Schleifseebach

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Schleifseebach
upper course: Kochklingenbach
Old name: Roman brook
Data
Water code DE : 2386634
location Swabian-Franconian forest mountains

Baden-Württemberg

River system Rhine
Drain over Bühler  → Kocher  → Neckar  → Rhine  → North Sea
source west of Bühlerzell- Geifertshofen in Göbelsrain .
49 ° 0 ′ 35 "  N , 9 ° 51 ′ 50"  E
Source height approx.  488  m above sea level NHN
muzzle between Bühlerzell and Kottspiel from the left and west into the beginning of the central reaches of the Bühler coordinates: 49 ° 0 '36 "  N , 9 ° 54" 51 "  E 49 ° 0" 36 "  N , 9 ° 54" 51 "  E
Mouth height below  379.4  m above sea level NHN
Height difference approx. 108.6 m
Bottom slope approx. 28 ‰
length 1.8 km
only name run
approx. 3.9 km 
with Kochklingenbach and an unconsidered upper section
Catchment area 3.708 km²
Discharge
A Eo : 3.708 km²
at the mouth 		MQ
Mq
 		45 l / s
12.1 l / (s km²)
Right tributaries Reutenbach
Residents in the catchment area under 400

The Schleifseebach is a 3.2 km long brook in northeastern Baden-Württemberg that flows into the upper Bühler from the left between Bühlerzell and Bühlertann - Kottspiel . Its left upper course is the Kochklingenbach , its shorter right the Reutenbach .

Surname

The Schleifseebach was called the Roman Bach from the confluence of its source brooks in the 19th century .

geography

Kochklingenbach

The left main strand upper course Schleifseebach rises about 2.3 km west of the Bühlerzell suburb of Geifertshofen at about 488  m above sea level. NHN in Waldgewann White Lache . The source area lies on the plateau of the Limpurger Mountains . From here the stream runs through a wedge-shaped, moderately steep forest Klinge to east-southeast, where it reaches the edge of the forest after about one kilometer. It then flows in the middle of a 300 m wide meadow between the Göbelsrain in the north and the Kirschenrain in the south, both of which are wooded from the middle up on the slope. After about 2.2 km it reaches the outskirts of Geifertshofen, finally in an easterly direction, where it joins the Reutenbach at the junction of the residential street Sommerhalde from the village Bachstraße .

The Kochklingenbach is about 2.1 km long and has a partial catchment area of ​​about 1.1 km².

Reutenbach

The right tributary upper course of Reutenbach is created in the Waldgewann Geschläg in a Wiesental basin , the center of which is a little southwest of the Geifertshofener Reutenbachhof, from the confluence of several hillside forest streams that arise at the edge of the plateau surrounding the basin in a semicircle. South of the Reutenbachhof, the stream runs through its somewhat flatter, but otherwise very similar valley to that of the Kochklingenbach between Kirschenrain in the northwest and Denzelhalde through the Buchrain fields and then under the Buchhalde in a northeast direction to the confluence. It is 1.3 km long from its official source west of the Wurzelhof to the confluence . Its sub-catchment area also covers about 1.1 km².

Schleiferseebach lower course

The Schleifseebach runs through the village for the most part in an open bed, up to its center next to the Bachstrasse, from which it is spanned by a few footbridges and bridges for access to the property; in the center of the village it flows in a walled trough enclosed by a parapet. After leaving the village soft patch, the creek strives steadily to east-north-east on its remaining course of just under a kilometer. He pulls through a very wide valley basin, which partly shows steep slopes to a first level of terrain; Below are valley meadows, above them mostly fields on the left, while on the right side the slope continues to rise up to the plateau foothills around Bühlerzell-Imberg. The valley level of the Bühler is reached by the Schleifseebach, here bordering the community of Bühlertann for a short left , through a pierced lake dam. After a total of 1.8 km from the confluence and about 3.9 km from the source of the Kochklingenbach, it flows at just under 379.4  m above sea level. NHN , from the left across from the Bühlerzell sewage treatment plant in the Bühler moving north here .

Catchment area

The Schleifseebach has a catchment area of ​​3.7 km², which has the shape of a pointed wedge directed towards the mouth and slightly longer in the northwest. In terms of natural space , it is located in the lower Limpurg Mountains of the Swabian-Franconian Forest Mountains . In its western parts it covers part of the wide forest plateau of this landscape, which is at the highest point a little west of the Kochklingenbach spring in the White Lache up to about 501  m above sea level. NHN raises. Starting there at the Weißen Lache , the northern watershed runs eastwards along the Kammwaldweg on the Göbelsrain to the Weißenhof, there descends to the Kreuzfeld and then runs over the Rotäcker towards the estuary. Otherworldly competitors are the right tributaries of the lower Fischach from the hamlet of Bach to almost its mouth. From there the catchment area border rises again to the ridge between Schleifseebach and the Bühlerzeller Liegelbach , follows this roughly to the west to the southwestern Denzelhalde , behind which the Gunzenbach runs to the Bühler. Then it turns to the northwest and moves through Kugelwald and Grünes Hölzle back to the White Lache. The otherworldly drainage competitor is the longest last stretch of the Klingenbach .

There are shifts of the Mittelkeuper in the entire catchment area . At the western tip on the plateau a little above the Kochklingenbach spring there is a gusset of Upper Bunten Mergels ( Mainhardt Formation ) on the otherwise stepped silica sandstone ( Hassberge Formation ), which is to the left of the Kochklingenbach as Göbelsrain , between the two upper reaches as a shorter Kirchenrain and to the right of Reutenbach and underflow in the Kugelwert and over the Denzelhalde protrudes furthest to the east. Below it, a first band of Unterer Bunter Mergel ( Steigerwald Formation ) folds into the erosion bays, including an equally wide band of reed sandstone ( Stuttgart Formation ). Then the upper reaches and Schleifseebach flow to the mouth in the Gipskeuper ( Grabfeld Formation ), the longest stretch in its estheria layers, only below Geifertshofen in its deeper layers in a sometimes quite wide strip of floodplain sediment. The southwestern source stream of the Reutenbach has created a small sinter bank . On the Kirschenrain ridge between the two upper courses, a geological fault line has been identified, the deep clod of which lies against the Reutenbach.

The largest part of the catchment area is in the area of ​​the municipality of Bühlerzell, around 13 hectares of agricultural land to the left of the lowest course belong to Bühlertann. Only the village of Geifertshofen is traversed by the Schleifseebach. In the Obertal of the Reutenbach is the Reutenbachhof, on the northern edge of the catchment area on the Göbelsrain-Sporn the Weißenhof. There are two newer agricultural properties on the lower reaches.

See also

Individual evidence

LUBW

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

  1. ↑ a b Height according to the contour line image on the topographic map background layer .
  2. ↑ Height according to black lettering on the background layer topographic map .
  3. ↑ a b c d Length according to the waterway network layer ( AWGN ) .
  4. ↑ a b Length measured on the background layer topographic map .
  5. ↑ Catchment area according to the basic catchment area layer (AWGN)
  6. ↑ a b Catchment area measured on the background layer topographic map .

Other evidence

  1. ↑ a b Old name Römischer Bach such as
  2. ↑ Modeled values ​​according to the discharge BW water node MQ / MNQ
  3. ↑ In the description of the place on the community website , "about 350" are mentioned for Geifertshofen, without it being made clear whether two old farms (Weißenhof, Reutebachhof) and two Aussiedlerhöfe were included or not.
  4. ↑ 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)
  5. ↑ Hansjörg Dongus : Geographical land survey: The natural spatial units on sheet 171 Göppingen. Federal Institute for Regional Studies, Bad Godesberg 1961. →  Online map (PDF; 4.3 MB)
  6. ↑ Geology according to the layers for Geological Map 1: 50,000 on: Map server of the State Office for Geology, Raw Materials and Mining (LGRB) ( notes ). The geological map listed under → Literature offers a similar picture  .

literature

  • Topographic map 1: 25,000 Baden-Württemberg North, as a single sheet No. 6925 Obersontheim and - only for the catchment area - No. 7025 Sulzbach-Laufen
  • Geological map of Baden-Württemberg 1: 25,000, published by the State Geological Office 1982, sheet no. 6925 Obersontheim with explanatory booklet.

Web links