Glane (Ems)
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Glane upper reaches: Recktebach → Uffelager Bach → Lienener Mühlenbach → Ladberger Mühlenbach |
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 Mühlenbach in Ladbergen, where the river is not yet called Glane. |
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| Data | ||
| Water code | EN : 334 | |
| location | Lower Saxony , North Rhine-Westphalia ; Germany | |
| River system | Ems | |
| Drain over | Ems → North Sea | |
| source | West of Bad Iburg as-stretched Bach 52 ° 9 '10 " N , 8 ° 1' 35" O |
|
| Source height | approx. 117 m above sea level NN | |
| muzzle | near Hembergen in the Ems Coordinates: 52 ° 9 ′ 7 ″ N , 7 ° 37 ′ 46 ″ E 52 ° 9 ′ 7 ″ N , 7 ° 37 ′ 46 ″ E |
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| Mouth height | 35 m above sea level NN | |
| Height difference | approx. 82 m | |
| Bottom slope | approx. 24 ‰ | |
| length | 3.4 km | |
| Catchment area | 353.708 km² | |
The Glane (water code number 334) is an orographically right tributary of the Ems south of Saerbeck in North Rhine-Westphalia , Germany . According to the NRW water register, the river is 35.1 km long, although it is usually only mentioned for the last 3.4 km from the confluence of Ladberger Mühlenbach and Eltingmühlenbach Glane. In the upper reaches the names Recktebach , Uffelager Bach , Lienener Mühlenbach and Ladberger Mühlenbach are used in sections.
geography
course
The course description follows the stationing of the water body number 334 from the source of the Recktebach to the mouth as Glane.
Recktebach and Uffelager Bach
The Glane arises as -stretched brook in Lower Saxony Bad Iburg 1.2 km west of the center on the south side of the Teutoburg Forest belonging highlands at an altitude of 117 m above sea level. NN . The stream initially flows south and passes Ostenfelde . Here the course turns to the west. After a total of around 2.8 km of flow, the stream crosses the border with North Rhine-Westphalia and thus changes its name for the first time.
The river, now known as the Uffelager Bach, continues to flow in a south-westerly direction. With the mouth of the Brookbieke after a further 2.1 km of flow, the brook changes its name again and is now called Lienener Mühlenbach .
Lienen mill stream
As Lienener Mühlenbach, often only briefly Mühlenbach, the water now mainly flows in westerly directions. After crossing under the Meckelweger Straße, the Mühlenbach flows through the Flaaken nature reserve , which it leaves on the Kattenvenner Straße southwest of Rethemeyer . At Baumhöfener , the stream flows past a larger pond and takes its drainage. After crossing under the Warendorfer Weg, the stream enters the Feuchtwiesen nature reserve on the Bullerbach . After a river stretch of about 1200 m, the stream leaves this again. After crossing under the K32, the Mühlenbach changes its course to the southwest until it reaches the Wanne-Eickel-Hamburg railway line . About halfway, water is cut into a ditch that flows into the Bullerbach southwest of the Blömker farm in the Holzhausen farming community . After the railway line has been crossed, the Mühlenbach passes the northern edge of a pond. With the mouth of the Bullerbach in the west of the pond, the course of the river changes its name again.
Ladberger Mühlenbach
The river, now known as the Ladberger Mühlenbach, continues to flow in predominantly western directions and forms the municipal boundary between Lengerich and Lienen up to around 800 m after the mouth of the Bullerbach . West of Stille , the Mühlenbach reaches the border between Ladbergen and Lengerich and with it the Gut Erpenbeck nature reserve , which it flows through over a length of 2.6 km. On this section, the aforementioned border runs on the northern bank. Continuing to the west, the Mühlenbach flows under the federal road 475 and then reaches the local area of Ladbergen, which it leaves again after crossing under the state road 555. Shortly before the brook crosses the A1 motorway , the brook Berlemanns Welle joins on the left . About 1 km after crossing the autobahn, the Mühlenbach reaches the Dortmund-Ems Canal . Before crossing under a culvert , the Ladberger Aa flows out on the right .
Immediately after crossing under the canal, the Mühlenbach leaves the municipality of Ladbergen. Initially, the river forms the border between Saerbeck in the north and Greven in the south for about 450 m . The river then flows a short distance in a north-westerly direction and touches the area of the Münster / Osnabrück Airport on its eastern border. Upon reaching the Ladberger Mühlenbach nature reserve , the river turns west again. After passing the new mill, the river forms the border between Greven and Saerbeck until it flows into the Ems. Around 3.4 km above its own mouth, the Eltingmühlenbach flows to the left .
Glane
Below the confluence, the river is called the Glane. After crossing the B219, flowing in north-westerly directions, the Glane reaches the Emsaue nature reserve, where it flows into the Ems on the right after a further 500 m stretch of river. The mouth is at a height of 36 m above sea level. NN . This means that the height difference between the source and the mouth is about 81 m. With a length of 35.1 km, the mean bed slope is less than 0.5 ‰.
Tributaries
In the following table, the named direct and indirect tributaries of the Glane are listed, as they are recorded in the NRW water register. Section names are not listed.
| Surname |
location |
Length [km] |
Catchment area [km²] |
Mouth height [m. ü. NN] |
DGKZ |
|---|---|---|---|---|---|
| Brookbieke | Left | 2.4 | 71 | 334 12 | |
| Yeltsebach | right | 2.9 | 334 14 | ||
| Line | right | 5.7 | 334 16 | ||
| Ölmühlenbach | right | 2.1 | 334 162 | ||
| Brüggelieth's brook | right | 3.6 | 334 164 | ||
| Glanebach | right | 7.1 | 334 18 | ||
| Bullerbach | Left | 9.1 | 11,421 | 334 2 | |
| Igelbach | right | 7.0 | 334 312 | ||
| Berlemann's wave | Left | 8.7 | 11.752 | 334 32 | |
| Ladberger Aa | right | 20.3 | 67.576 | 334 4 | |
| Lengericher Aa Bach | - | 334 4 | |||
| Hülsbach | right | 1.6 | 334 4132 | ||
| Hagenbach | Left | 4.2 | 334 414 | ||
| Black pool ditch | Left | 4.8 | 334 416 | ||
| Papenbrökegraben | Left | 1.3 | 334 4184 | ||
| Aldruper Mühlenbach | right | 8.1 | 22.282 | 334 42 | |
| Wechter Mühlenbach | right | 11.7 | 334 426 | ||
| Rehagenbach | right | 6.3 | 334 52 | ||
| Eltingmühlenbach | Left | 51.3 | 166,342 | 334 6 | |
| Sunderbach | right | 1.8 | 334 6112 | ||
| Freedenbach | Left | 4.1 | 4,668 | 334 612 | |
| Föhrenteichsbach | right | 1.9 | 334 6122 | ||
| Vogelpohl's Bach | right | 3.8 | 334 6132 | ||
| Glahne | Left | 1.6 | 334 6154 | ||
| Old Glaner Bach | Left | 3.9 | 0.565 | 334 616 | |
| Frenzied Boller | right | 2.5 | 334 6192 | ||
| Deslager Bach | right | 2.9 | 334 6194 | ||
| Dubte | Left | 5.8 | 334 6196 | ||
| Bockhorn Bach | right | 11.7 | 29.818 | 334 62 | |
| Noerenbrooker Trench | Left | 5.8 | 334 622 | ||
| Freienhägener Graben | right | 3.6 | 334 6222 | ||
| Imhorster Bach | Left | 1.5 | 334 626 | ||
| Riedenbach | right | 6.0 | 9.228 | 334 64 | |
| War trench | Left | 3.5 | 334 652 | ||
| Vorblecksbach | right | 5.7 | 334 654 | ||
| Saatgau brook | Left | 2.6 | 334 656 | ||
| Deppengaugosse | Left | 3.9 | 334 658 | ||
| Malleable cast iron | right | 3.6 | 334 6592 | ||
| Wöstengutter | Left | 5.0 | 4.987 | 334 66 | |
| Luetke Beeke | right | 11.0 | 13,153 | 334 68 |
Catchment area
The catchment area of the Glane is located in the Ostmünsterland southwest of the Teutoburg Forest . Its subsoil consists of predominantly sandy deposits from the Saale cold period ( pre- and post-filling sands of the inland ice ). The floodplains of the moderately winding to meandering streams are increasingly deepened down to about 7 meters. In the upper reaches, some sub-catchment areas of the Glane have been significantly changed by the creation of drainage channels and mill ditches. At the foot of the sandy alluvial fan in the south-west of the Teutoburg Forest, which is close to the groundwater, several bogs that are under nature protection have formed.
The surface catchment area of the Glane has a size of 354.025 km². Lower Saxony has 76.634 km² and North Rhine-Westphalia 277.391 km². The main hydrological strand of the Glane is formed by the Ladberger Mühlenbach with a catchment area of 182.187 km². That of the Eltingmühlenbach is just under 16 km² smaller at 166.342 km.
Course of the river code number
In the NRW register of waters, the main strand is assigned the code 334 and the name of the Glane lower course as a designation . The hydrographic main branch of the river system, however, is 35.8 km long and is downstream from the roll-call sections Uffelager Bach , Lienener Mühlebach , Ladbergen Mühlebach and Glane the longest at 54.8 kilometers flow path in this river system runs over Glaner Bach, Oedingberger Bach, Aa and Eltingmühlenbach (code 3346).
| Section | from kilometrage. |
Partial length km |
Total length km |
Catchment area km² |
to confluence |
Total length km |
Catchment area km² |
|
|---|---|---|---|---|---|---|---|---|
| Uffelager Bach | 35.118 | 4.893 | 4.893 | 7.453 | Brockbieke | 2.404 | 0.950 | |
| Lienen mill stream | 30.225 | 21.204 | 26.097 | 99.944 | Lengericher Aabach | 20,354 | 67.576 | |
| Ladberger Mühlenbach | 9.021 | 5,589 | 31.686 | 182.502 | Elting- mühlenbach |
51,344 | 166.341 | |
| Glane | 3.432 | 3.432 | 35.118 | 354,022 |
natural reserve
The floodplains of Glane, Eltingmühlenbach and Ladberger Mühlenbach are still in a relatively natural state in large sections. The meandering lowland sand brooks here again and again form sandbanks as well as impact and sliding slopes . The river beds, partially constrained by up to six meters high terrace edges, are lined with beech and oak forests. The largely natural sections of Glane and Mühlenbach are the most important in North Rhine-Westphalia. Therefore, 309 hectares of the ecologically high quality, typical sandy streams were designated as a protected area in the sense of the FFH directive ( FFH area Eltingmühlenbach , Natura 2000 -No. DE-3811-301). An 11 hectare part of the floodplain of the Ladberger Mühlenbach is also designated as a nature reserve ( nature reserve Ladberger Mühlenbach , identifier ST-049).
Earlier courses according to historical maps, names of places and waters
The original courses of water in the catchment area of the Glane, which have hardly been changed by canals and diversions, emerge from the maps of Le Coq (Sect. XIII, engraved in 1805). Only in the upper reaches of today's Eltingmühlenbach appears with the Edingberger Graben a straight watercourse, over which the northern arm of the Bever ( labeled as Bever Fl. (Uss)) has also received water from the Bever. It branches off to the right a little below where the Glaner Bach flows into the Bever. This northern Bever arm flows through the Beverbruch and then the place Schmedinghausen with the Eltings mill . Today the Glaner Bach merges into the Edingberger Graben and the Eltingmühlenbach without having reached the Bever beforehand.
The etymology of the hydronym has not been clarified beyond doubt. It could be derived from the Celtic word glana (i.e. pure, bright, clear, flowing; sand rivers mostly have clear water because of the filtering effect of the sand), similar to the French Glane , the Swiss Glâne or the Austrian Glan ; in addition, "Glan" was part of the name of the Celtic water god Glanus or Glanos. According to Hermann Jellinghaus, on the other hand, the name is of Germanic origin mainly because of its frequency .
Web links
Individual evidence
- ↑ a b Measurement based on the German basemap 1: 5000
- ↑ a b c d e f g h i Water directory of the State Office for Nature, Environment and Consumer Protection NRW 2010 (XLS; 4.67 MB) ( Notes )
- ↑ Landscape plan III Lienen ( Memento of the original from September 23, 2013 in the Internet Archive ) Info: The archive link has been inserted automatically and has not yet been checked. Please check the original and archive link according to the instructions and then remove this notice. (PDF; 1.1 MB)
- ↑ Water directory of the State Office for Nature, Environment and Consumer Protection NRW 2006 ( Memento from February 15, 2010 in the Internet Archive ) (PDF; 1.03 MB)
- ↑ Note: The determination of the main line (with the larger water flow in each case) is possible here by comparing the catchment areas in pairs at each confluence point, as the differences in climate and soil are not great.
- ↑ supplemented by subsequent measurements in TIM-online
- ↑ The designation in the water directory of the LaNUV Brockbieke for the uppermost section is obviously erroneous in view of the length information and can only refer to the Uffelager Bach, which is also supported by measuring the length online in TIM.
- ↑ Natura 2000 area "DE-3811-301 Eltingmühlenbach" in the specialist information system of the State Office for Nature, Environment and Consumer Protection in North Rhine-Westphalia
- ↑ Nature reserve "ST-049 Ladberger Mühlenbach" in the specialist information system of the State Office for Nature, Environment and Consumer Protection in North Rhine-Westphalia
- ↑ Illustration of the Kärntner Glan
- ^ Hermann Jellinghaus writes in village names around Osnabrück (Osnabrück 1922), p. 3 u. 15: “No part of old Germany between the Rhine and Elbe, i.e. precisely the area in which Celtic and Slavic place names have not yet been identified, has so many village names that defy reliable interpretation as the area of the Ems and its tributaries. … Glane , Kr. Iburg, originally part of Visbeck : Glana, Glano 1088 Glandorf: Glanathorpe 1070. From the Glane stream flowing into the Ems. The word has been declared Celtic. But then it would not be so common: Glane near Wildeshausen and Gronau, Glanhorst, Kr. Minden, Glanemeier near Barkhausen , Kr. Wittlage , the Glenne , Kr. Lippstadt, the Glenbach im Deister . "
