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Source Of The Red Main
The Red Main Spring (german: Rotmainquelle) is the source of the Red Main river, the left-hand and southern headstream of the River Main in Germany. It is located in the Lindenhardt Forest, ten kilometres south of Bayreuth near Hörlasreuth at a height of on the southern slopes of the Tannenberg (596 m). Although the Red Main is several kilometres longer than the Weiße Main, the stronger White Main Spring is seen as the source of the Main itself. The Red Main Spring was enclosed in stone in 1907 and, from there, the water flows along a narrow wooden pipe. The source region lies in the Franconian Switzerland-Veldenstein Forest Nature Park and belongs geologically to the Brown Jura. The river gets its name from the boggy red subsoil and the associated fluvial sediment that gives it its red appearance. In the vicinity of the Red Main Spring is the origin of the Fichtenohe, the upper course of the River Pegnitz The Pegnitz () is a river in Franconia in the German sta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rotmainquelle DSCF7667
The Red Main Spring (german: Rotmainquelle) is the source of the Red Main river, the left-hand and southern headstream of the River Main in Germany. It is located in the Lindenhardt Forest, ten kilometres south of Bayreuth near Hörlasreuth at a height of on the southern slopes of the Tannenberg (596 m). Although the Red Main is several kilometres longer than the Weiße Main, the stronger White Main Spring is seen as the source of the Main itself. The Red Main Spring was enclosed in stone in 1907 and, from there, the water flows along a narrow wooden pipe. The source region lies in the Franconian Switzerland-Veldenstein Forest Nature Park and belongs geologically to the Brown Jura. The river gets its name from the bog A bog or bogland is a wetland that accumulates peat as a deposit of dead plant materials often mosses, typically sphagnum moss. It is one of the four main types of wetlands. Other names for bogs include mire, mosses, quagmire, and muskeg; a ...g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Source
The headwaters of a river or stream is the farthest place in that river or stream from its estuary or downstream confluence with another river, as measured along the course of the river. It is also known as a river's source. Definition The United States Geological Survey (USGS) states that a river's "length may be considered to be the distance from the mouth to the most distant headwater source (irrespective of stream name), or from the mouth to the headwaters of the stream commonly known as the source stream". As an example of the second definition above, the USGS at times considers the Missouri River as a tributary of the Mississippi River. But it also follows the first definition above (along with virtually all other geographic authorities and publications) in using the combined Missouri—lower Mississippi length figure in lists of lengths of rivers around the world. Most rivers have numerous tributaries and change names often; it is customary to regard the longest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 long and descends a total of . 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. Sources The Red Main rises south of Bayreuth near Hörlasreuth (Creußen) in the Lindenhardt Forest at a height of . The source of the Red Main (''Rotmainquelle'') was impounded in stone in 1907, the water flows out of a small wooden pipe. Its source region lies in the Franconian Switzerland-Veldenstein Forest Nature Park. Geologically it belongs to the Brow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Main
The Main () is the longest tributary of the Rhine. It rises as the White Main in the Fichtel Mountains of northeastern Bavaria and flows west through central Germany for 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). Geography The Main flows through the north and north-west of the state of Bavaria then across southern Hesse; against the latter it demarcates a third state, Baden-Württemberg, east and west of Wertheim am Main, the northernmost town of that state. The upper end of its basin opposes that of the Danube where the watershed is recognised by natural biologists, sea salinity studies (and hydrology science more broadly) as the European Watershed. The Main begins near Kulmbach in Franconia at the joining of its two headstre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bayreuth
Bayreuth (, ; bar, Bareid) is a town in northern Bavaria, Germany, on the Red Main river in a valley between the Franconian Jura and the Fichtelgebirge Mountains. The town's roots date back to 1194. In the 21st century, it is the capital of Upper Franconia and has a population of 72,148 (2015). It hosts the annual Bayreuth Festival, at which performances of operas by the 19th-century German composer Richard Wagner are presented. History Middle Ages and Early Modern Period The town is believed to have been founded by the counts of Andechs probably around the mid-12th century,Mayer, Bernd and Rückel, Gert (2009). ''Bayreuth – Tours on Foot'', Heinrichs-Verlag, Bamberg, p.5, . but was first mentioned in 1194 as ''Baierrute'' in a document by Bishop Otto II of Bamberg. The syllable ''-rute'' may mean ''Rodung'' or "clearing", whilst ''Baier-'' indicates immigrants from the Bavarian region. Already documented earlier, were villages later merged into Bayreuth: Seulbitz (in 1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
White Main
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 Fichtelgebirge 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. Sources The source of the White Main is a wellspring located at 887 m above NN on the eastern slope of the Ochsenkopf. Margrave Frederick fixed it and had it enclosed in granite blocks in 1717. He also had the Hohenzollern coat-of-arms carved into the granite. Johann Wolfgang von Goethe visited the spring in 1785, but reckoned the Seehausbrunnen southeast of the Schneeberg as the source of the Main, for he wrote: "''...the source of the Main, which rises close to the house here and where the stream here amounts to a no ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
White Main Spring
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'' () 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 li ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Franconian Switzerland
Franconian Switzerland (german: Fränkische Schweiz) is an upland in Upper Franconia, Bavaria, Germany and a popular tourist retreat. Located between the River Pegnitz in the east and the south, the River Regnitz in the west and the River Main in the north, its relief, which reaches 600 metres in height, forms the northern part of the Franconian Jura (''Frankenjura''). Like several other mountainous landscapes in the German-speaking lands, e.g. Holstein Switzerland, Märkische Schweiz, or Pommersche Schweiz, Franconian Switzerland was given its name by Romantic artists and poets in the 19th century who compared the landscape to Switzerland. Franconian Switzerland is famous for its high density of traditional breweries. Name The region was once called ''Muggendorfer Gebürg'' (''Muggendorf hills''). The first tourists arrived during the age of Romanticism. Two law students of Erlangen University, Ludwig Tieck and Wilhelm Heinrich Wackenroder have been credited as "discoverers" o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Veldenstein Forest
The Veldenstein Forest (german: Veldensteiner Forst) lies in the east of the Franconian Switzerland-Veldenstein Forest Nature Park between the towns of Pegnitz and Plech. Its name is derived from Veldenstein Castle, a large, well preserved, medieval fortification above Neuhaus an der Pegnitz. The Veldenstein Forest, with its extensive pine and spruce woods has an area of around 70 km2 and is one of the largest contiguous areas of forest in Bavaria. A large part of the Veldenstein Forest lies on the territory of the district of Bayreuth and forms the fourth largest unincorporated area in Bavaria (55.60 km2). Sights A particular attraction in the Veldenstein Forest is the wildlife park. In the east the nature reserve of ''Pegnitzau zwischen Ranna und Michelfeld'' borders immediately on the forest. The forest also has numerous rock formations, caves and dolines, some of which are classified as natural monument A natural monument is a natural or natural/cultural f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brown Jura
The Brown Jurassic or Brown Jura (german: Brauner Jura or ''Braunjura'') in earth history refers to the middle of the three lithostratigraphic units of the South German Jurassic, the latter being understood not as a geographical, but a geological term in the sense of a lithostratigraphic super group. Formerly and even occasionally today in the popular scientific literature, this term is equated to the chronostratigraphic series of the Middle Jurassic. This is however not quite correct, because the Brown Jura does not exactly coincide with the chronostratigraphic boundaries of the Middle Jurassic. In addition, the term ''Dogger'', which was formerly frequently used (and sometimes is today) as a synonym should no longer be used in connexion with the South German Jurassic. Instead the term "Dogger" should be reserved for the roughly equivalent lithostratigraphic unit in the North German Jurassic. The Brown Jurassic was deposited about 175-161 million years ago. The Brown Jurassic f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
