Aula (river)

BW

Geography

The small river formed about 2 miles north-west of Upper Aula Knüllgebirge by the confluence of the creek Salzer ( Salzer Born source ) with the Hollenbach to 372 m above sea level. NN. The Hollenbach from Mount Tall tree ( 563 m above sea level. NN ) at 483 m above sea level. NN and submit to the union with the Salzer Bach 1.6 km back. The latter is 1.3 km long and originates at Lotterberg ( 463 m above sea level. NN ) to 442 m above sea level. NN.

The auditorium first flows in an easterly direction and is a short distance to turn to the southeast. It flows through the upper hall, where their left Easter brook flows. After upper auditorium, the auditorium turns into a sharp bend to the east. In the bend flows right of the houses Bach.

On their way to the east flows through the auditorium Wahlshausen, takes the left side Berschbach and flows south past Gersdorf, Frielingen and Heddersdorf. Here she takes on the flowing of the north Kisselbach and turns its course south again. It flows through Kirchheim and takes shortly after the city's right accruing to Ibra.

Later she crosses the A7 and reaches the community Niederaula. There flows the east past the hamlet Kleba and takes just before the nucleus Niederaula on the right flowing, coming from the west, had Bach. After Kleba the auditorium Viaduct of the high-speed line Hannover -Würzburg spans the auditorium.

Then it flows west past Niederaula to at 206 m above sea. NN to open into the Fulda. On its 20 km long path the auditorium has overcome a height difference of 166 m.

Tributaries

The following are the tributaries of the Great Hall are listed by their formation (372 m above sea level. NN ) to the mouth (216 m above sea level. NN ) in the Fulda.: ( Hyphens added for better overview and to sort downriver are in the DGKZ digits after the 4256 - - Aula! )

Natural areas

The middle reaches of the hall is the natural area roughly the boundary between the crumpled (main unit 356 ) in the north and the south followed Fulda Haune - plateau (355). Within the last main unit in turn separates the lower reaches from about Heddersdorf the Ottrauer Bergland ( 355.0; on the right, so first south, then west ) from Kirchheimer Bergland ( 355.4, left).

The tributaries of the auditorium spring z.T. on the slopes of the most prominent mountains of crumpled and its southern slopes, in particular:

• The Kisselbach originates from the eastern slope of the Eisenberg, at 636 meters the highest mountain of crumpled and eastern side center.
• The Ibra rises on the northeast slope of the 592 m high Rimberges, a striking Südausläufers the volcanic activity of the crumpled into Ottrauer Bergland, who, he would expect to crumpled, still the third highest mountain alone would be there.
• The Osterbach rises on the northern slope of the 492 meter high Nöll 's southern Hochknüll.
• The houses creek and its tributaries originate from the north-eastern slope of the 533 m high the limestone, the southernmost mountain of crumpled, the " connects " the Hochknüll with the Rimberg.