The White Main (German: Weißer Main or Weißmain, not to be confused with the Weismain), is the larger and shorter of the two headstreams of the river Main. It rises in the Fichtel Mountains and merges near Steinenhausen, southwest of Kulmbach, with the left-hand, southern headstream, the Red Main, to form the Main. The length of the White Main is 51.7 km. The source of the White Main lies on light granite rock, which lends it its white colouration.
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👉 White Main in the context of Main (river)
The Main (German pronunciation: [ˈmaɪn] ) is the longest tributary of the Rhine, one of the major European rivers. It rises as the White Main in the Fichtel Mountains of northeastern Bavaria and flows west through central Germany for 525 kilometres (326 mi) to meet the Rhine below Rüsselsheim, Hesse. The cities of Mainz and Wiesbaden are close to the confluence.
The largest cities on the Main are Frankfurt am Main, Offenbach am Main and Würzburg. It is the longest river lying entirely in Germany (if the Weser-Werra are considered separate).
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White Main in the context of Red Main
The Red Main (German: Roter Main or Rotmain) is a river in southern Germany. It is the southern, left headstream of the river Main. It rises in the hills of Franconian Switzerland, near Haag and flows generally northwest through the towns Creußen, Bayreuth, Heinersreuth and Neudrossenfeld. It merges with the White Main near Kulmbach to form the Main. The Red Main is 72 kilometres (45 mi) long and descends a total of 283 metres (928 ft).
The waters of the Red Main flow through a region of clayey soils, which is why the river carries a lot of suspended solids, especially after rainfall, and acquires a red-brown colour, hence the name Red Main.
White Main in the context of Source of the White Main
The White Main Spring (German: Weißmainquelle) is the source of the White Main river, the right-hand and northern headstream of the River Main, a major tributary of the Rhine in Germany. It is located at a height of 887 metres above sea level on the eastern slopes of the Ochsenkopf mountain and is viewed as the source of the Main, even though the Red Main is several kilometres longer. Usually the White Main Spring is stronger (i.e. has a higher volumetric flow) than the Red Main Spring.
Margrave Frederick of Brandenburg had it traced in 1717 and impounded in granite blocks bearing the Hohenzollern coat of arms. The spring bears the name Fürstenbrunnen ("Prince's Well"), but is not to be confused with the Upper and Lower Fürstenbrunnen on the Ochsenkopf. By contrast, in 1785 Goethe considered the Seehausbrunnen (50°01′57″N 11°52′18″E / 50.0324418°N 11.871652°E) southeast of the Schneeberg as the source of the Main and wrote: "the source of the Main, which rises right by the house here and makes the brook look like a tin wash".