Fichtelgebirge

The Fichtel MountainsRandlesome, C. et al. (2011). ''Business Cultures in Europe'', 2nd ed., Routledge, Abingdon and New York, p. 52. . (german: Fichtelgebirge, cs, Smrčiny), form a small horseshoe-shaped mountain range in northeastern Bavaria, Germany. They extend from the valley of the Red Main River to the Czech border, a few foothills spilling over into the Czech Republic. They continue in a northeasterly direction as the Elster Mountains, and in a southeasterly direction as the Upper Palatine Forest. The Fichtel Mountains contain an important nature park, the Fichtel Mountain Nature Park, with an area of .

Etymology

The first person to write about the Fichtel Mountains, Matthias of Kemnath (actually Matthias Widmann, born 23 February 1429 in Kemnath) reported in 1476: ''Ein bergk, hoch, weitt, wolbekant ligt in Beiern, gnant der Fichtelberg'' ("A mountain, high, wide and well-known, lies in Bavaria, known as the Fichtelberg"). In descriptions of the border in 1499 and 1536, the mountain that is now called the Ochsenkopf was called ''Vichtelberg''; thereafter the name was extended to the whole mountain region. It is also mentioned in old documents: around 1317 the lords of Hirschberg were enfeoffed ''inter alia'' with the ''walt zu dem Vythenberge''. By the 14th century iron ore was being extracted in the ''St. Veith'' Pit on the southern foot of the mountain. ''Vyth → Veit → Fichtel''. High-profile local history and name researchers have still not had the last word.

Geography

The Fichtel Mountains lie between the towns of Hof and Weiden. In the west there is a good transport link to the nearby city of Bayreuth.

The county town in the heart of the Fichtel Mountains is Wunsiedel with its famous Luisenburg Rock Labyrinth. Other main settlements are Marktredwitz, Marktleuthen, Arzberg, Röslau, Weißenstadt, Waldershof, Kirchenlamitz and Tröstau (all on the upper reaches of the Ohře/ Eger and the Röslau rivers). The largest settlement in the Czech part of the Fichtel Mountains is Aš.

Further to the southeast and south are Bischofsgrün, Fichtelberg, Mehlmeisel, Nagel, Neusorg, Speichersdorf, Kemnath, Erbendorf, Wiesau and Fuchsmühl, in the west are Weidenberg, Creußen, Bayreuth, Goldkronach, Bindlach and Bad Berneck, in the northwest are Gefrees, Zell im Fichtelgebirge, Weißdorf, Münchberg (Obere Saale), and in the north Selb, Rehau and Hof.

The boundary between the (East) Franconian dialect in the north and west and the (North) Bavarian and Upper Palatine dialects in the east and south runs diagonally through the Fichtel from northeast to southwest. This language border does not coincide with the administrative boundary of Upper Franconia and the Upper Palatinate, but, for example, Bavarian is also spoken in the Upper Franconian district of Wunsiedel.
Moreover, there are descendants of those who, after the World War II came from Bohemia, Moravia, Silesia and East Prussia into the Fichtel Mountains, and who make up a significant percentage of the population.

Geomorphology

In terms of geomorphological division of Germany, the Fichtel Mountains forms a major natural region called the Thuringian-Franconian Highlands (no. D48 and 39) together with the Thuringian Forest, Thuringian Highland and Franconian Forest. In terms of geomorphological division of the Czech Republic, the Fichtel Mountains is a mesoregion within the Ore Mountains Highlands together with Ore Mountains and Elbe Sandstone Mountains.

Geomorphologically the Fichtel Mountains are a horseshoe-shaped massif consisting of several linked ridges, hence the term Fichtel Mountain Horseshoe (''Fichtelgebirgs-Hufeisen''). The most important are the:

* High Fichtel with the Schneeberg, Ochsenkopf and Kösseine massif,
* Northern ridge of Waldstein including the mountains of Großer Waldstein, Epprechtstein and Kornberg
* Southern section with its Steinwald and Reichsforst forests and the Kohlberg mountain
* Inner Fichtel Plateau.

To the northeast the Fichtel Mountains transitions into the Elster Mountains and the Ore Mountains, to the southeast is the Upper Palatine Forest, the Bohemian Forest and the Bavarian Forest. To the northwest is a clear geological divide with the Franconian and Thuringian Forests. To the southwest it descends to the morphologically very different Franconian fault-block landscape.

In early times the Fichtel was known as the 'navel of Germany' (''Nabel Deutschlands'') or the 'wellspring of Europe' (''Herzbrunnen Europas'') because four important rivers rise here and flow in four different directions of the compass:

* to the north flows the Saxon Saale
* to the east flows the Ohře, known here as the Eger and its tributary, the Röslau
* to the south two headstreams of the Naab: the Fichtelnaab in the centre and the Haidenaab to one side
* to the west the White Main
Numerous moors and marshes, which are now protected, are valuable water collectors. The European watershed from the North Sea to the Black Sea runs over these mountains.

Mountains and hills

The highest mountain is the Schneeberg at . Rivers rising from the Fichtel Mountains are the White Main, the Saxon Saale, the Ohře/Eger and the Fichtelnaab which later joins the Waldnaab. Major towns on the edge of the mountain region are Bayreuth and Hof.

While the mountains dip gradually away to the north and the south, they form a steep slope in the west where the Red Main forms the boundary of the mountains.

The Ochsenkopf ("Ox Head") is the second highest mountain of the Fichtel Mountains, at . There are two chair-lifts to the summit, one from Bischofsgrün in the north and one from Fleckl in the south. The "Asenturm" (Æsir Tower) is an observation tower on the summit with a restaurant attached.

The following are the highest and best-known mountains in the Fichtel Mountains (listed with heights in metres (m) above sea level (NN):

Geology

Early mountain building

Geologically the Fichtel massif consists mainly of granite. The history of its orogeny begins in the Precambrian Eon about 750–800 million years ago. From that time only the truncated uplands of the once-towering mountain chain are left.

Subsequently, the area was covered by sea, and rivers transported sediments from the old eroding mountains on the coast. These sediments were deposited as layers of clay, sand and limestone.

At the beginning of the Cambrian Period, about 570 million years ago, these beds were folded and raised up to form new mountains. High temperatures and pressure during this mountain folding process, which lasted into the Upper Carboniferous Period, created metamorphic rock. The shale layers were transformed into phyllites and schists, sandstones metamorphosed into quartzite and limestone produced Wunsiedel marble. These mountains, which may have been several kilometres high, were also eroded to sea level again.

Variscan orogeny: mountains from the depths of the sea

In the next phase, great, deep-sea sediments were laid down under the present-day Fichtel Mountains and the Franconian Forest from the Silurian, Devonian and Lower Carboniferous periods; these are especially well recorded in the Franconian Forest, whose rocks were only subject to very low-grade metamorphism (associated with volcanism and ore formation) and which contain easily dated fossils. Finally, in the Upper Carboniferous period 285 million years ago, the Hercynian mountain building phase began and raised the Fichtel Mountains, Franconian Forest and Münchberg gneiss plateau into high mountains – like almost all the fold mountains formed during the Hercynian period.
This mountain building episode was the ''Variscan orogeny'', named after Hof's Latin name (and the tribe of Varisci) of ''Curia variscorum''. At the same time, magma intruded in several phases into the folds, where it solidified under the Earth's surface into the present-day granites. As granite formed, secondary rocks were only affected by slight contact metamorphism. The rest of the molten rock with its ore-containing fluids formed pegmatite, as well as veins of ore and minerals – the basis of the medieval mining industry and early industrialisation of this region.

During the Upper Carboniferous and Lower Permian (''Rotliegendes'') large quantities of rock debris were deposited in intramontane basins and onto the foreland of the mountain range. These basins were formed by extensional tectonics which were accompanied by an intermediate to acidic volcanism. The sediments of the ''Rotliegendes'' are only exposed in a few places, but have been confirmed across a wide area by drilling beneath the platform southwest of the Franconian Line. Late Variscan volcanic rocks occur in the Fichtel Mountains as layers of rhyolite.

Alpine orogeny creates new pressures

In the neogene (Upper Tertiary beginning 26 million years ago) period, tectonic activity increased again – just as the Alpine orogeny (Alps, Carpathians etc.) slowly came to an end. In that time, parts of this and other older massifs (such as the Bohemian-Moravian Highlands or Bohemian Massif in the Alpine foothills) sometimes ended up underneath younger rock. In the Upper Miocene (10 million years ago), molten basalt broke through in northern Upper Palatinate as the Eger Graben was being formed. Through erosion, the remains of former diatremes have been uncovered and may be seen e.g. on the Rauher Kulm or at Parkstein near Weiden. Basaltic surface layers, i.e. extensive flows of low-viscosity lava, are visible e. g. on the Teichelberg near Pechbrunn. These basaltic nappes should not however be confused with the formation of tectonic layers.

The formation of the present landscape finally took place in the younger Pliocene

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