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the mountain range
Mountain range in Germany

The Fichtel Mountains (Fichtelgebirge, ) is a mountain range in Germany and the Czech Republic. They extend from the valley of the Red Main River in northeastern Bavaria to the Karlovy Vary Region in western Czech Republic. The Fichtel Mountains contain an important nature park, the Fichtel Mountain Nature Park. The Elster Mountains are a part of the Fichtel Mountains.

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. A folk etymology connecting the name Fichtelgebirge with the German word Fichte (meaning "spruce tree" or "pine tree") fails to account for the typically non spruce forests which predominated in the area at the time when the name Fichtelgebirge became established.

The Fichtel Mountains have an area of about The Czech part has an area of The Fichtel Mountain Nature Park in Germany has an area of
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 Luisenburg Rock Labyrinth. Other main settlements are Marktredwitz, Marktleuthen, Arzberg, Röslau, Weißenstadt, Waldershof, Kirchenlamitz and Tröstau (all on the upper reaches of the Ohře 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 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.

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.

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.

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 about 5 million years ago: an earlier formed Franconian fault line came under pressure again and the Fichtel Mountains, Franconian Forest, the Münchberg Gneiss Massif and the northern Upper Palatine Forest were uplifted along it. This last uplift gave the forces of erosion more to do again and the rivers cut deeply into the already, almost levelled, mountain range. So the present day structure was created from a plateau: a low mountain range which is being gnawed away at on all sides, with a long and varied history. Although often difficult to interpret, it is an 'Eldorado' for geologists from a wide range of specialisms.

The Huguenots introduced the Easter decorations on wells, so called Osterbrunnen, in the shape of a lily (emblem of the Bourbon kings) (as described e. g. in the April 2007 of the Fränkische Post).

There are many places in the Fichtel Mountains that still produce glassware at competitive prices. The porcelain industry, centred on the town of Selb, is internationally renowned and the foremost in Germany. Local firms such as Rosenthal and Hutschenreuther are of international standing. Tourism is the main source of income for many places in the Fichtel Mountains today. In some towns such as Bischofsgrün tourism has a long tradition going back to the 1920s. After the Second World War the stream of holidaymakers increased sharply, both in summer for walking and in winter for winter sports. The Fichtel Mountains became the local mountain range (Hausgebirge) for (West )Berliners who, unable to holiday in East Germany, were able to get there on the transit route of the A 9 motorway. This has changed since German reunification and the opening up of other mountainous holiday areas. The Fichtel Mountains are a nationally important holiday destination in winter. Several lifts, the longest being two chair lifts on the Ochsenkopf, but also a plethora of cut cross country trails are the mainstay of this industry. The Fichtel Mountains attract many tourists throughout the year. In the winter the mountains are a common destination for people seeking outdoor recreational sports like alpine skiing, cross country skiing, and sledding. The warmer summer months find people mountain biking, hiking, and sight seeing amongst the many large rock formations.

Naturpark Fichtelgebirge and Naturpark Steinwald. Walking map with tourist tips, coloured path marking and car parks for walkers Official walking map of the Fichtelgebirge Club and Fichtel Mountains Nature Park 1:50.000 16th edn. Fritsch Landkarten Verlag Hof (Fritsch Karten: No. 52) o. J.,