The Red Main flows initially in a southeasterly direction, before it swings northeast and passes through Creußen. From there it heads almost due north and then turns west beyond Eremitage. It passes through the town of Bayreuth from east to west. In the town centre it has been confined since the 1970s in a concrete channel and partially covered. In the vicinity of the Bayreuth folk festival square the river divides into two branches. The southern branch is called the Mühlkanal, because it used to feed several mills within the town. Its water flow is held roughly constant by a weir and it runs above ground as far as the Münzgasse. Behind the former state central bank it disappears into a tunnel and surfaces again opposite the Graser School just before reuniting with the northern branch. In the late 1990s a section of the channel in Opernstraße was exposed and swept up as part of the rebuilding at the southern end of Luitpoldplatz. The northern arm usually carries only a small amount of water, but acts as a flood channel at times of high water and has a very wide river bed. It is partly covered by two car parks. Beyond Bayreuth the Red Main flows northwest in wide meanders through a broad valley, past the villages of Heinersreuth and Neudrossenfeld. South of Kulmbach, near Steinenhausen Castle, it is united with the White Main, which rises in the Fichtelgebirge mountains near Bischofsgrün. The Red Main is long, the White Main. At the confluence of the two headstreams a bridge was built in 2009 where the young Main may be crossed right at its beginning. Information boards on the bridge describe the rest of the river's course, the local walking and cycle routes and the surrounding countryside.
Bodenmühlwand geotope
In the vicinity of the Bodenmühle mill east of Bayreuth the Red Main has carved out a bluff on a bend in the river caused by erosion, the so-called Bodenmühlwand, a steep slope in height. This has exposed rock strata from the Middle Keuper period. Around 225 million years ago the area was a coastal region with frequent changes caused in the influence of land and sea. As a result, today, layers of claystone and Benker sandstone lie on top of each other. In the latter, geologists found fossils of ostracods, after which the layers are named, the remains of coelacanth as well as the scales, teeth and fin spines of prehistoric sharks. The highest and thickest rock layerbelongs to reed sandstones of the Carnian stage.
The Red Main Trail, which was laid out by Fichtelgebirge Club, begins near the source. This main footpath is marked by a red M on a white background throughout its length. Its 60 kilometre long route is as follows: Sourche of the Red Main-Creußen-Eimersmühle-Schlehenberg-Eremitage-Bayreuth-Martinsreuth-Altenplos-Grüngraben-Jöslein-Langenstadt-Affalterhof Katschenreuth-Steinenhausen Castle near Kulmbach. The Main-Mies Trail, established by the Upper Palatinate Forest Club also begins near the source. Here the trail is marked by at red diagonal cross on a white background. The 93 km long route is as follows: Source of the Red Main-Creußen-Seidwitz-Frankenberg-Neustadt am Kulm-Erbendorf-Falkenberg-Tirschenreuth-Griesbach.
