Glane (Ems)

Mill Brook in Ladbergen, where the river is yet to be named Glane.

The Glane (water code 334 ) is an orographic right tributary of the Ems River south of Saerbeck in North Rhine -Westphalia, Germany. According to the waters Directory NRW, the river is 35.1 km long, where he is known only to the last 3.4 kilometers from the confluence of Ladbergen mill creek and Eltingmühlenbach Glane. In the upper reaches of the name -stretched Bach, Bach Uffelager, Lienener mill creek mill creek and Ladbergen be used in sections.

Geography

Course

The course description is followed by the deployment of the water code 334 from the source to the mouth of the Bach -stretched as Glane.

Stretched Bach and Bach Uffelager

The Glane arises as Recktenwald brook in Lower Saxony Bad Iburg about 1.2 km west of the city center on the southern flank of belonging to the Teutoburg Forest highlands at an altitude of 117 m above sea level. NN. The river first flows into southern directions and this happens Ostenfelde. Here the term applies to the west. After a total of 2.8 km of stream flow path crossed the border to North Rhine -Westphalia has changed its name for the first time.

The now Uffelager Bach called river continues to flow in southwestern directions. With the mouth of the Brookbieke for further 2.1 km flow path of the stream re-enters the name and is now called Lienener mill creek.

Lienener Mühlebachstrasse

As Lienener mill creek, often only briefly mill creek, the water now flows predominantly in western directions. After crossing under the Meckel Weger road to the mill brook flows through the nature reserve Flaaken, which he left at the south-west of Rethemeyer Kattenvenner road again. In Baumhöfener the creek flows past a large pond and takes its drain on. After crossing under the Warendorf path of the brook enters the wetland nature reserve on Bullerbach. After a flow distance of about 1200 m of stream leaves this again. After crossing under the K32 mill creek changed to reach the railway line pan - Eickelmann -Hamburg its course to the southwest. Approximately half-way water is knocked into a ditch, which flows south-west of the court Blömker in the peasantry Holzhausen in the Bullerbach. After the railway line was crossed the mill stream passes through the northern edge of a pond. With the mouth of Bull Erbach in the west of the pond of the river again changes his name.

Ladbergen Mühlebachstrasse

The now named as Ladbergen mill creek river continues to flow in a predominantly western directions and forms to approximately 800 m to the mouth of Bull Erbach the municipal boundary between Lengerich and Lengerich. West of silence reaches the mill brook, the border between Ladbergen and Lengerich, and thus the nature reserve Good Erpenbeck through which it flows at about 2.6 km in length. In this section the previously mentioned limit on the north bank runs. Continue westwards flowing passes under the mill creek State Road 475 and then reached the local situation of Ladbergen he 555 leaves again after the crossing under the main road. Just before the creek crosses the A1 motorway flows on the left side of the creek Berlemanns shaft. About 1 km after the crossing of the highway reaches the mill brook the Dortmund- Ems Canal. Before passing under a culvert on the right side opens the Ladbergen Aa.

Immediately after passing under the canal leaves the mill Bach The municipality of Ladbergen. First, the river for about 450 m forms the border between the north and Saerbeck Greven in the south. Then the river flows for a short distance in northwestern directions and touches through the territory of the airport Münster- Osnabrüch on its eastern border. With the achievement of the nature reserve Ladbergen mill creek, the river turns west again. After passing the new mill of the river to the mouth of the Ems forms in the boundary between Greven and Saerbeck. Approximately 3.4 km upstream of the estuary 's left side flows to the Eltingmühlenbach.

Glane

Below the confluence of the river is called Glane. Flowing in a northwesterly direction reaches the Glane after crossing the B219 the nature reserve Emsaue in which they the right side opens into the Ems after another 500 m stretch of river. The mouth is situated at an altitude of 36 m above sea level. NN. Thus, the difference in height between the source and mouth is about 81 m. With a length of 35.1 km results in an average bed slope of less than 0.5 ‰.

Inflows

The following table shows the named direct and indirect tributaries of the Glane be listed, as they are listed in the directory waters NRW. Section names are not listed.

Catchment area

The catchment area of ​​the Glane is in the Ostmünsterland southwest of the Teutoburg Forest. Its subsoil is predominantly sandy deposits of the Saale glaciation (pre-and Nachschüttsande of the inland ice ). In it the floodplains of moderately sinuous to meandering streams down the valley are increasingly deepened to about 7 meters. In the headwaters of several sub-basins of the Glane have been significantly altered by the installation of drainage canals and mill races. At the groundwater near foot of sandy alluvial fans in south-west of the Teutoburg Forest, several bogs have formed that are under nature protection.

The superficial catchment area of ​​the Glane has a size of 354.025 km ². In Lower Saxony account for 76.634 km ² and North Rhine-Westphalia 277.391 km ². The hydrological main strand of the Glane forms of Ladbergen mill stream with a 182.187 km ² Einzugsgebiegt. The smaller the Eltingmühlenbachs with 166.342 km to almost 16 km ².

Course of the river code

In waters directory NRW the umbilicus the code is assigned to 334, and as the name, the name of the lower reaches Glane. The hydrographic main branch of the river system, however, is 35.8 km long and consists downstream from the roll-call sections Uffelager Bach, Lienener mill creek, Ladbergen mill creek and Glane The longest 54.8 km flow path in this river system runs through Glaner Bach, Oedingberger Bach, Aa and Eltingmühlenbach ( code 3346 ).

Conservation

The floodplains of Glane, Eltingmühlenbach and Ladbergen mill creek are in large sections still in relatively near-natural state. The meandering lowland streams sand form here again and again from sandbanks and impact and Gleithänge. The partial of up to six meters high terrace edges constrained river beds are lined with beech and oak forests. The largely untouched sections of Glane and mill streams are considered the most important in North Rhine -Westphalia. Therefore were 309 acres of ecologically valuable, typical sand streams as a protected area for the purposes of the Habitats Directive ( FFH Eltingmühlenbach, Natura 2000 no. DE 3811 -301) reported. A 11 -acre portion of the floodplain of Ladbergen mill Bach is also designated as a nature reserve ( natural reserve Ladbergen mill creek, ID ST -049 ).

Earlier courses according to historical maps, local and waters name

The original, of canals and diversions hardly changed water courses in the catchment area of the Glane go from the card by Le Coq ( Sect. XIII, engraved 1805) produced. Appears only in the upper reaches of today's Eltingmühlenbaches with the Edingberger digging a straight stream, ( labeled as Bever Fl. ( Uss ) ) on the north arm of the apparently Bever additional water received from the Bever. It branches little below the mouth of the creek in the Glaner Bever to right. This Bever - north arm flows through the Beverbruch and then the place Schmedinghausen with the Eltings mill. Today, the Glaner stream enters the Edingberger ditch and the Eltingmühlenbach, without having previously obtained the Bever.

After the name of researcher Hermann Jellinghaus to the flow path Glaner Bach - Bach Oedingberger - Aa - Eltingmühlenbach - have been originally called Glane throughout the course Glane. It referred to the names:

• Glane for the source location in Bad Iburg
• Glandorf (1070 AD: Glanathorpe ) on Glaner Bach
• Epithet Glane village for the place Schmedehausen ( after the local mill with customs station of Schulze Elting is the stream named today. )
• Glane for the last stretch of the river below the junction with the Ladbergen Mühlebachstrasse

Over time, local names have been successful on the river.

The hydronym is etymologically not been unequivocally ascertained. It could be from the Celtic word glana (ie, pure, bright, clear, fluent, sand rivers have because of the filtering effect of the sand mostly clear water ) can be derived, similar to the French Glane, the Swiss Glane or Austrian Glan; also was " Glan " part of the name of the Celtic god of water Glanus or Glanos. After Hermann Jellinghaus the name is, however, mainly because of its frequency of Germanic origin.

A comprehensive name search in the course of earlier cartographic surveys was complicated by the fact that the upper course ran through the Kingdom of Hanover and the lower reaches of the province of Westphalia the Kingdom of Prussia.