hydrogeological investigations confirmed an underground connection with the Hörsel valley. From Ettenhausen an der Nesse to Stockhausen the Hörsel water feeds a dozen strong karst springs.

In the Wartburgkreis the Nesse flows through the community Hörselberg-Hainich, where in Großenlupnitz the Böber flows from the right and reaches the area of the town Eisenach at Stockhausen. As the last tributary, the Trenkelbach flows into the Nesse at Petersberg.

Confluence edit

The river mouth you can see today, was created in the Middle Ages by the construction of the Köpping Graben. This originally served to regulate the water level of the Hörsel. The Köppinggraben is located between the Köppingbrücke (Weimarische Straße) and Heinrichstraße. After about 300 m (330 yd), the river meets a weir. Here the Nessemühlgraben branches off from the Hörsel and diverts about half of its water volume into the medieval mill area on the northern and western edge of Eisenach's old town. The original mouth of the Nesse can still be recognised on historical maps from the 18th century: it was located to the west of Eichhölzchen on what is now Tiefenbacher Allee. The site has been reshaped since the construction of the car factory.

Tributaries edit

The catchment area of the Nesse River, with 426.3 km2 (164.6 sq mi), comprises 54.4 % of the total catchment area of the Hörsel (784 km2 (303 sq mi)) and 139.5 % of the Hörse catchment area above the Nesse estuary (305.6 km2 (118.0 sq mi)) Thus, the Nesse brings about the same amount of water (3.14 m3/s (111 cu ft/s)) to unite with the Hörsel as the Hörsel itself (3.11 m3/s (110 cu ft/s)). All Nesse tributaries come from the Thuringian Basin and its marginal plates, while its receiving water Hörsel is largely fed by the montane Thuringian Forest.

Most of the tributaries of the Nesse are typical lowland streams with low gradient. Today, their courses are largely straightened and integrated into a system of drainage ditches. The stream lengths given below each refer approximately to the permanently water-bearing part. Since most of the courses are canalized and integrated into the drainage system up to the corresponding watershed, they temporarily carry water over a much longer length during high precipitation or snowmelt, but in dry seasons they are de facto sometimes much shorter than indicated.

The Leina Channel forms a connection from the Hörsel headwaters Leinaand the (upper) Apfelstädt from the system Gera/Unstrut/Saale/Elbe —to the subsystem of the Nesse. It was already built in the Middle Ages to supply the town Gotha with water from the Thuringian Forest, and to which the Nesse flows via the Wilder Graben. The catchment area of the Wilder Graben is with 104.6 km2 (40.4 sq mi) barely smaller than that of the Nesse above (131.4 km2 (50.7 sq mi)), in addition there is the proportionate catchment area of Leina (estimated by TLUG Jena to be 20.8 km2 (8.0 sq mi)[3]) and Apfelstädt. In purely mathematical terms, the length of the Nesse River over the upper Leina, Leinakanal and Wilden Graben is 63.5 km (39.5 mi).

Name


Direction Length
[km]

[1]
Catchment-
area
[km²]
[4][3]
Mouth
elevation
[m. ü. NN]
[5]
Location of
confluence
(*: bei)
DGKZ


[4][6]
Mollbach (Origin in Alacher See) right 7,0 14,0 285 Nottleben 4168-1?
Immer (with Talsperre Friemar) right 3,8 281 Friemar 4168-1?
Neußenbach right 4,3 7,6 278 oberh. Molschlebens 4168-1?
Attichbach right 3,7 276 unterh. Molschlebens 4168-1?
Eschenberger Bach right 3,5 275 4168-1?
Wingferborn right 5,7 274 Eschenbergen* 4168-1?
Lachgraben left 3,0 272 oberh. Bufleben-Pfullendorfs 4168-1?
Krautmaßengraben right 2,7 258 Wangenheim* 4168-1?
Wilder Graben (inc. Leinakanal)[7] left 17,1 104,6 258 Goldbach* 4168-2
Mittagswasser (with Talsperre Tüngeda) right 11,5 28,2 257 oberh. Sonneborn-Eberstädts 4168-3?
Arzbach left 3,5 14,8 256 Sonneborn 4168-4
Gliemen left 4,1 255 4168-5?
Brüheimer Bach right 2,9 254 4168-5?
Bieberbach right 8,6 47,5 252 Friedrichswerth 4168-6
Matergraben right 2,3 234 Wenigenlupnitz 4168-7?
Böber right 8,9 29,5 228 Großenlupnitz 4168-8
Holzbach right 1,9 225 Eisenach-Stockhausen 4168-9?

Ecology and energy production edit

Especially in the 1980s, the Nesse was affected by heavy pollution from the confluence of the Wilden Graben. Via the Wilden Graben, insufficiently treated wastewater from the catchment area of the Gotha sewage treatment plant was fed into the river. With the construction of a state-of-the-art sewage treatment plant in Gotha by 1993, the water quality could be decisively improved.[8]

Active hydropower plants are located on the River Nesse in the districts of Ettenhausen, Wenigenlupnitz and Großenlupnitz in the municipality of Hörselberg-Hainich and in Eisenach.

See also edit

References edit

  1. ^ a b Flusslängen nach Geopfaden (kmz, 150 kB)
  2. ^ Möller, Wolfgang (2004): The Nesse. Part 1 - From the source area to the Wilden Graben. In: Hörselbergbote, H. 56, p. 26-31.
  3. ^ a b Gewässerlängsschnitt Nesse[] (TLUG Jena) - PDF, 59 kB
  4. ^ a b Thüringer Landesanstalt für Umwelt (publ.): Regional and Waterbody Figures (Gebiets- und Gewässerkennzahlen) - directory and map. Jena 1998, 26 pages.
  5. ^ Map services of the Federal Agency for Nature Conservation
  6. ^ Zur besseren Sortierbarkeit sind hinter der 4168 (=Nesse) je Bindestriche eingefügt.
  7. ^ Länge über Ratsrinne/Flutgraben - über obere Leina und Leinakanal 47,7 km lang!
  8. ^ Thüringer Landesanstalt für Umwelt: The Nesse - Development of a watercourse, Jena 1993

nesse, hörsel, nesse, kilometre, long, tributary, hörsel, southern, thuringia, strictly, speaking, represents, second, right, main, branch, hörsel, which, brings, about, much, water, join, hörsel, hörsel, itself, drains, even, larger, catchment, area, nesseloc. The Nesse is a 54 5 kilometre long 33 9 mi 1 tributary of the Horsel in the southern Thuringia Strictly speaking it represents a second right main branch of the Horsel which brings about as much water to join the Horsel as the Horsel itself and drains an even larger catchment area NesseLocationCountryGermanyStateThuringiaPhysical characteristicsSource elevation295 m 968 ft Mouth locationHorsel coordinates50 58 48 N 10 20 24 E 50 9799 N 10 3399 E 50 9799 10 3399 elevation215 m 705 ft Basin featuresProgressionHorsel Werra Weser North Sea The Nesse is a typical lowland river with an average bed gradient of only about 1 5 According to the Thuringia Water Act it has the status of a first order watercourse and is therefore under the maintenance obligation of the Free State of Thuringia Contents 1 Origin 2 Course 2 1 Source area and upper cours 2 2 Lower course 2 3 Confluence 3 Tributaries 4 Ecology and energy production 5 See also 6 ReferencesOrigin editThe Nesse was formed at the end of the last ice age geologists assume that a dammed lake with meltwater forced the breakthrough to the west Neighbouring rivers belong to the Elbe river basin the watershed of both rivers runs over Alacher Hohe and Bienstadter Hohe 2 Course edit nbsp The County of Thuringia around 1645 after Blaeu detail Source area and upper cours edit The Nesse river is created by the confluence of several drainage and spring ditches at 295 m 968 ft above about 7 km 4 3 mi west of Erfurt in the district Alach not far from Erfurt Airport and then flows in a westerly direction through the north of the district of Gotha In Nottleben the Mollbach its first bigger tributary flows from the right further right tributaries of the upper course flowing further below come from the Fahnersche Hohe Lower course edit At the former railway station of Wangenheim the Wilder Graben Nesse which is fed in particular by the Leinakanal flows into the Nesse from Gotha or coming from the left Here ends the upper course of the Nesse which up to now has been classified as a water body of 2nd class according to 3 of the Thuringian Water Act Up to the estuary the Nesse is a watercourse of the 1st class About 1 kilometre 0 62 mi to the west of Wangenheim is the Talsperre Tungeda Wangenheim which is fed by the Mittagswassergraben from the direction Tungeda and drains about 2 km 1 2 mi southeast into the Nesse The Wangenheimer See existed in its place until the 18th century This is the first inflow from the Hainich At Sonneborn 2 5 km 1 6 mi further on the Arzbach flows from the left and another Hainich tributary flows another 4 km 2 5 mi below at Friedrichswerth with the Bieberbach from the right Directly at the district border of the district of Gotha with the Wartburgkreis the 380 m 420 yd long Talbrucke Nessetal of the Bundesautobahn 4 spans the water since 2009 On the left side the river approaches the Horselberge from which however only very short streams come Hydrogeological investigations confirmed an underground connection with the Horsel valley From Ettenhausen an der Nesse to Stockhausen the Horsel water feeds a dozen strong karst springs In the Wartburgkreis the Nesse flows through the community Horselberg Hainich where in Grossenlupnitz the Bober flows from the right and reaches the area of the town Eisenach at Stockhausen As the last tributary the Trenkelbach flows into the Nesse at Petersberg Confluence edit The river mouth you can see today was created in the Middle Ages by the construction of the Kopping Graben This originally served to regulate the water level of the Horsel The Koppinggraben is located between the Koppingbrucke Weimarische Strasse and Heinrichstrasse After about 300 m 330 yd the river meets a weir Here the Nessemuhlgraben branches off from the Horsel and diverts about half of its water volume into the medieval mill area on the northern and western edge of Eisenach s old town The original mouth of the Nesse can still be recognised on historical maps from the 18th century it was located to the west of Eichholzchen on what is now Tiefenbacher Allee The site has been reshaped since the construction of the car factory Tributaries editThe catchment area of the Nesse River with 426 3 km2 164 6 sq mi comprises 54 4 of the total catchment area of the Horsel 784 km2 303 sq mi and 139 5 of the Horse catchment area above the Nesse estuary 305 6 km2 118 0 sq mi Thus the Nesse brings about the same amount of water 3 14 m3 s 111 cu ft s to unite with the Horsel as the Horsel itself 3 11 m3 s 110 cu ft s All Nesse tributaries come from the Thuringian Basin and its marginal plates while its receiving water Horsel is largely fed by the montane Thuringian Forest Most of the tributaries of the Nesse are typical lowland streams with low gradient Today their courses are largely straightened and integrated into a system of drainage ditches The stream lengths given below each refer approximately to the permanently water bearing part Since most of the courses are canalized and integrated into the drainage system up to the corresponding watershed they temporarily carry water over a much longer length during high precipitation or snowmelt but in dry seasons they are de facto sometimes much shorter than indicated The Leina Channel forms a connection from the Horsel headwaters Leina and the upper Apfelstadt from the system Gera Unstrut Saale Elbe to the subsystem of the Nesse It was already built in the Middle Ages to supply the town Gotha with water from the Thuringian Forest and to which the Nesse flows via the Wilder Graben The catchment area of the Wilder Graben is with 104 6 km2 40 4 sq mi barely smaller than that of the Nesse above 131 4 km2 50 7 sq mi in addition there is the proportionate catchment area of Leina estimated by TLUG Jena to be 20 8 km2 8 0 sq mi 3 and Apfelstadt In purely mathematical terms the length of the Nesse River over the upper Leina Leinakanal and Wilden Graben is 63 5 km 39 5 mi Name Direction Length km 1 Catchment area km 4 3 Mouthelevation m u NN 5 Location ofconfluence bei DGKZ 4 6 Mollbach Origin in Alacher See right 7 0 14 0 285 Nottleben 4168 1 Immer with Talsperre Friemar right 3 8 281 Friemar 4168 1 Neussenbach right 4 3 7 6 278 oberh Molschlebens 4168 1 Attichbach right 3 7 276 unterh Molschlebens 4168 1 Eschenberger Bach right 3 5 275 4168 1 Wingferborn right 5 7 274 Eschenbergen 4168 1 Lachgraben left 3 0 272 oberh Bufleben Pfullendorfs 4168 1 Krautmassengraben right 2 7 258 Wangenheim 4168 1 Wilder Graben inc Leinakanal 7 left 17 1 104 6 258 Goldbach 4168 2 Mittagswasser with Talsperre Tungeda right 11 5 28 2 257 oberh Sonneborn Eberstadts 4168 3 Arzbach left 3 5 14 8 256 Sonneborn 4168 4 Gliemen left 4 1 255 4168 5 Bruheimer Bach right 2 9 254 4168 5 Bieberbach right 8 6 47 5 252 Friedrichswerth 4168 6 Matergraben right 2 3 234 Wenigenlupnitz 4168 7 Bober right 8 9 29 5 228 Grossenlupnitz 4168 8 Holzbach right 1 9 225 Eisenach Stockhausen 4168 9 Ecology and energy production editEspecially in the 1980s the Nesse was affected by heavy pollution from the confluence of the Wilden Graben Via the Wilden Graben insufficiently treated wastewater from the catchment area of the Gotha sewage treatment plant was fed into the river With the construction of a state of the art sewage treatment plant in Gotha by 1993 the water quality could be decisively improved 8 Active hydropower plants are located on the River Nesse in the districts of Ettenhausen Wenigenlupnitz and Grossenlupnitz in the municipality of Horselberg Hainich and in Eisenach See also editList of rivers of ThuringiaReferences edit a b Flusslangen nach Geopfaden kmz 150 kB Moller Wolfgang 2004 The Nesse Part 1 From the source area to the Wilden Graben In Horselbergbote H 56 p 26 31 a b Gewasserlangsschnitt Nesse dead link TLUG Jena PDF 59 kB a b Thuringer Landesanstalt fur Umwelt publ Regional and Waterbody Figures Gebiets und Gewasserkennzahlen directory and map Jena 1998 26 pages Map services of the Federal Agency for Nature Conservation Zur besseren Sortierbarkeit sind hinter der 4168 Nesse je Bindestriche eingefugt Lange uber Ratsrinne Flutgraben uber obere Leina und Leinakanal 47 7 km lang Thuringer Landesanstalt fur Umwelt The Nesse Development of a watercourse Jena 1993 Retrieved from https en wikipedia org w index php title Nesse Horsel amp oldid 1052553420, wikipedia, wiki, book, books, library,

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