Herboldshauser Bach

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Herboldshauser Bach
Herboldshauser Bach
Data
Water code DE : 238819142
location Hohenloher and Haller level

Kocher-Jagst Plains

Baden-Württemberg

River system Rhine
Drain over Jagst  → Neckar  → Rhine  → North Sea
source in a forest island about 0.9 km south-southwest of the Kirchberg hamlet Herboldshausen
49 ° 10 ′ 15 ″  N , 9 ° 58 ′ 31 ″  E
Source height below  424  m above sea level NHN
muzzle at the Lobenhauser Mühle in the Mühlkanal to the left of the central Jagst coordinates: 49 ° 11 '18 "  N , 10 ° 0' 21"  E 49 ° 11 '18 "  N , 10 ° 0' 21"  E
Mouth height approx.  355  m above sea level NHN
Height difference approx. 69 m
Bottom slope approx. 18 ‰
length 3.8 km
Catchment area 4.607 km²

The Herboldshauser Bach is a brook in northeastern Baden-Württemberg in the district of Schwäbisch Hall , which lies in the area of ​​the small town of Kirchberg an der Jagst and on its edge. It is not quite 4 km long, flows a little northeast and flows from the left into the Mühlkanal next to the central Jagst at the Lobenhauser Mühle of the town, which belongs to the hamlet of Lobenhausen .

geography

course

The Herboldshauser Bach arises at almost 424  m above sea level. NHN in a forest island less than half a square kilometer on the city limits from Crailsheim to Kirchberg an der Jagst near the forest-crossing route of the K 2500 from Crailsheim's hamlet Saurach in the south to Kirchberg's hamlet Herboldshausen in the north. On the first third of its course the brook runs approximately northwards, soon outside the forest between fields. Together with the district road, the brook crosses under the federal motorway 6 and then runs on the western edge of the meadow soft area around Herboldshausen. At the former moated castle, the Greutbach flows in from the right, the first major tributary that arises on the motorway and previously runs through the hamlet. The desert stream , which comes from the west, follows about two hundred meters further .

There the course bends to the northeast and crosses under the K 2500 for the second time after the autobahn underpass, from which a connecting road to Lobenhausen now branches off. The forest islands of Hochholz on the left and Großes Weilersholz on the right come close to the bottom of the now stronger valley . Near an abandoned and overgrown old shell limestone quarry, the valley becomes a forest-filled little blade , in which large limestone blocks protect the left bank to protect the road running close to the water. This section of the blade, in the Crailsheim area from the southeast partially stretches a few steps across the stream, ends after a good half a kilometer, not at the mouth of the stream, but at the edge of the Lobenhauser Jagstschlinge around the eponymous Kirchberg hamlet, which is abandoned by the river.

In this gallery it flows flatter at first, soon increasing from Lobenhausen to below 377  m above sea level. NHN opens a small inlet in the middle of the loop and almost touches the western edge of the hamlet. The L 1041 Crailsheim – Kirchberg descends with it into the valley on its remaining half a kilometer long run, which is partly lined with reed strips. At the edge of the hamlet at the Lobenhauser Mühle , it finally flows into the Mühlkanal to the left of the central Jagst after a 3.8 km long path with a mean bottom slope of about 2.1 ‰ .

Catchment area

The 4.6 km² catchment area of ​​the Herboldshauser Bach is naturally located, with its southwest and central part, predominantly in the lower area of ​​the Haller Plain of the Hohenloher and Haller Plains , in which the brook also rises and remains for a good half of the first half. Afterwards, in the neighboring natural area of Kocher-Jagst Plains, it traverses the stripes parallel to the hunt from the sub-areas of Eastern Kocher-Jagst-Riedel and finally the Middle Jagst Valley . With over 445  m above sea level. NHN highest is the terrain is at the westernmost point between the highway exit Kirchberg the Federal Highway 6 and the southern Geißholz , but also in the whole arc of the upper watershed down both sides of the middle course in high wood left in Great Weiler wood right, the terrain falls almost never 435  m above sea level NHN .

The catchment area is a predominantly open and mostly arable landscape with four times parts of forest islands on the edge; the first in the very south, in which the Herboldshauser Bach rises; the goatwood in the west of the upper reaches; the high wood on the left and the large hamlet on the right above the middle course. The latter merges down the slope into the narrow and short Klingenwald, which the stream runs through shortly before entering the old loop of the Jagst near Lobenhausen, in which there is also a narrow strip of sloping forest on the old rebound slope, which in turn joins the left slope forest at the mouth of the stream Jagsttales passes over. There is only settlement in the area in the form of the hamlet of Herboldshausen a little to the right of the upper course at the tributary of the Greutbach and the hamlet of Lobenhausen also a little to the right just before the mouth, which also includes the Lobenhauser Mühle at the mouth, the only settlement right on the run. In addition, there is a gusset of a newer industrial park in the outer area of ​​the hamlet of Kleinallmerspann , which is itself outside, near the Kirchberg motorway exit. All of these belong to the small town of Kirchberg an der Jagst , as does the vast majority of the area. Otherwise only the city of Crailsheim with two forest spandrels has a share in this, with the southeastern half of the forest island, called Reisich , in which the stream arises, as well as the Großer Weilersholz , where in the Klinge the urban area even extends a few meters over the stream to the left bank of the stream .

The northern watershed from Hochholz to the estuary borders the immediate catchment area of ​​the downward Jagst , which is close by , which only experiences an inflow on this section from the Scheide through a short and unstable ravine through the Teufelsklinge and an equally unstable short slope channel. Behind the entire right watershed from the mouth up to the southern edge of the forest island, in which the Herboldshauser Bach arises, the Grundbach, which flows a little upstream of the Herboldshauser Bach, collects the runoff on the other side, first in the area of ​​the old Lobenhauser Jagstschlinge directly, then mostly via its left tributaries Weilersbach and Fürbach . The Tiefenbach and the Brühlbächle , two right tributaries of the Schmerach running to the Bühler , compete on the southwestern catchment area border, on which their hydrologically most important section runs along the Kocher -Jagst watershed. The higher Scherrbach tributary of the Hofbach , the Heppach and finally the Schindelbach follow one after the other on the north-west , which also drain into the Jagst downstream of the Herboldshauser Bach.

Tributaries and lakes

List of tributaries from the source to the mouth. Length of water, catchment area and altitude according to the corresponding layers on the LUBW online map. Other sources for the information are noted.

Origin of the Herboldshauser Bach at about 424  m above sea level. NHN in the forest island south of Herboldshausen on the profit boundary between the Crailsheim-Triensbacher Reisach and the Kirchberg-Lendsiedler community wood . The stream initially flows north.

  • Greutbach , from the right and southeast to about 423  m above sea level. NHN at Herboldshausen through which it previously flowed, 0.6 km and approx. 0.5 km². Arises at about 432  m above sea level. NHN next to the federal motorway 6 south-southeast of Herboldshausen.
  • Wüstenbach , from the left and west to about 421  m above sea level. NHN about 0.2 km after the previous one, 0.7 km and about 1.0 km². Arises at about 429  m above sea level. NHN at a fork in the field northwest of Herboldshausen.
  • (Inconsistent brook from the high wood ), from the left and west to about 418  m above sea level. NHN opposite the former quarry at the Großer Weilersholz , approx. 0.6 km and approx. 0.3 km². Arises at about 434  m above sea level. NHN next to a west-east forest path through the high wood . Flows in the lower reaches drained under a field.
  • (Inconsistent brook in the Lobenhausener Jagsttalschlinge), from the right and southeast to below 377  m above sea level. NHN , approx. 0.4 km and approx. 0.4 km². Flows at about 478  m above sea level. NHN behind house no. 18 in Lobenhausen is a tiny pond. Probably originated in or on the Brunnenwiesen field in the southeast of Lobenhausen. Drains most of the former southern Jagsttal loop.

Mouth of the Herboldshauser Bach from the left and southwest to about 355  m above sea level. NHN at the Lobenhauser Mühle in the local Mühlkanal on the left of the middle Jagst . The stream is 3.8 km long and has a catchment area of ​​4.6 km².

geology

The typical sequence of layers of the left Jagst tributaries near Kirchberg can also be seen in the catchment area of ​​the Herboldshauser Bach. The uppermost layer is a loess sediment layer consisting of Quaternary deposits on the Lettenkeuper ( Erfurt Formation ), which is dominant over a large area of ​​the plateau , the lowest Keuper layer. Underneath, the Upper Muschelkalk sets in , recognizable and mostly visible by the blade incisions in the direction of Jagst, in which the bed of the receiving river Jagst lies around Kirchberg. In the case of the Herboldshauser Bach, the source lies in the area of ​​the loess sediment layer and the shell limestone begins at or shortly after the bend to the northeast. At the old Muschelkalkbruch before the beginning of the wooded section of the blade, the Upper Muschelkalk is exposed on a small wall. the old quarry and a layer joint cavity at the foot of the wall are geotopes. The Upper Muschelkalk is also cut in a lower position to the left of the L 1041 at the transition to the Jagsttal. This geotope is not clearly visible because of a retaining wall against the mountain in the lower area.

See also

Individual evidence

LUBW

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

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

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. ↑ Geology roughly based on: Map server of the State Office for Geology, Raw Materials and Mining (LGRB) ( notes )

literature

  • Topographic map 1: 25,000 Baden-Württemberg, as single sheet No. 6825 Ilshofen and No. 6826 Crailsheim

Web links