Heimbach (stove)

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Heimbach
Data
Water code DE : 23865734
location Hohenloher and Haller level

Baden-Württemberg

River system Rhine
Drain over Kocher  → Neckar  → Rhine  → North Sea
source west of the Heimbach settlement in Hall on the route of the western bypass ( B 14 )
49 ° 6 ′ 36 ″  N , 9 ° 42 ′ 27 ″  E
Source height approx.  372  m above sea level NHN
muzzle At the Haller Ritterbrücke from a pipe from the left in the Kocher coordinates: 49 ° 6 '47 "  N , 9 ° 43' 59"  E 49 ° 6 '47 "  N , 9 ° 43' 59"  E
Mouth height 273.2  m above sea level NHN
Height difference approx. 98.8 m
Bottom slope approx. 46 ‰
length 2.1 km
Catchment area approx. 1.73 km²
Medium-sized cities Schwäbisch Hall

The Heimbach is a two-kilometer-long left tributary of the Kocher in the town of Schwäbisch Hall in the district of Schwäbisch Hall in north-eastern Baden-Württemberg , which runs through the Heimbachklinge .

geography

The Heimbach arises a little west of the Heimbach settlement on the route of the Schwäbisch Hall western bypass. At the very beginning it runs southeast, then turns east and runs in a settlement-free hollow between the old hamlet of Heimbach in the south and the Heimbach settlement in the north, one behind the other through two silting ponds of around 0.1 ha each. From the lower one it flows piped under the Stuttgarter Straße through and underground on its south side to below the confluence of the B 19 from a south-eastern side hollow. On the left side of the road there is a long-abandoned quarry with a high wall in the Upper Muschelkalk and covered with Lower Copper.

After this Seitentalzulauf in which no open water flows, it enters a stone's throw from the well Heimbacher platforms Stuttgart said road to light up and running for about half a kilometer in a narrow, with limestone slabs quite naturally designed bed hard on the right foot of its steep blade downhill to the northeast. About a hundred meters before it flows into the Kochertal, it changes the side of the road and on the other side enters an open concrete canal with a retention device for floating debris, which then disappears under the northern foot of the viaduct of the Crailsheim – Heilbronn railway line crossing the Klinge . It then runs underground a few meters north of Heimbacher Gasse, which runs in the deepest part of the trough, through the suburb Beyond Kochens the Schwäbisch Hall old town to the Ritterbrücke, where it flows from a pipe from the left into the middle cooker .

The Heimbach is about 2.1 km long, has a mean bed gradient of about 46 ‰, on the steepest kilometer through its blade even of 70 - 80 ‰, and it drains an area of ​​about 1.7 km². Its highest point at about 410  m above sea level. NHN is almost three kilometers west of the estuary at its western tip on a hilltop of the forest cemetery. In north-south direction, the catchment area is nowhere wider than one and a quarter kilometers. Except in its western wedge, in the village-like soft area around Heimbach and on the steep slopes of the blade, almost all of it is built on.

The Heimbach runs through layers of the Unterseuper , the Upper and finally the Middle Muschelkalk . In the west of the catchment area lies Gipskeuper ( Grabfeld Formation ) above the Lower Keuper, which also belongs to the Mittelkeuper . In front of the mouth of the blade, the geological map draws an alluvial fan on the lowest slope of the Kocher valley, which, however, cannot be recognized morphologically in nature, at least in the southern part (hollow).

The Heimbach often falls completely dry on its open course due to its blade, but can then swell surprisingly when there is a downpour and has even flooded Steigenstrasse.

history

Up until the middle of the 19th century there was no road in the impassable Klinge of the Heimbach, then called the Hofklinge . The important overland connection from Schwäbisch Hall to the west in the direction of Mainhardt and further used a much steeper ascent from Schwäbisch Hall in the valley via the so-called Alte Heimbacher Steige. At the top it then ran further west on the southern edge of the brook gorge. The new path was opened in 1840.

See also

Individual evidence

  1. After the contour line image on the background layer topographic map at the map services of the LUBW.
  2. Reservoir level of the digester above the Dreimühlen weir (Salinenstraße), labeling on the background layer of the topographic map at the LUBW map services.
  3. State Institute for the Environment Baden-Württemberg (LUBW) ( information )
  4. Measured with the aid of the catchment areas layer for the LUBW map services.
  5. ^ Geology according to GK50-SFW.
  6. Topographical Atlas of Württemberg, sheet 30, 1841 (JPG; 15.7 MB).
  7. Allgemeine Zeitung of July 30, 1840 ( digitized in the Google book search)

literature

  • "TK25": Topographic map 1: 25,000 Baden-Württemberg North, as single sheet no. 6824 Schwäbisch Hall
  • "GK50-SFW": 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