Glattenzainbach

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Glattenzainbach
image
Data
Water code DE : 238648
location Swabian-Franconian forest mountains

Baden-Württemberg

River system Rhine
Drain over Fichtenberger Rot  → Kocher  → Neckar  → Rhine  → North Sea
source at the Gschwender Streusiedlungshof Hengstberg on the northwest tip of the municipality area
48 ° 56 '39 "  N , 9 ° 40' 42"  E
Source height approx.  550  m above sea level NN
muzzle opposite the Fichtenberger sports area from the right and south in the red coordinates: 48 ° 58 ′ 59 ″  N , 9 ° 42 ′ 46 ″  E 48 ° 58 ′ 59 ″  N , 9 ° 42 ′ 46 ″  E
Mouth height approx.  340  m above sea level NN
Height difference approx. 210 m
Bottom slope approx. 32 ‰
length 6.5 km
Catchment area 7.423 km²
Left tributaries see below
Right tributaries see below

The Glattenzainbach is a 6.5 km long brook in north-eastern Baden-Württemberg , which flows into the "Fichtenberger" Rot from the right and south near Fichtenberg in the Schwäbisch Hall district .

geography

course

The Glattenzainbach rises on the northern edge of the Lias plateau of the Welzheimer Forest in the north-western tip of the Gschwender community area, which is already divided by several streams . About a hundred meters northwest of its scattered settlement yard Hengstberg it arises at the beginning of the hillside forest down to the lower Stubensandstein high level ( Löwenstein formation ) around Murrhardt - Kirchenkirnberg . He quickly runs down the wooded step and then turns to the east in the open corridor in front of the L 1150, which has almost reached Kirchenkirnberg at the foot of its winding forest paths from Kaisersbach , first to take up two short streams from the right, along with theirs Inflows arise more or less high up on the same step edge.

Then it turns to the northeast, feeds a small pond shortly before crossing under the state road ("Gschwender Straße") which now continues out of the village to the east to the B 39 , takes an inlet from the village immediately after it and reaches a little further downhill of the Kirchenkirnberg sewage treatment plant, the confluence with a larger tributary that drains the first part of the step edge that continues to the east. From Kirchenkirnberg the valley road enters the valley, a forest road that from now on accompanies the stream to its mouth.

At this confluence, the Glattenzainbach already flows into a forest valley sunk a few dozen meters into the Stubensandstein surface, in which it continues in a northerly direction about 1.5 km to the Murrhardt-Kirchenkirnberger Weiler Täle , where it takes the brook from the Tiefen Klinge from the left and then, here a little way in the open valley floodplain, moves east into the municipality of Fichtenberg . After less than a further kilometer, a last more significant brook flows in from the south from the right, the remaining 2½ km to the mouth of the Glattenzainbach runs north-northeast and so close to the Rauhenzainbach , which is parallel to the east beyond the elongated mountain forest ridge Staufenberg , that from now there are no more tributaries from this side, but definitely from the left from the Schönhart , first one from the Gies- and then one from the Hirschblade .

A little below this, for the first time, a larger forest clearing extends to the left bank, soon afterwards the Glattenzainbachtal opens up to that of the Rot , here the stream finally enters the open corridor. The Glattenzainbach runs between a new development area on the left and an industrial area on the right, which already belong to Fichtenberg, and then flows across from the sports grounds from the right and south into the Rot, which runs eastwards here .

Catchment area

The Glattenzainbach drains almost 7½ km² of predominantly wooded area on the Lias edge of the Welzheimer forest and the upstream sandstone step south of the Rottal valley. It extends from the source to the mouth about 5 km in a north-northeast direction and has a maximum width of about 2½ km perpendicular to it. The catchment area is divided into the municipality of Fichtenberg, the city of Murrhardt and the municipality of Gschwend, in order of decreasing share; the proportions differ only slightly; Fichtenberg has less than a third more area than Gschwend.

In the northwest is the catchment area of ​​the smaller red tributary Dappach , in the northeast that of the receiving "Fichtenberger" Rot , which moves to the Kocher , in the entire east that of the Rauhenzainbach , also a tributary of the Fichtenberger Rot . Beyond the Lias edge in the south, another red flows south to the confluence with the Lein at the Voggenberger Sägmühle . To the west of the watershed, all competitors drain to the upper Murr , on whose much longer section the Gänsbach over the Otterbach and on a smaller, almost again in the northwest, the Seebach , which runs through the Fornsbacher Waldsee, to the Fornsbach .

Tributaries

also of a higher order, in each case from the source to the mouth and indented under the receiving water. Length of water as a rule according to LUBW-FG10, areas according to LUBW-SG10, heights according to the contour line image on the background map of the geodata viewer. Different data sources are indicated in footnotes.

Source of the Glattenzainbach about a hundred meters northwest of the Gschwender Streusiedlungshof Hengstberg at the beginning of the hillside forest at about 550  m above sea level. NN .

  • (Inflow), from the right at the entrance to the forest of a dirt road south of the Kirchenkirnberg cemetery at about 460  m above sea level. NN , about 0.465 km. Arises east of Gschwend- Hengstberg am Werrenbusch at about 540  m above sea level. NN .
    • (Shorter source branch), from the left to about 482  m above sea level. NN , about 0.225 km. Arises northeast of Hengstberg at about 530  m above sea level. NN .
  • (Inlet), from the right to about 460  m above sea level. NN , about 0.370 km. Arises southwest of Murrhardt - Leukers in the Werrenbusch at about 505  m above sea level. NN .
    • (Shorter source branch), from the right to about 470  m above sea level. NN , about 0.208 km. Arises closer to Leukers in the corridor at about 490  m above sea level. NN .
  • RiverIcon-SmallLake.svgFeeds a 0.0546 hectare pond in front of Gschwender Straße from Murrhardt - Kirchenkirnberg at about 455  m above sea level. NN .
  • (Inflow from Kirchenkirnberg), from the left on the edge of Gschwender Straße at about 450  m above sea level. NN , 1.067 km and 0 km². Arises east of the water reservoir next to the slope of the L 1150 at about 525  m above sea level. NN , reaches the village next to the old Dorfsteige (Kaisersbacher Straße) walking, then verdolt in the village. Almost as long as the official source branch.
  • (Periodic inflow from the west through the village), from the left to about 444  m above sea level. NN , about 0.581 km. Arises on the western edge of the village to Strut at about 460  m above sea level. NN . Accompanied in the village of Mühlbachweg, mostly with open barrel, reached the Glattenzainbach through a small side blade in which the Tälesstraße follows him down the left.
  • (Inlet through a pronounced forest blade from the east), from the right next to a footbridge immediately after the sewage treatment plant to below 440  m above sea level. NN , 0.93 km. Arises from the runoff of a 0.6271 hectare pond west of the road to Gschwend- Eichenkirnberg at about 470  m above sea level. NN .
    • (Longer source branch), from the left in the Waldklinge to about 463  m above sea level. NN , 0.443 km. Arises on the slope next to Gschwend- Krämersberg at about 480  m above sea level. NN .
    • (Inlet from the direction of Altersberg), from the left less than 200 m before the confluence at 439  m above sea level. NN , 1.234 km². Arises on the northwest edge of the soft patch from Gschwend- Altersberg to the hillside forest on the Lias edge at a little below 558  m above sea level. NN and flows past Leukers.
      • (A little shorter source branch), from the left near Leukers at about 485  m above sea level. NN , 0.392 km. Arises a few steps from the other Altersberger source at about 553  m above sea level. NN .
  • (Waldklingenbach from the playground), from the left to below 420  m above sea level. NN , 0.519 km. Arises east of Murrhardt- Spielhof on the edge of the Haseläcker forest at about 465  m above sea level. NN . A somewhat longer source branch comes from the north.
  • (Waldklingenbach), from the right to about 410  m above sea level. NN , 0.371 km. Arises in the east of the Gewanns Mad and partial forest at about 450  m above sea level. NN .
  • (Waldklingenbach through the play forest ), from the left to 402  m above sea level. NN , 0.641 km. Arises in front of the northeast tip of the sports field at the playground at about 470  m above sea level. NN .
  • (Waldklingenbach), from the left on the southern edge of Murrhardt- Täle to less than 400  m above sea level. NN , 0.802 km. Arises in the northern play forest at about 470  m above sea level. NN .
    • RiverIcon-SmallLake.svg Immediately in front of its mouth it feeds a 0.0402 hectare pond into which a left branch of the Glattenzainbach also flows.
  • (Bach from the Tiefen Klinge ), from the left on the eastern edge of Täle at about 395  m above sea level. NN , 1.418 km. Arises on the K 1804 Spielhof – Fichtenberg- Hinterlangert at about 481  m above sea level. NN . Long border from Murrhardt to Fichtenberg .
  • (Waldklingenbach from the south), from the left at the north-northwest bend at 379.1  m above sea level. NN , 0.731 km. Arises in the eastern Mad and partial forest at about 470  m above sea level. NN .
  • (Waldbach from the Giesklinge ), from the left to 371  m above sea level. NN , 1.053 km. Arises in the Schönhart at about 470  m above sea level. NN .
  • ( Forest stream through the deer blade ), from the left to about 460  m above sea level. NN , 0.605 km. Arises at about 420  m above sea level. NN .

Mouth of the Glattenzainbach on the eastern edge of Fichtenberg next to the Hirschäcker road at about 340  m above sea level. NN from the right and south into the lower Fichtenberger Rot .

Settlements on the run with territorial affiliations

Settlements on the brook are only given the names in the deepest nesting level

geology

The Glattenzainbach rises in the marl ( Trossingen formation ), its secondary brook of the second order from Altenberg even a little higher in the locally overlapping Liaskappe around the hamlet. These source brooks soon reach the Stubensandstein ( Löwenstein Formation ), from which they switch to the Upper Bunten Marl ( Mainhardt Formation ) roughly along the route of the L 1150 ; here the runs also begin to deepen more steeply. From here to the hamlet of Täle, silica sandstone ( Hassberge formation ), Untere Bunte marl ( Steigerwald formation ) and reed sandstone ( Stuttgart formation ) are passed through very quickly , there the Glattenzainbach enters the Gipskeuper ( grave field formation ), in which it up remains to the mouth.

In the southern part of the catchment area there is extensive Stubensandstein, which also continues on both sides of the valley in the east on the plateau to the edge of the valley section running eastwards to Täle, and in the west along the watershed even a little further. In Schönhart there is extensive Upper Bunter Marl, the remaining middle Keup layers above the Gipskeuper lie in almost everywhere only narrow strips around the valley cuts of the Glattenzainbach and its larger lower tributaries.

The floodplain clay strip begins a little below the Kirchenkirnberg sewage treatment plant and accompanies the stream to its mouth as a very narrow band until almost the end; These valley fillings are also found in the lower valleys of the larger tributaries below.

The forest valley that flows from the right at the Kirchenkirnberg sewage treatment plant follows a geological fault line that continues beyond the Glattenzainbach and its western watershed far northwest towards Fornsbach . Approximately parallel another 1 - 1.5 km in the southwest runs another fault, in between lies a deep floe, so that Kirchenkirnberg like the Liaskappe around Altenberg, on the edge of which the higher springs are, lie tectonically deeper than the surroundings. This may have contributed to the extensive preservation of the Lias layer, which has already been removed further east.

See also

Web links

Commons : Glattenzainbach  - Collection of images, videos and audio files

Individual evidence

  1. ↑ a b According to the contour line image on the background map of the geodata viewer.
  2. ↑ a b According to LUBW-GEZG (data record entry).
  3. ↑ a b c d e f g Measured on the geodata viewer.
  4. ↑ a b c Text entry in blue at the mouth on the background map of the geodata viewer.
  5. ↑ Labeling in blue at the mouth on the background map of the geodata viewer, with altitude point on the mouth.

literature

  • "TK25": Topographic map 1: 25,000 Baden-Württemberg North, as single sheet no. 7024 Gschwend
  • "GK50": Geological map of the Swabian-Franconian Forest Nature Park 1: 50,000, published by the State Office for Geology, Raw Materials and Mining Baden-Württemberg, Freiburg i. Br. 2001

Web links