Roggelshäuser Bach

	Roggelshauser Bach; Roggelshauser Bach
	; Image wanted
	Data
Water code	DE : 2388338
location	Kocher-Jagst Plains Bartenstein-Langenburger platters; Middle Jagsttal; Baden-Württemberg Schwäbisch Hall district Gde. Blaufelden ; City of Schrozberg ; ; Hohenlohe district Gde. Mulfingen ; ;
River system	Rhine
Drain over	Jagst → Neckar → Rhine → North Sea
source	east of Blaufelden- Simmetshausen at the northwestern tip of the Kellerholz ; 49 ° 19 ′ 19 ″ N , 9 ° 52 ′ 54 ″ E
Source height	approx. 456 m above sea level NHN
muzzle	in Mulfingen from the right and east-southeast in the middle Jagst coordinates: 49 ° 20 '27 " N , 9 ° 47' 48" E 49 ° 20 '27 " N , 9 ° 47' 48" E;
Mouth height	approx. 262 m above sea level NHN
Height difference	approx. 194 m
Bottom slope	approx. 25 ‰
length	7.7 km
Catchment area	13,492 km²

The Roggelshäuser Bach or Roggelshauser Bach is a not quite 8 km long brook in northeastern Baden-Württemberg , first in the Schwäbisch Hall district , then in the Hohenlohe district , which flows from the right into the middle Jagst in the village of Mulfingen .

Surname

The brook is apparently named after the place Roggelshausen , which fell into desolation in the 14th century , which, according to old location information and the still common, identical gain name, was located in the area of the upper retention basin at the foot of the Kappelberg . Roggelshausen is a modification of the original name Rakundshausen, mentioned in 1303, meaning 'Haus einer Ratgund ', which was mentioned in 1303.

The name form of the stream is a bit uncertain. The most commonly encountered is Roggelsh ä user Bach , rarely one finds also Roggelsh a user Bach .

The lower valley running westwards in front of Mulfingen is named Öltal , apparently after an oil mill that once existed there .

geography

course

The Roggelshäuser Bach arises about 0.8 km southwest of the center of the village of Herrentierbach in the municipality of Blaufelden and about 0.6 km east of the hamlet of Simmetshausen, which is also in the Herrentierbach submarket, at about 456 m above sea level. NHN at the northwestern tip of the forest island of Kellerholz . The creek, which initially runs in a ditch next to a dirt road and also often runs dry in the upper reaches, runs for a long time approximately northwest and slowly digs its long, flat and not very narrow valley basin.

After less than 200 meters, it passes under the K 2535, which connects the two places mentioned, and then flows for the most part unaccompanied by paths and without tree cover between fields. Less than 400 meters north-east of the outskirts of Simmetshausen, a ditch, which is also drying up, joins a dirt road in the Brühl . Only about 1.8 km after its source feeds the Roggelshäuser Bach for the first time somewhat longer and less dehydrated, trench-led tributary from the edge of the forest island of Eichholz , after which it constantly carries water and flows gently under trees on the bank for the first time.

After two hundred meters he reaches the outskirts of the hamlet of Alkertshausen , which is also part of Herrentierbach, and through which it flows diligently . The place is hidden in the creek trough, which is now about 50 meters opposite the lateral heights, which is crossed here by the L 1022 Herrentierbach – Mulfingen. Above the stream that follows the village in natural loops and is accompanied by trees on the bank, forest quickly replaces the previous fields and after the inflow of a stream coming from the right from the direction of Wittmersklingen , the now deeply cut valley is soon completely forested.

About from the mouth of the Hasenklingenbach to only about 375 m above sea level. NHN valley and stream turn south of the Schrozberger hamlet Mäusberg on the right edge of the hill quickly to the west. The following lower course is almost from the beginning in the area of the municipality Mulfingen . Between the Lauberg on the left and the Kappelberg on the right, the valley forest opens up on the ground and the slopes also become lighter. In the Wiesengewann Roggelshausen , the water runs through the upper of the two flood retention basins in the valley, which is only filled in the event of a flood, after which it flows out at about 315 m above sea level. NHN the brook from the right side valley Greutklinge .

The valley basin is now open up to the middle slopes and the Roggelshäuser Bach then flows into the lower of the flood retention basin, in which it is constantly dammed into a nearly 300 meter long and 1.7 hectare lake with a small island of trees.

Below the dam, the Roggelshäuser Bach, still winding and with tree-lined banks, flows along the south side of the sports area on the eastern edge of Mulfingen, through which the brook from the map blade flows open , the second of the two largest tributaries. After entering the settlement area of the village, it soon disappears in a Verdolung, the route of which follows the Bachgasse , the main street and then the street Unterer Bach . Finally, it crosses under the Ailringer Straße (L 1025) following the river bank and finally flows out at about 262 m above sea level. NHN less than 50 meters before the St. Anna Bridge and opposite the St. Anna Chapel from the right into the middle Jagst .

The Roggelshäuser Bach has a 7.7 km long, first northwest, then western course with a mean bottom gradient of about 25 ‰ and flows about 194 meters below its origin.

Catchment area

The Roggelshäuser Bach has a catchment area of 13.5 km² with the contour of a tube up to a little over two kilometers wide around the first northwest, then west flowing water. From a natural point of view, it belongs to the Kocher-Jagst Plains , largely to its sub-area Bartenstein-Langenburger Platten , near the mouth of the sub-area Middle Jagsttal . The highest point in the Kellerholz in the southeastern tip, a little above the source of the stream, rises only a little over 475 m above sea level. NHN .

In the north and northeast it borders on the catchment area of the Ette , the next and somewhat larger right tributary of the Jagst , in the east on that of the left Ette upper reaches Tierbach . In the south-east the Blaubach flows outside , which also feeds the Jagst from the right via the Brettach significantly further upwards. The adjoining area in the south is drained by the Rötelbach, which flows less high up to the same, while in the south-west, the Märzenbach tributary on the right, which flows as the last before the Roggelshäuser Bach, carries the outflow to the other side.

Only the hamlet of Alkertshausen of the municipality of Blaufelden is traversed by the stream on the upper reaches , while the hamlet of Simmetshausen is already on the left and a small part of the village of Herrentierbach on the right. At the bend in the run, the area of the town of Schrozberg extends for about half a kilometer to the right bank, from which the hamlets Wittmersklingen , Hirschbronn and Mäusberg lie above the now deepened brook on the right plateau. The lower reaches to the west soon crosses the border of the district of Schwäbisch Hall to the area of the municipality of Mulfingen in Hohenlohekreis , of which the hamlet of Ochsental stands on the right plateau and the estuary village of Mulfingen is only the second place directly on the river.

The plateau parts of the catchment area consist predominantly of open, arable agricultural land, but there are also some small forest islands that are generically called Hölzle in the region . To the west of Simmetshausen, a somewhat larger forest island extends into the catchment area. The valley is already completely wooded between Alkersthausen and before its bend to the west and it remains for a long time, at least on the slope almost to Mulfingen; Continuations of these hillside forests sometimes extend far over the upper bend in the slope to the edge of the plateau.

Tributaries and lakes

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

Origin of the Roggelshäuser Bach at about 456 m above sea level. NHN approx. 0.6 & nbsü: km east of the center of Blaufelden - Simmetshausen on the northwestern tip of the Kellerholz .

(Graben between Weilerfeld and Brühl ), from the left and southwest to about 439 m above sea level. NHN , less than 0.4 km and approx. 0.7 km². Arises at about 448 m above sea level. NHN on the northern edge of Simmetshausen. Incessantly water-bearing ditch between fields
(Stream from the edge of the oak ), from the right and east-northeast to about 415 m above sea level. NHN just before Blaufelden- Alkertshausen , approx. 0.7 km and approx. 0.7 km². Arises at about 442 m above sea level. NHN about 0.8 km east of the center of Alkertshausen on the north-western edge of the Eichholz . The longest part of the digging in a natural hollow.
(Bach from the direction of Wittmersklingen), from the right and northeast to about 397 m above sea level. NHN between Alkertshausen and a last isolated house in front of the valley forest, approx. 0.7 km and approx. 0.6 km². Arises at about 443 m above sea level. NHN about 0.3 km west of the center of Schrozberg - Wittmersklingen on a dirt road branching off the road from Wittmershausen to Schrozberg- Mäusberg . Initially digging away.
Hasenklingenbach , from the right and east-northeast to about 375 m above sea level. NHN south of Schrozberg- Mäusberg in the valley forest, 1.3 km and 1.3 km². Arises at about 447 m above sea level. NHN in the large fields a little southeast of Schrozberg- Hirschbronn .
After this inflow, the Roggelshäuser Bach quickly turns to the west.
- (Inflow), from the right and northeast to about 403 m above sea level. NHN in the forest edge of the lower reaches, approx. 0.6 km and approx. 0.5 km². Arises at about 445 m above sea level. NHN on a dirt road a little before the north-western outskirts of Hirschbronn and initially flows as a vegetation-free ditch in a natural hollow along a field border.
  The main arm is about 0.9 km up to this tributary and has a sub-catchment area of about 0.7 km².
  - About 150 meters northeast of the beginning of the ditch there is a pond in the catchment area at about 449 m above sea level. NHN a little north of Hirschbronn, 0.1 ha.
(Blade inflow), from the right and north-northeast to about 367 m above sea level. NHN south-southwest of Mäusberg in the valley forest, approx. 0.3 km and approx. 0.3 km². Arises at about 415 m above sea level. NHN at the beginning of the blade forest.
(Bach from the Hundsklinge ), from the right and north-northeast to about 360 m above sea level. NHN southwest of Mäusberg in the valley forest on the border with Mulfingen , over 0.3 km and approx. 0.3 km². Arises at about 415 m above sea level. NHN at the edge of the blade forest.
Flows through below 330 m above sea level. NHN in the floodplain, which is open again, the usually empty upper basin of the flood protection systems at the foot of the Kapellenberg .
(Bach from the Greutklinge ), from the right and northeast to 315.4 m above sea level. NHN , 0.8 km and 0.8 km². Arises at almost 410 m above sea level. NHN a little south of Mulfingen- Ochsental at the beginning of the Klingenwald.

Lower basin of the flood retention systems in front of Mulfingen

Flows through below 310 m above sea level. NHN the permanently dammed lower basin of the flood protection systems in front of the sports fields on the eastern edge of Mulfingen, 1.7 ha.
(Stream from the cat's blade) , from the right and northeast to about 286 m above sea level. NHN in the middle of the sports fields on the eastern edge of Mulfingen, 1.3 km and 1.4 km². Arises at about 402 m above sea level. NHN west of Ochsental near the K 2306 to Mulfingen at the beginning of its blade forest. At the middle course in the area of a filled landfill apparently verdolt.
Flows through to about 285 m above sea level. NHN a pond in the area of the sports fields, just under 0.1 ha.

Mouth of the Roggelshäuser Bach from the right and finally east to about 262 m above sea level. NHN in Mulfingen shortly before the St. Anna Bridge from the right and finally east into the middle Jagst . The brook is about 7.7 km long and has a 13.5 km² catchment area.

Retention basin

At the Roggelshäuser Bach there are two flood retention basins about 2.7 km and about 1.5 km before the mouth of the brook in the village in the area of the municipality of Mulfingen . Both are operated by the Ette-Kessach water board and dam behind earth embankments. The stream flows through each of them ("main circuit") and their flood water is drained uncontrolled.

Flood retention basin on the Roggelshäuser Bach
Surname	location			Dammed water and drainage	Storage space in m ³		EZG	Storage space		Dam height	Construction year
			place		Maximum	Duration		Max	Duration
Upper pelvis	⊙49.340969444444 9.8299527777778 330	in front	Inflow from Greutklinge	Roggelshäuser Bach	146,000	-	09.0 km ²	?	-	15.1 m	1964
Lower basin	⊙49.341472222222 9.8147388888889 310	in front	Inflow from cat blade	Roggelshäuser Bach	210,000	066,000	11.2 km ²	?	1.7 ha	15.8 m	1965
Information on storage space, dam height and year of construction and the usual area of the permanently dammed basins according to the official waterway map. The upper retention basin (with the entry "-" in the column for the permanent storage space) is usually waterless. The catchment areas were measured on this map, taking as far as possible the area values for the sub-catchment areas that were not to be cut up for this purpose.

geology

In the subsurface of the catchment area of the Roggelshäuser Bach in the Kocher-Hagst-Platten, there is shell limestone everywhere . The brook rises in the Lettenkeuper ( Erfurt formation ), which overlies over wide areas on the uppermost course and later on both sides on the edge heights . After about half of the way to Alkertshausen, the creek basin has deepened into the Upper Muschelkalk . The stream remains in this layer until it bends westward and into the Mulfingen municipality. At the level of the Middle Muschelkalk , which is spreading on the valley flanks , the stream then runs to the lower of the two rainwater retention basins, where it is then replaced by the Lower Muschelkalk .

While the stream is already surrounded by a mostly narrow flood plain after Alkertshausen, at the bottom of the valley mouth funnel with the village center of Mulfingen there are also Holocene runoff masses.

In the catchment area there are some faults moving from east-south-east to west-north-west, a slightly larger number sweeps perpendicularly from south-south-west to north-north-east, including a single longer fault over upward Jagst and Roggelshäuser Bach near the mouth in Mulfingen.

The inconsistent water-bearing upper reaches of the Roggelshäuser Bach and most of its tributaries show the karstification of the shell limestone. About 400 meters to the left shortly after the Laufknie in the Saubühl forest are two larger funnel-shaped dolines in a location typical of the region on the boundary between Upper Muschelkalk and Lettenkeuper; at the edge of one of them, the so-called Saubrunnen rises , a weak spring whose drain sinks after a few meters into the sinkhole of the sinkhole. The sinkholes are designated as a geotope.

Nature and protected areas

Around Simmetshausen, the Roggelshausen brook is classified as rich in fine material , then classified as a low mountain range carbonate brook that is rich in coarse material up to the mouth . At the upper reaches the stream tends to dry up, it runs here as a field-separating ditch with few changes of direction and with only one section, next to a short field path, tree cover on the bank. A little before Alkertshausen, it then begins to show a more natural picture with windings and trees on the bank, which continues in the hamlet after the rotting. There it is one to two and a half meters wide.

With the beginning of the valley forest, it meanders even more and also forks in parts. At first it has more fine sandy and muddy sediment, then more and more block-rich. The stream flows over slabs of rock and small rapids, falls into pools and its bed width fluctuates greatly. There is sometimes rock on the steep bank sections.

In the Mulfingen area, the bed widens to three to five meters. The course is a little straighter here again, perhaps because of an earlier regulation, because there are remains of fortifications on the bank. Small, temporary side arms of the more and more rubble bed probably follow natural old stream routes. Two fords with an artificial threshold cross the stream on this section. Somewhat in front of the upper basin of the Mulfingen flood retention system, which is mostly a green meadow and which the stream then runs straight through, there is a rubble rake in the bed.

Below the basin dam, the stream flows more naturally again, and is now up to seven meters wide. After the inflow from the right from the Greutklinge, stone bars run down vertically on the south-facing slope of this valley side, the sequence of which continues into the Jagsttal. After the dammed Lower Basin and the Katzenklinge (Katzenklinge), which is already close to the village, there are Steinriegel to the left of the Geißberg opposite the Eichhörnle and the Schweinberg . The brook is almost completely ruined through Mulfingen.

Below Alkersthausen, the valley lies up to the Mulfingen outskirts in two landscape protection areas, first up to the district boundary in the Mittleres Jagsttal area with side valleys and adjacent areas , on the subsequent larger section on Mulfinger Grund in the Jagsttal area with side valleys and adjacent areas between the district boundary Schwäbisch Hall and Krautheim / Schöntal municipal boundary .

Individual evidence

LUBW

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

↑ ^a ^b ^c ^d ^e Height according to the contour line image on the background layer topographic map .

↑ ^a ^b Length according to the water network layer ( AWGN ) , supplemented by a small initial section not included on the waterway map, which was measured on the topographic map background layer .

↑ ^a ^{b Catchment} area summed up from the sub-catchment areas according to the basic catchment area layer (AWGN) .

↑ Evidence for the two forms of name:
- The current topographic map background layer does not have any lettering on the barrel.

↑ Length according to the waterway network layer (AWGN) .

↑ ^a ^b Lake area according to the layer standing waters .

↑ ^a ^{b Catchment} area after the basic catchment area layer (AWGN) .

↑ ^a ^b ^c ^d ^e ^f ^g Length measured on the background layer topographic map .

↑ ^a ^b ^c ^d ^e ^f ^g ^h Catchment area measured on the background layer topographic map .

↑ Height according to the gray lettering on the background layer topographic map .

↑ Data on the dams according to the relevant layer.

↑ Protected areas according to the relevant layers, nature partly according to the biotope layer .

Other evidence

↑ name history and location of Roggelhausen by

the chapter on Mulfingen of the description of the Oberamt Künzelsau from 1883, p. 708
the page Roggelshausen - desertification of the regional historical information system www.leo-bw.de

↑ Origin of the Name Öltal (there still Olt h al ) for the valley to the dialed oil mill by

the chapter on Mulfingen of the description of the Oberamt Künzelsau from 1883.

According to the wording there, it is unclear whether this oil mill itself belonged to the town of Roggelshausen.

↑ 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)

↑ 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 )
↑ Geotope profile of the two sinkholes and the suction well (PDF, 898 kByte) on the website of the State Office for Geology, Raw Materials and Mining (LGRN).

literature

Topographic map 1: 25,000 Baden-Württemberg, as single sheet No. 6624 Mulfingen and No. 6625 Schrozberg West

Web links

Commons : Roggelshäuser Bach - Collection of images, videos and audio files

Map of the course and catchment area of the Roggelshäuser Bach on: State Institute for the Environment Baden-Württemberg (LUBW) ( information )
Measuring table sheets in the Deutsche Fotothek :
- 6624 Dörzbach from 1939
- 6625 Schrozberg from 1939

[TK-HLB-Höhe-1] Height according to the contour line image on the background layer topographic map .

[Name+Lage-Roggelshausen-4] story and location of Roggelhausen by

the chapter on Mulfingen of the description of the Oberamt Künzelsau from 1883, p. 708

the page Roggelshausen - desertification of the regional historical information system www.leo-bw.de

[3] the chapter on Mulfingen of the description of the Oberamt Künzelsau from 1883, p. 708

[4] the page Roggelshausen - desertification of the regional historical information system www.leo-bw.de

[Name-Öltal-6] Origin of the Name Öltal (there still Olt h al ) for the valley to the dialed oil mill by
the chapter on Mulfingen of the description of the Oberamt Künzelsau from 1883.
According to the wording there, it is unclear whether this oil mill itself belonged to the town of Roggelshausen.

[6] the chapter on Mulfingen of the description of the Oberamt Künzelsau from 1883.

[BfL-162-7] 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)