Nesselbach (Bühler)

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Nesselbach
outdated: Nestelbach, Eschelbach
View from the left bank of the Bühler over the river to the Nesselbach flowing from the east.

View from the left bank of the Bühler over the river to the Nesselbach flowing from the east.

Data
Water code DE : 2386654
location Swabian-Franconian forest mountains

Hohenloher and Haller level


Baden-Württemberg

River system Rhine
Drain over Bühler  → Kocher  → Neckar  → Rhine  → North Sea
source in the Hahnenbergwald about 1 km northeast of Markertshofen
49 ° 4 ′ 36 ″  N , 9 ° 57 ′ 3 ″  E
Source height approx.  490  m above sea level NHN
muzzle between Bühlertann and Obersontheim in the Bühler coordinates: 49 ° 3 ′ 1 ″  N , 9 ° 54 ′ 19 ″  E 49 ° 3 ′ 1 ″  N , 9 ° 54 ′ 19 ″  E
Mouth height approx.  368.1  m above sea level NHN
Height difference approx. 121.9 m
Bottom slope approx. 20 ‰
length 6 km
Catchment area 12.471 km²
Discharge
A Eo : 12.471 km²
at the mouth
MQ
Mq
148 l / s
11.9 l / (s km²)
Flowing lakes Schenkenseen (from the Schenkenbach tributary )

The Nesselbach is a creek in north-eastern Baden-Württemberg about six kilometers long, which flows into the middle Bühler from the right between Bühlertann and Obersontheim . Its left upper course is almost the same length as the Schenkenbach .

geography

Source and history

The Nesselbach rises in the eastern part of the Hahnenberg forest area , around 1 km northeast of Markertshofen and around the same distance west of Brunzenberg, both hamlets of the Frankenhardt community . For its first nearly kilometer, the stream flows in a steadily deepening forest gorge in a south-south-west direction to a valley spider, from where it runs permanently in the open. Here it takes up some sloping streams from the Hahnenberg , which curves around the valley spider to the north, and turns south. After a long half a kilometer, it reaches the middle of the hamlet of Markertshofen, where the L 1066 crosses it in another valley spider.

The mouth of the Schenkenbach is from the right in the picture

A kilometer further to the south it is reached from the left by its almost equally long Schenkenbach tributary , which arises between the Birkhof and Vorderuhlberg (both also to Frankenhardt) and joins in a westerly direction. The combined stream then continues in a west-southwest direction and already a quarter of a kilometer down the valley from the left takes on the Milan stream .

The floodplain of the Milan stream

This rushes in a west-north-westerly direction through a narrow valley from the outskirts of Frankenhardt- Hinteruhlberg . After the mountain forest areas of Dörnich in the south and Ebersberg in the north have narrowed the Nesselbachaue briefly to a width of only about 300 m, the forest to the right of the brook then recedes about 1.5 km from the brook, on the left a little over 0.5 km to the foot of the slope Buchenschnabs ,

Wetland on the brook from the upper Lindich

From here, a series of shorter bodies of water flow one after the other from the Lindich corridor in front of this corridor . Meanwhile , the Birkelbach , its 2.8 km longest tributary, reaches it from the right opposite , in the area of ​​the damp Schwarze Lache lowland . In a wide basin and in a straightened course since at least the inflow of the Schenkenbach , it now runs between a Aussiedlerhof standing on its flat valley slope first to the right and then to the left and then reaches the dirt road bridge of the Tiefen Weg , from where its character changes completely. This is where a section with small, winding meadow meanders begins. And so far it has only been accompanied by very young and low bushes on the straightened section on the bank, old alders now line its bank, the rhizomes of which visibly cause its winding course. From about two hundred meters before the mouth it runs as a natural dam river on the right a little above the deepest of the trough, through which the water leaving the stream bed rushes over a shorter route to the Bühler when it is high . Opposite a reforested impact slope, it finally flows into the Bühler from the right and almost vertically about 6.0 km below its source.

Catchment area

The Nesselbach has a catchment area of ​​12.5 km². It has roughly the shape of a triangle, the longest side of which connects its mouth at the southwest corner with the southeast corner near a district road triangle near Vorderuhlberg. The third corner lies in the north in the area of ​​the plateau of the Geschäufelte Marsh near the Frankenhardt village of Spaichbühl.

On its northeast side between Spaichbühl in the north and Vorderuhlberg in the southeast borders the catchment area of ​​the Speltach and its tributaries, on a small section afterwards on the plateau between Vorder- and Hinteruhlberg in the south the Blinde Rot competes , everywhere else the Bühler tributaries or the drainage beyond the watershed Bühler itself. Just west of the plateau near Hinteruhlberg, the border runs for a long time to the catchment area of ​​the Bühlertanner Bühler tributary Dammbach on the northern edge of a ridge that stretches from the Vetterhöfen to Bühlertann, and then bends before its western drop to the mouth. From there, the border climbs northeast up the Bühlerhang, then leads east around the opencast mine on the former Obersontheimer Heerberg and then follows the Birkelbach uphill to the west at a distance of less than 0.3 km . In this section, beyond the watershed, the short waters of Speckbach and then Hambach zur Bühler drain . On the remainder of the border, which closes after crossing the Hahnenberg plateau on the Geschäufelte Marsh , the precipitation flows beyond the watershed in the northwest via its tributary Lanzenbach to the Bühler.

Tributaries and lakes

List of tributaries and RiverIcon-SmallLake.svglakes from source to mouth.

Origin of the Nesselbach at about 490  m above sea level. NHN approx. 1 km northeast of the Markertshofen town center, at the transition from the Hahnenbergwald to the Kammerforst to the east.

  • (Northern source arm), from the right, approx. 0.2 km. About the same length as the official upper reaches.
  • (Northern tributary), from the right a little east of the field boundary, approx. 0.4 km. From a blade east of the forest hut with winter fodder meadow on the Hahnenberg .
  • Hahnenbach , from the right to 423  m above sea level. NHN in the Talspinne north of Markertshofen, 0.8 km. It rises a little north-northeast of the Hahnenberg-Forsthütte in an overman-high clay gully and runs through a small blade pond on the upper slope. There used to be a spring pipe on the slope of the clay channel where the foresters used to gather drinking water.
    • (Meadow channel), from the left just before the mouth, approx. 0.1 km.
  • Häfnerbach , a few steps from the right after the Hahnenbach, 0.8 km. Arises in the west on the southeast slope of the Hahnenberg.
  • (Western tributary from the edge of the southern Häfnersteige ), from the right in northern Markertshofen, approx. 0.7 km. Verdolt in the local area.
  • Gemeindebach , from the left near the center of Markertshofen, 1.7 km. Arises on the northwestern edge of a forest meadow on the road to Frankenhardt -Gründelhardt. Flows in the beginning forest west of the meadow through a pierced lake dam, feeds fish ponds halfway after exiting the forest, in the local area Verdolt.
    • (Northern source branch), from the right, approx. 0.2 km. Arises near the forest path between the forest meadow and the chamber forest .
    • (Inflow), from the left probably shortly before the mouth, approx. 0.7 km. Arises in the Klinge east of Markertshofen, through which the valley trail of the L 1066 runs from Gründelhardt into the hamlet, near an old sand reed quarry in the Mörder forest, which is not very upward . Flows in the blade, in which fillings can be seen, partly underground. Verdolt in Markertshofen.
Renatured meadow course of the Schenkenbach in front of its mouth
  • Schenkenbach, from the left just before the Markertshofener sewage treatment plant, 2.7 km. Origin west of the path of the K 2637 from Birkhof to Vorderuhlberg up on the western slope of the valley level around the Birkhof. Runs through the wooded, partly steep Killerblade and in it the two remaining Schenkensen .
    • (Klingenbach from Höllberg ), from the left in the Mörderklinge , approx. 0.2 km.
At the rear Schenkensee lies the
Burgstall near the Schenkenseen on a peninsula
    • RiverIcon-SmallLake.svgRuns through the rear Schenkensee , 0.5 ha, at the Burgstall near the Schenkenseen .
    • Runs through the pierced dam of what was once a middle Schenkensee.
    • RiverIcon-SmallLake.svgShortly before the forest emerges, runs through the front Schenkensee , 0.2 ha.
    • (Inflow), from the left at the outflow of the front Schenkensee, approx. 0.5 km. From a blade on the Schmiedsberg slope northwest of Hinteruhlberg .
  • Milanobach , from the left shortly after the Markertshofener sewage treatment plant, 1.7 km. Origin in a soon steep blade that begins near the village chapel of Hinteruhlberg; In the lower part of the blade, the Bühlertann -Vetterhöfe-Markertshofen forest path runs along the edge of a long and narrow meadow tongue .
  • (Wiesenbach), from the left opposite the Ebersberg , approx. 1.0 km. Arises at the single farm Himmelreich on the slope under the Vetterhöfe.
  • (Bach from Upper Lindich ), from the left, approx. 0.5 km.
  • (Another stream from the Upper Lindich ), from the left, approx. 0.4 km.
  • Birkelbach , from the right to 384.6  m above sea level. NHN on the Black Lache , 2.8 km. Arises near a remnant of Wellingtonia on a right branch of the Höhenwaldweg through Gewann Häfnersteige , which runs west to the valley next to its soon-to-be steep blade. The stream and path then turn abruptly in a south-easterly direction after less than a kilometer.
  • Bräunlinsbach , from the right to 379.2  m above sea level. NHN a little southeast of an Obersontheimer Ausiedlerhof, approx. 0.7 km. Arises in the damp meadows of the Obersontheim district of Bräunlinshausen next to the L 1066 and passes a small fountain for hikers at the Aussiedlerhof.
The Buchenschnäue wetland is located in a gypsum keuper basin
  • (Stream east of Neuhof ), from the left a little northeast of Neuhof, approx. 0.5 km. Drains u. a. the superficially drainless Buchenschnäue wetland at the foot of the Buchenschnab forest (common name on the map, Buchenschnäue on the map ), a herbaceous little hollow in a gypsum keuper depression that is under protection.
  • (Wiesenrinne), from the left a little below the Nesselbach bridge of the Tiefen Weg from Neuhof to Obersontheim, approx. 0.3 km long. Arises near the western edge of the Buchenschnab forest at the northwestern foot of the Bühlertanner vineyard as a continuation of a mostly dry clay gutter at the upper bend in the slope and a meadow hollow below.
  • (Drainage ditch at the foot of the Grübig ), from the right shortly before the mouth of the Nesselbach to Parallellauf, approx. 0.2 km.

Mouth of the Nesselbach at a little below 368.1  m above sea level. NHN from the right and finally east between their valley villages Bühlertann and Obersontheim into the Bühler . The Nesselbach is 6.0 km long, has a mean bed gradient of about 20 ‰ and a catchment area of ​​12.5 km².

Localities

The hamlet of Markertshofen is the only village on the banks of the Nesselbach or one of its tributaries. The also Frankenhardt village Hinteruhlberg is in the south just in the catchment area, apart from these, its settlement is limited to the Bühlertanner single house Himmelreich and two Obersontheimer Aussiedlerhöfe. Most of the creek and the catchment area lie in the territory of the Frankenhardt community, a smaller part belongs to Obersontheim, the border runs in the north on or on the ridge that separates the upper Nesselbach and Birkelbachtal, and in the south along the eastern one upper slope edge of the Milanobach valley. A significantly smaller part of the catchment area belongs to Bühlertann, it lies on the southern edge and extends for less than a kilometer in front of the mouth from the left to the lower reaches.

geology

Old reed sand quarry in the Mörderklinge (upper Schenkenbach)
The plowed plain to the west above Markertshofen lies on the Corbula bank of the Gipskeupers, the sagging layer on the eastern edge breaks off at a terrace

The course of the Nesselbach lies entirely in the Keuper . It rises at the border between the Upper Bunter Mergeln and the Kieselsandstein and runs through the forest ravine in quick succession through Kieselsandstein, Untere Bunte Mergel and reed sandstone , in order to reach the Gipskeuper in the valley spider north of Markertshofen , in which it runs as far as the mouth of the Birkelbach remains at the Schwarzer Lache, the remaining stretch to the mouth belongs to the Unterkeuper . The larger tributaries Schenkenbach and Birkelbach arise on slopes in the Untere Bunter Mergeln, the community stream in the reed sandstone, the tributaries of the lower reaches mostly in the Gipskeuper.

The upper reaches of the Nesselbach and Birkelbach follow the extensive tectonic basin line of the east-north-east oriented Neckar-Jagst furrow , the isolated occurrence of the Upper Bunter Merkel at the Nesselbach spring is also explained by this tectonic low elevation; Apart from this, the highest layer in the catchment area is the silica sandstone. The middle to lower Birkelbach runs roughly on the line of the south-east moving Vellberger Fault.

South of the Vorderen Schenkensee there are two sinkholes next to each other in Gipskeuper, one of which was recently (as of 2010) filled in by excavation from the lake.

In the catchment area, gypsum mining took place in some places, to the greatest extent on the Heerberg, over the ridge of which the watershed ran about one kilometer northeast of and parallel to the lower reaches. In the meantime, the mountain has been cleared and the opencast mine on base gypsum has almost been discontinued, the remaining pit now serves primarily as a landfill. To the east of Markertshofen, there were quarries in the reed sandstone that had long ceased to exist. On the little forest road that leads through the murderer blade, there is a small abandoned reed sand quarry in which resedimentation breccia is exposed.

Landscape image

Below their source blades, which are mostly located in the hillside forest, the Nesselbach and its larger tributaries flow in wide, flat, often moist hollows in open fields in which the grassland dominates. The fields are often on higher terraces above the valley basins. To the east of Markertshofen are the reed sandstone plateaus of Helmesberg and Krautäcker unterm Pflug, to the west on the ridge that separates the upper Nesselbach valley from the Birkelbachtal, the level is built, a leveled area on the Corbula bank of the Gipskeuper. In the Obersontheim district, where the layers above the Gipskeuper are rare and even the upper Gipskeuper has mostly been cleared, the small platform-like high elevation of the Lindich between the stream and the slope forest of the Buchenschnabs is striking .

Below the mouth of the Birkelbach, a trough around the course of the Nesselbach forms more clearly, which becomes a little narrower below the bridge of the Tiefen Weg .

Sights and buildings

In the south of the rear Schenkensee there is a Wurst-like peninsula, separated from the foot of the slope by a now dry ditch. It used to be a hunting lodge, today a wooden forest hut.

See also

Individual evidence

LUBW

Official online waterway map with a suitable section and the layers used here: Course and catchment area of ​​the Nesselbach
General introduction without default settings and layers: State Institute for the Environment Baden-Württemberg (LUBW) ( notes )

  1. Height according to the contour line image on the topographic map background layer .
  2. a b Height according to black lettering on the background layer topographic map .
  3. Length according to the waterway network layer ( AWGN ) .
  4. a b Catchment area summed up from the sub-catchment areas according to the basic catchment area layer (AWGN) .
  5. Geotopes according to the relevant layer.

Other evidence

  1. Wolf-Dieter Sick : Geographical land survey: The natural space units on sheet 162 Rothenburg o. D. Deaf. Federal Institute for Regional Studies, Bad Godesberg 1962. →  Online map (PDF; 4.7 MB)
  2. Modeled values ​​according to the discharge BW water node MQ / MNQ
  3. The TK25 also names him Eschelbach in brackets , an old information provider in the nearby village also mentioned the name Nestelbach (in dialect [ ˈnɛʃdl̩ˌbax ]), also mentioned in the description of the Oberamt Ellwangen from 1886; however, both forms of name no longer seem to be alive.
  4. The TK25 calls this forest marking Buchenschnäue , a shape that is completely uncommon in the area.
  5. Leads from Obersontheimer Hirtensteige to Neuhof and then to Lindich .
  6. Sometimes you can also read the form of the name Molder blade .
  7. ^ Name of a desert
  8. ↑ Found in nature, but not in any of the sources.
  9. Geology according to the geological map listed under →  Literature . A rough overview also provides: Mapserver of the State Office for Geology, Raw Materials and Mining (LGRB) ( notes )

literature

  • Topographic map 1: 25,000 Baden-Württemberg, as single sheet No. 6925 Obersontheim
  • Geological map of Baden-Württemberg 1: 25,000, published by the State Geological Office 1982, sheet no. 6925 Obersontheim with explanatory booklet

Web links

Geoportal Baden-Württemberg ( information ), especially with the partial maps / layers