105:
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formation, Wolfstein, Hohenstein, Ochsenkopf, Hundslohe and
Gregnitz valley; on the Kornberg: the Wolfsgarten forest and the south-southwestern part of the Großer Kornberg; relatively coarse, has an unusual appearance due to the blue feldspar, black biotite and richly sprinkled dark foreign bodies; Wolfsgarten Granite is somewhat lighter blue.
1799:
There are numerous pockets of Kösseine
Granite containing hornfels, cm-large biotite-rich shreds and nodules of host rock, rounded or round quartz-feldspar rich pockets on the Kösseine massif: narrow band on the north, east and southern edge, small labyrinth, Kleinwendern quarry, Hirschensprung rock
1883:
ore deposits were discovered. The metals were worked in hammer mills (hence the many place names ending with -hammer) on the
Fichtel's rivers, in furnaces and at metalsmiths. The forests of the Fichtel Mountains supplied the wood necessary for the manufacture of charcoal. During the
1833:
between the
Steinwald Granite and the Falkenberg Porphyritic Granite; it forms the basement of the Pechbrunn basalt region and surfaces there at various places between the basalt nappes; porphyritic structure, especially rich in feldspar
2041:
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.
1395:
1806:
is restricted to the central massif and occurs on the
Rudolfstein, on the Drei Brüder almost to the summit of the Schneeberg, western slope of the Seehügel, between Seehügel and Platte, Fuchsbau and Zufurt west of
1782:
occurs on the Kösseine, including the
Burgstein, Haberstein and Schauerberg, and the southern part of the Großer Kornberg massif; small- to medium-grained, porphyritic structure weak or missing; low in
723:
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
2532:
Dietmar
Herrmann: "Rund um den Großen Waldstein im Fichtelgebirge", Heft 16/2008 der FGV-Schriftenreihe Das Fichtelgebirge, HG: Fichtelgebirgsverein, Theresienstraße 2, 95632 Wunsiedel
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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
370:("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
1601:
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
1752:
occurs in all the prominent massifs of the Fichtel Mountains (the Ochsenkopf, the southern part of the Schneeberg and the Haberstein, the Platte to the Hohe Matze, the
1024:
The Ochsenkopf ("Ox Head") is the second highest mountain of the Fichtel Mountains, at 1,024 metres (3,360 ft). There are two chair-lifts to the summit, one from
812:
2026:
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 (
1605:: 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
543:
The Fichtel Mountains have an area of about 1,600 square kilometres (620 sq mi). The Czech part has an area of 289 km (112 sq mi). The
3631:
1746:
triangle; medium- and also fine-grained, its variable mineral composition produces colourations from light grey, dark grey and dark green-grey to almost black.
1021:
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.
3139:
1817:
of the Steinwald massif: in the western part of the Steinwald, e. g. on the Dachsfelsen, and the northwestern part of the Grandfelsen; small-grained.
378:; 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
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1632:) and its derivatives make up about 40% of the area – its impact being all the more striking because this very hard, yet hydrous, rock forms the highest
137:
413:(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
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2003:
There are many places in the Fichtel Mountains that still produce glassware at competitive prices. The porcelain industry, centred on the town of
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2705:
1450:) large quantities of rock debris were deposited in intramontane basins and onto the foreland of the mountain range. These basins were formed by
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block and on the eastern perimeter of the Schneeberg; it forms outcrops of in the shape of numerous rock formations; medium- to coarse-grained.
1410:, where it solidified under the Earth's surface into the present-day granites. As granite formed, secondary rocks were only affected by slight
731:, but, for example, Bavarian is also spoken in the Upper Franconian district of Wunsiedel. Moreover, there are descendants of those who, after
735:
came from Bohemia, Moravia, Silesia and East Prussia into the Fichtel Mountains, and who make up a significant percentage of the population.
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occurs in just two small outcrops near Holzmühl, 3 km southeast of Marktleuthen and near Längenau on the Wartberg, east-northeast of
3134:
2529:
Heft 11 und 12 der Schriftenreihe „Beiträge zur Geschichts- und Landeskunde des Fichtelgebirges“, Verlag Buchhandlung Kohler, Wunsiedel
1029:
1706:
Granite (found northeast of the upper massif near Schwarzenhammer and running through the Selb Forest and the Czech Republic into
503:
362:
The first person to write about the Fichtel Mountains, Matthias of Kemnath (actually Matthias Widmann, born 23 February 1429 in
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occurs in the centre, including the Weißenstein, Platte, Katzentrögel, Reiseneggerfelsen and Hackelstein; coarse-grained.
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The following are the highest and best-known mountains in the Fichtel Mountains (listed with heights in metres (m) above
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301:
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271:
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1969:
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periods; these are especially well recorded in the Franconian Forest, whose rocks were only subject to very low-grade
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341:
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2030:) for (West-)Berliners who, unable to holiday in East Germany, were able to get there on the transit route of the
1984:
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987:
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80:
17:
2595:. (Dissertationsschrift.) Forstliche Forschungsberichte München, Nr. 167. Frank, München 1998, 297 (VII/XI) S.
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forests. To the southwest it descends to the morphologically very different Franconian fault-block landscape.
471:
290:
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Walking map with tourist tips, coloured path marking and car parks for walkers.. Official walking map of the
2829:
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Dietmar Herrmann: "Der Ochsenkopf im Fichtelgebirge", Heft 17/2009 der FGV-Schriftenreihe Das Fichtelgebirge
1341:
In the next phase, great, deep-sea sediments were laid down under the present-day Fichtel Mountains and the
2854:
2018:
Tourism is the main source of income for many places in the Fichtel Mountains today. In some towns such as
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the mining industry became depressed and the ore deposits were largely exhausted. In the 18th century
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Period, about 570 million years ago, these beds were folded and raised up to form new mountains. High
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are only exposed in a few places, but have been confirmed across a wide area by drilling beneath the
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station has rail services to Eger, Regensburg, Nuremberg, Munich, Hof, Bayreuth, Dresden and Leipzig
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in the area. Its stark appearance and the early emergency of industry here have made their mark on
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Europe's Green Revolution and its Successors: The Rise and Fall of Peasant-Friendly Plant Breeding
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Numerous moors and marshes, which are now protected, are valuable water collectors. The European
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927:) because four important rivers rise here and flow in four different directions of the compass:
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etc.) slowly came to an end. In that time, parts of this and other older massifs (such as the
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from the old eroding mountains on the coast. These sediments were deposited as layers of
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in western Czech Republic. The Fichtel Mountains contain an important nature park, the
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In terms of geomorphological division of Germany, the Fichtel Mountains forms a major
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1811:; very even, medium grain; little biotite, a lot of muscovite; lighter, brighter hue.
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1313:. These mountains, which may have been several kilometres high, were also eroded to
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394:. High-profile local-history and name researchers have still not had the last word.
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An insight into the history of mining in the Fichtel Mountains may be gained from:
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at 1,051 metres (3,448 ft). Rivers rising from the Fichtel Mountains are the
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1:50.000 16th edn. Fritsch Landkarten-Verlag Hof (Fritsch Karten: No. 52) o. J.,
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2012:
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man had begun to mine in the Fichtel Mountains. The most important products were
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This article is about the mountain range. For the asteroid named after them, see
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Fichtelgebirge, Frankenwald, Coburger Land. Vom Oberen Maintal bis zum Vogtland.
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2103:
2019:
1724:; medium-grained with a higher biotite content, unevenly grained microstructure.
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consisting of several linked ridges, hence the term Fichtel Mountain Horseshoe (
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2007:, is internationally renowned and the foremost in Germany. Local firms such as
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tried to revive the mining industry again. Many towns and villages (e. g.
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rivers). The largest settlement in the Czech part of the Fichtel Mountains is
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formed during the Hercynian period. This mountain building episode was the
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Ein bergk, hoch, weitt, wolbekant ligt in Beiern, gnant der Fichtelberg
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phase began and raised the Fichtel Mountains, Franconian Forest and
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1948:
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558:. In the west there is a good transport link to the nearby city of
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Fichtelgebirge-Frankenwald-Steinwald. Die schönsten Ausflugsziele.
2601:
HB-Verlags- und Vertriebsgesellschaft 1998 (HB Bildatlas: H.190),
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Goldstadtverlag, Pforzheim 2002 (Goldstadt Reiseführer Bd. 318),
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1554:. Basaltic surface layers, i.e. extensive flows of low-viscosity
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tourism has a long tradition going back to the 1920s. After the
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In early times the Fichtel was known as the 'navel of Germany' (
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in Germany has an area of 1,020 km (390 sq mi).
87:
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1406:. At the same time, magma intruded in several phases into the
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Eon about 750–800 million years ago. From that time only the
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Official presentation of Czech part of the Fichtel Mountains
2565:
Mit Kindern im Fichtelgebirge. Wo Wandern zum Erlebnis wird.
2088:
892:
To the northeast the Fichtel Mountains transitions into the
614:
63:
The Schneeberg (left) and the Ochsenkopf (right), seen from
3219:
3195:
2824:
2248:
2065:, and sight seeing amongst the many large rock formations.
2004:
1856:
1848:
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1526:) sometimes ended up underneath younger rock. In the Upper
1507:
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1255:
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Fichtel Mountains within the division of the Czech Republic
701:
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1422:, as well as veins of ore and minerals – the basis of the
386:. By the 14th century iron ore was being extracted in the
3267:
1852:
1542:
was being formed. Through erosion, the remains of former
1415:
1362:
908:. To the northwest is a clear geological divide with the
565:
The county town in the heart of the Fichtel Mountains is
2706:
The Fichtelgebirge, described by a resident of Franconia
2537:
Fichtelgebirge. Streifzüge durch das granitene Hufeisen
2038:
and the opening up of other mountainous holiday areas.
1760:); its groundmass is small-grained with phenocrysts of
1485:
1951:
introduced the Easter decorations on wells, so-called
1337:
Variscan orogeny: mountains from the depths of the sea
941:, known here as the Eger and its tributary, the Röslau
1585:
came under pressure again and the Fichtel Mountains,
1566:
should not however be confused with the formation of
1010:. Major towns on the edge of the mountain region are
2577:
Gerhard Bayerl, Manfred Schultes, Bernhard Settwon:
2468:, 2nd ed., Routledge, Abingdon and New York, p. 52.
1454:
which were accompanied by an intermediate to acidic
1324:
Typical granite rocks in the Fichtel Mountains: the
827:
are the northwestern part of the Fichtel Mountains.
2613:
Fichtelgebirge. Steinwald. Bayreuth, Kulmbach, Hof.
2514:. Ellwanger Verlag, Bayreuth 2009 (twote Auflage).
2419:
A description of the minerals in the Leskean Museum
1959:kings) (as described e.g. in the April 2007 of the
2567:Fleischhauer & Spohn Verlag, Bietigheim 1994,
2434:, Butterick, Frederick A. Stokes, New York, p. 82.
1384:plateau into high mountains – like almost all the
2678:Naturpark Fichtelgebirge and Naturpark Steinwald.
1938:the local heritage and mining museum in Erbendorf
1558:, are visible e. g. on the Teichelberg near
358:Characteristic landscape in the Fichtel Mountains
3678:
1935:the mining industry information point at Arzberg
1546:have been uncovered and may be seen e.g. on the
1789:is found in the central Fichtelberg/Ochsenkopf/
1702:is, by contrast, finer with a bluish-grey hue.
1246:Subsequently, the area was covered by sea, and
805:geomorphological division of the Czech Republic
550:The Fichtel Mountains lie between the towns of
2954:
1908:) owe their emergence to the mining industry.
1243:of the once-towering mountain chain are left.
27:"Fichtel" redirects here. For other uses, see
2940:
2784:
1581:about 5 million years ago: an earlier-formed
833:the Fichtel Mountains are a horseshoe-shaped
2487:"Česko: Geomorfologické celky podle rozlohy"
1654:/Liebenstein massif (including the towns of
1478:occur in the Fichtel Mountains as layers of
539:View of the Fichtel Mountains from Waldstein
2400:, Routledge, Abingdon and New York, p. 47.
1919:of Gleissinger Fels near Fichtelberg-Neubau
459:. Unsourced material may be challenged and
278:. Unsourced material may be challenged and
2947:
2933:
2791:
2777:
1365:formation) and which contain easily dated
1207:
1040:on the summit with a restaurant attached.
390:Pit on the southern foot of the mountain.
109:The Fichtel Mountains in northeast Bavaria
2657:Oberfränkische Verlagsanstalt, Hof 1983,
2653:Friedrich Wilhelm Singer, Georg Pöhlein:
1612:
523:Learn how and when to remove this message
342:Learn how and when to remove this message
2072:
2057:. The warmer summer months find people
1955:, in the shape of a lily (emblem of the
1498:beginning 26 million years ago) period,
1319:
1211:
774:
766:
758:
750:
742:
534:
353:
2655:Fichtelgebirge. Das granitene Hufeisen.
2593:Die Forstgeschichte des Fichtelgebirges
1922:the Schmutzler gallery near Goldkronach
1502:activity increased again – just as the
1414:. The rest of the molten rock with its
620:Further to the southeast and south are
14:
3679:
2753:Homepage of the 'Fichtelgebirgsverein'
2714:Official Fichtelgebirge tourist portal
2625:Godehard Schramm, Bernd-Heinz Häuser:
2512:Das Fichtelgebirge im Luftbildportrait
1998:
1797:Kösseine and Wolfsgarten Kern Granite.
1227:the Fichtel massif consists mainly of
981:
719:in the north and west and the (North)
2928:
2808:Mountain ranges of the Czech Republic
2772:
1925:the gold mining museum in Goldkronach
236:are a part of the Fichtel Mountains.
216:. They extend from the valley of the
1486:Alpine orogeny creates new pressures
944:to the south two headstreams of the
848:with the Schneeberg, Ochsenkopf and
457:adding citations to reliable sources
424:
276:adding citations to reliable sources
243:
1879:, clay and peat). In earlier times
1176:Highest mountain of the Czech part
791:(no. D48 and 39) together with the
24:
2639:Reinhard Feldrapp, Günter Hertel:
2489:(in Czech). Treking.cz. 2009-12-15
1838:
1714:) is fine-grained, but grey again.
1609:from a wide range of specialisms.
1597:were uplifted along it. This last
1577:finally took place in the younger
1373:period 285 million years ago, the
25:
3703:
2699:
2535:Reinhard Feldrapp, Bernd Häuser:
2034:motorway. This has changed since
923:) or the 'wellspring of Europe' (
605:(all on the upper reaches of the
3665:
2913:
2800:
1983:
1968:
1305:, sandstones metamorphosed into
738:
700:(Obere Saale), and in the north
429:
248:
103:
57:
2761:Fichtel Mountains in Oberfanken
2077:Places in the Fichtel Mountains
2015:are of international standing.
1593:Gneiss Massif and the northern
1530:(10 million years ago), molten
1361:(associated with volcanism and
1285:process, which lasted into the
1072:Former Cold War listening post
841:). The most important are the:
789:Thuringian-Franconian Highlands
177:Thuringian-Franconian Highlands
2722:Fichtelgebirge holiday country
2629:Rosenheimer Verlagshaus 1992,
2527:Vom Bergbau im Fichtelgebirge.
2479:
2464:Randlesome, C. et al. (2011).
2458:
2437:
2424:
2411:
2390:
2068:
1032:in the south. The "Asenturm" (
13:
1:
2686:Fichtel Mountains Nature Park
2563:Reinhard Müller, Horst Ruhl:
2447:, Sterling, New York, p. 48.
2383:
2320:
1942:
1928:the mining exhibition in the
1859:, minerals, earths and rock (
1573:The formation of the present
1398:Latin name (and the tribe of
1297:layers were transformed into
931:to the north flows the Saxon
807:, the Fichtel Mountains is a
573:. Other main settlements are
2643:. H. Stürtz, Würzburg 1984,
1750:Rand Granite (Dach Granite)
986:The highest mountain is the
545:Fichtel Mountain Nature Park
420:
239:
230:Fichtel Mountain Nature Park
92:1,051 m (3,448 ft)
7:
2466:Business Cultures in Europe
2144:Höchstädt im Fichtelgebirge
1772:, sometimes sprinkled with
1516:Bohemian-Moravian Highlands
1375:Hercynian mountain building
978:runs over these mountains.
859:including the mountains of
10:
3708:
3692:Mountain ranges of Bavaria
3591:Thuringian Slate Mountains
2581:Druckhaus Oberpfalz 2000,
2579:Steinmeer und Siebenstern.
2504:
2421:, Mercier, Dublin, p. 493.
1534:broke through in northern
1418:-containing fluids formed
1202:
1028:in the north and one from
896:, to the southeast is the
873:Southern section with its
33:
26:
3663:
3567:Teutoburg Forest (Osning)
2963:
2911:
2890:Moravian-Silesian Beskids
2815:
2553:. Ackermann-Verlag, Hof,
2443:Schumann, Walter (2008).
1662:) and extending into the
1220:, on the Großer Waldstein
771:Source of the Fichtelnaab
717:(East) Franconian dialect
715:The boundary between the
571:Luisenburg Rock Labyrinth
168:
129:
115:
101:
96:
86:
76:
71:
56:
51:
46:
41:Mountain range in Germany
3077:Elbe Sandstone Mountains
2969:Anterior Bavarian Forest
2840:Elbe Sandstone Mountains
2830:Central Bohemian Uplands
2430:N. Hudson Moore (1906).
1269:At the beginning of the
821:Elbe Sandstone Mountains
779:Source of the White Main
52:Fichtelgebirge / Smrčiny
29:Fichtel (disambiguation)
2900:Upper Palatinate Forest
2855:Hostýn-Vsetín Mountains
2671:
1692:up to 8 cm across.
1309:and limestone produced
1208:Early mountain building
839:Fichtelgebirgs-Hufeisen
813:Ore Mountains Highlands
684:, in the northwest are
384:walt zu dem Vythenberge
3364:North Palatine Uplands
2551:Lexikon Fichtelgebirge
2539:. Echter Verlag 2003,
2432:The Collector's Manual
2314:Zell im Fichtelgebirge
2078:
1904:, Fichtelberg-Neubau,
1890:Alexander von Humboldt
1625:
1613:Predominant rock types
1333:
1221:
1006:which later joins the
952:in the centre and the
937:to the east flows the
888:Inner Fichtel Plateau.
846:High Fichtel Mountains
780:
772:
764:
756:
748:
690:Zell im Fichtelgebirge
540:
359:
201:
193:
3603:Upper Palatine Forest
3477:Geiersberg (Breitsol)
3046:(Prussian) Velmerstot
2445:Minerals of the World
2417:Karsten, DLG (1798).
2076:
1930:Fichtelgebirge Museum
1780:Kösseine-Rand Granite
1595:Upper Palatine Forest
1583:Franconian fault line
1550:or at Parkstein near
1452:extensional tectonics
1323:
1231:. The history of its
1215:
898:Upper Palatine Forest
778:
770:
762:
754:
746:
538:
392:Vyth → Veit → Fichtel
357:
3632:Paschenburg Mountain
3201:Brocken (Blocksberg)
2870:Ještěd–Kozákov Ridge
2396:Harwood, J. (2012).
2051:cross country skiing
2036:German reunification
1829:is the transitional
1643:In detail there is:
1412:contact metamorphism
453:improve this section
417:became established.
401:connecting the name
366:) reported in 1476:
272:improve this section
36:10248 Fichtelgebirge
3082:Großer Zschirnstein
2682:Fichtelgebirge Club
1999:Economy and tourism
1827:Friedenfels Granite
1648:Porphyritic Granite
1438:Upper Carboniferous
1371:Upper Carboniferous
1355:Lower Carboniferous
1287:Upper Carboniferous
1216:The Devil's Table,
982:Mountains and hills
925:Herzbrunnen Europas
797:Thuringian Highland
755:Source of the Saale
472:"Fichtel Mountains"
291:"Fichtel Mountains"
226:Karlovy Vary Region
149: /
3596:Großer Farmdenkopf
3495:Lusatian Mountains
3172:Gladenbach Uplands
3140:Sieben-Linden-Berg
2880:Lusatian Mountains
2865:Javořice Highlands
2743:2022-05-22 at the
2730:Information portal
2641:Das Fichtelgebirge
2611:Gernot Messarius:
2591:Karl-Heinz Mayer:
2549:Dietmar Herrmann:
2525:Dietmar Herrmann:
2378:Hof-Plauen Airport
2079:
1734:and occurs in the
1369:. Finally, in the
1334:
1222:
1098:Platte (Steinwald)
921:Nabel Deutschlands
855:Northern ridge of
831:Geomorphologically
781:
773:
765:
763:Source of the Ohře
757:
749:
660:, in the west are
541:
360:
72:Highest point
3687:Fichtel Mountains
3674:
3673:
3579:Thuringian Forest
3424:Rothaar Mountains
3273:Lauensteiner Kopf
3208:Hildesheim Forest
3148:Franconian Forest
3113:Fichtel Mountains
2922:
2921:
2905:White Carpathians
2845:Fichtel Mountains
2520:978-3-925361-68-5
2510:Franz X. Bogner:
2453:978-1-4027-5339-8
2406:978-0-415-59868-2
2109:Brand (Oberpfalz)
1886:Thirty Years' War
1871:, granite, silt,
1845:Early Middle Ages
1821:Steinwald Granite
1587:Franconian Forest
1562:. These basaltic
1470:southwest of the
1431:industrialisation
1343:Franconian Forest
1241:truncated uplands
1200:
1199:
1038:observation tower
801:Franconian Forest
793:Thuringian Forest
533:
532:
525:
507:
352:
351:
344:
326:
186:Fichtel Mountains
182:
181:
131:Range coordinates
47:Fichtel Mountains
16:(Redirected from
3699:
3669:
3506:Zittau Mountains
3436:Saalhausen Hills
3292:Kaufungen Forest
3101:Elster Mountains
2949:
2942:
2935:
2926:
2925:
2917:
2875:Jizera Mountains
2835:Doupov Mountains
2809:
2805:
2804:
2793:
2786:
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2770:
2769:
2765:
2757:
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2415:
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2394:
2359:Bundesautobahnen
2024:Second World War
1987:
1972:
1718:Holzmühl Granite
1712:Elster Mountains
1536:Upper Palatinate
1524:Alpine foothills
1474:. Late Variscan
1433:of this region.
1404:Curia variscorum
1391:Variscan orogeny
1311:Wunsiedel marble
1291:metamorphic rock
1289:Period, created
1283:mountain folding
1118:Großer Waldstein
1056:Height (m)
1050:
1049:
959:to the west the
881:forests and the
861:Großer Waldstein
825:Elster Mountains
729:Upper Palatinate
528:
521:
517:
514:
508:
506:
465:
433:
425:
347:
340:
336:
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284:
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244:
234:Elster Mountains
220:in northeastern
172:
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107:
61:
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3698:
3697:
3696:
3677:
3676:
3675:
3670:
3661:
3584:Großer Beerberg
3560:Großer Feldberg
3400:Palatine Forest
3340:Lenne Mountains
3160:Franconian Jura
3004:Bavarian Forest
2993:Bohemian Forest
2959:
2956:Central Uplands
2953:
2923:
2918:
2909:
2885:Maple Mountains
2850:Giant Mountains
2820:Bohemian Forest
2811:
2807:
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2747:
2745:Wayback Machine
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2340:Federal roads (
2323:
2318:
2071:
2059:mountain biking
2013:Hutschenreuther
2001:
1994:
1990:Easter well in
1988:
1979:
1975:Easter well in
1973:
1961:Fränkische Post
1945:
1841:
1839:Mining industry
1758:Großer Kornberg
1732:Syenite Granite
1730:is also called
1615:
1520:Bohemian Massif
1488:
1472:Franconian Line
1427:mining industry
1339:
1210:
1205:
1139:Großer Kornberg
984:
906:Bavarian Forest
902:Bohemian Forest
741:
725:Upper Franconia
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466:
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3064:Volcanic Eifel
3049:
3041:Egge Mountains
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2700:External links
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1614:
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1504:Alpine orogeny
1496:Upper Tertiary
1487:
1484:
1476:volcanic rocks
1394:, named after
1386:fold mountains
1338:
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1235:begins in the
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815:together with
803:. In terms of
785:natural region
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415:Fichtelgebirge
403:Fichtelgebirge
399:folk etymology
350:
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218:Red Main River
214:Czech Republic
206:mountain range
194:Fichtelgebirge
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3388:Ore Mountains
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2895:Ore Mountains
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2190:
2187:
2185:
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2177:
2175:
2172:
2170:
2167:
2165:
2164:Kirchenlamitz
2162:
2160:
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2147:
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2056:
2052:
2048:
2047:alpine skiing
2043:
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2029:
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2016:
2014:
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1226:
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1190:
1189:
1185:
1183:
1180:
1179:
1175:
1172:
1170:
1167:
1166:
1162:
1160:
1159:Epprechtstein
1157:
1156:
1152:
1150:
1147:
1146:
1142:
1140:
1137:
1136:
1132:
1130:(Königsheide)
1129:
1126:
1125:
1121:
1119:
1116:
1115:
1111:
1109:
1106:
1105:
1101:
1099:
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1066:
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1062:
1058:
1055:
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1051:
1048:
1046:
1041:
1039:
1036:Tower) is an
1035:
1031:
1027:
1022:
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1013:
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1001:
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989:
979:
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930:
929:
928:
926:
922:
917:
915:
911:
907:
903:
899:
895:
894:Ore Mountains
887:
884:
880:
876:
872:
870:
866:
865:Epprechtstein
862:
858:
854:
851:
847:
844:
843:
842:
840:
836:
832:
828:
826:
822:
818:
817:Ore Mountains
814:
810:
806:
802:
798:
794:
790:
786:
777:
769:
761:
753:
745:
739:Geomorphology
736:
734:
730:
726:
722:
718:
713:
711:
707:
703:
699:
695:
691:
687:
683:
679:
675:
671:
667:
663:
659:
655:
651:
647:
643:
642:Speichersdorf
639:
635:
631:
627:
623:
618:
616:
612:
608:
604:
600:
599:Kirchenlamitz
596:
592:
588:
584:
580:
576:
572:
568:
563:
561:
557:
553:
548:
546:
537:
527:
524:
516:
505:
502:
498:
495:
491:
488:
484:
481:
477:
474: –
473:
469:
468:Find sources:
462:
458:
454:
448:
447:
443:
438:This section
436:
432:
427:
426:
418:
416:
412:
408:
404:
400:
395:
393:
389:
385:
381:
377:
373:
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356:
346:
343:
335:
324:
321:
317:
314:
310:
307:
303:
300:
296:
293: –
292:
288:
287:Find sources:
281:
277:
273:
267:
266:
262:
257:This section
255:
251:
246:
245:
237:
235:
231:
227:
223:
219:
215:
211:
207:
203:
199:
195:
191:
187:
178:
175:
173:
167:
162:
134:
132:
128:
125:
121:
118:
114:
106:
100:
95:
91:
89:
85:
82:
79:
75:
70:
66:
60:
55:
50:
45:
37:
30:
19:
3654:
3651:Wiehen Hills
3649:
3642:
3637:
3630:
3625:
3618:
3613:
3606:
3601:
3594:
3589:
3582:
3577:
3570:
3565:
3558:
3553:
3547:Hoher Randen
3545:
3540:
3534:
3531:Swabian Jura
3529:
3522:
3517:
3509:
3504:
3498:
3493:
3487:
3482:
3475:
3470:
3463:
3458:
3451:
3446:
3439:
3434:
3427:
3422:
3415:
3410:
3403:
3398:
3391:
3386:
3381:Katzenbuckel
3379:
3374:
3367:
3362:
3355:
3350:
3343:
3338:
3331:
3326:
3319:
3314:
3307:
3302:
3295:
3290:
3283:
3278:
3271:
3266:
3258:
3253:
3247:
3242:
3235:
3230:
3223:
3218:
3211:
3206:
3199:
3194:
3187:
3182:
3175:
3170:
3163:
3158:
3151:
3146:
3138:
3133:
3127:
3122:
3116:
3112:
3111:
3106:Kapellenberg
3104:
3099:
3094:Eilumer Horn
3092:
3087:
3080:
3075:
3067:
3062:
3056:
3051:
3044:
3039:
3032:
3027:
3020:
3015:
3009:Großer Arber
3007:
3002:
2998:Großer Arber
2996:
2991:
2984:
2981:Black Forest
2979:
2972:
2967:
2844:
2709:(in English)
2677:
2654:
2640:
2626:
2612:
2598:
2592:
2578:
2564:
2550:
2536:
2526:
2511:
2491:. Retrieved
2481:
2465:
2460:
2444:
2439:
2431:
2426:
2418:
2413:
2397:
2392:
2374:
2357:
2341:
2335:
2330:Marktredwitz
2326:
2184:Marktredwitz
2179:Marktleuthen
2174:Marktleugast
2104:Bischofsgrün
2044:
2040:
2027:
2020:Bischofsgrün
2017:
2002:
1977:Marktleuthen
1960:
1953:Osterbrunnen
1946:
1932:at Wunsiedel
1917:visitor mine
1910:
1842:
1834:phenocrysts.
1826:
1820:
1815:Rand Granite
1814:
1809:Leupoldsdorf
1804:Zinn Granite
1803:
1796:
1787:Kern Granite
1786:
1783:phenocrysts.
1779:
1749:
1736:Marktredwitz
1731:
1727:
1717:
1696:Reut Granite
1695:
1671:
1656:Marktleuthen
1647:
1642:
1640:and people.
1616:
1572:
1489:
1464:Rotliegendes
1463:
1447:Rotliegendes
1445:
1435:
1403:
1389:
1359:metamorphism
1340:
1325:
1281:during this
1275:temperatures
1268:
1250:transported
1245:
1225:Geologically
1223:
1218:Teufelstisch
1217:
1182:Fürstenstein
1042:
1026:Bischofsgrün
1023:
1020:
985:
965:
924:
920:
918:
891:
838:
829:
782:
733:World War II
714:
622:Bischofsgrün
619:
579:Marktleuthen
575:Marktredwitz
564:
549:
542:
519:
513:October 2022
510:
500:
493:
486:
479:
467:
451:Please help
439:
414:
410:
402:
396:
391:
387:
383:
379:
375:
367:
361:
338:
332:October 2022
329:
319:
312:
305:
298:
286:
270:Please help
258:
185:
183:
171:Parent range
158:50.05; 11.85
65:Heinersreuth
3627:Weser Hills
3608:Kreuzfelsen
3465:Große Blöße
3417:Wasserkuppe
3393:Fichtelberg
3369:Donnersberg
3309:Wüstegarten
3280:Kaiserstuhl
3260:Ellerspring
3225:Bloße Zelle
2974:Einödriegel
2764:(in German)
2756:(in German)
2733:(in German)
2725:(in German)
2717:(in German)
2356:Motorways (
2304:Weißenstadt
2134:Goldkronach
2124:Fichtelberg
2094:Bad Berneck
2069:Settlements
2028:Hausgebirge
1992:Weißenstadt
1906:Goldkronach
1898:Weißenstadt
1686:phenocrysts
1652:Weißenstadt
1548:Rauher Kulm
1540:Eger Graben
1512:Carpathians
1436:During the
1330:Weißenstadt
1326:Rudolfstein
1237:Precambrian
1004:Fichtelnaab
996:Saxon Saale
956:to one side
950:Fichtelnaab
879:Reichsforst
811:within the
787:called the
682:Bad Berneck
674:Goldkronach
626:Fichtelberg
591:Weißenstadt
376:Vichtelberg
374:was called
156: /
3681:Categories
3644:Fuchskaute
3639:Westerwald
3615:Vogelsberg
3429:Langenberg
3333:Kulpenberg
3328:Kyffhäuser
3304:Kellerwald
3297:Hirschberg
3189:Hohes Gras
3165:Dürrenberg
3118:Schneeberg
2958:of Germany
2748:(in Czech)
2493:2023-10-31
2384:References
2321:Approaches
2294:Weidenberg
2284:Waldershof
2274:Thierstein
2269:Thiersheim
2239:Schönbrunn
2234:Schirnding
2194:Mehlmeisel
1943:Traditions
1865:brown coal
1744:Thiersheim
1728:Redwitzite
1666:as far as
1607:geologists
1440:and Lower
1429:and early
1149:Hohe Matze
1078:Ochsenkopf
1065:Schneeberg
992:White Main
988:Schneeberg
961:White Main
914:Thuringian
910:Franconian
809:mesoregion
662:Weidenberg
630:Mehlmeisel
595:Waldershof
483:newspapers
380:inter alia
372:Ochsenkopf
302:newspapers
81:Schneeberg
3656:Heidbrink
3620:Taufstein
3572:Barnacken
3524:Hohe Egge
3357:Köterberg
3321:Eisenberg
3285:Totenkopf
3249:Erbeskopf
3213:Griesberg
3177:Angelburg
3153:Döbraberg
3124:Steinwald
3069:Ernstberg
3058:Hohe Acht
3034:Nordhelle
2309:Wunsiedel
2244:Schönwald
2199:Münchberg
2119:Erbendorf
2009:Rosenthal
1949:Huguenots
1894:Wunsiedel
1877:soapstone
1774:muscovite
1676:contains
1638:landscape
1591:Münchberg
1575:landscape
1560:Pechbrunn
1544:diatremes
1460:sediments
1456:volcanism
1420:pegmatite
1379:Münchberg
1345:from the
1315:sea level
1307:quartzite
1299:phyllites
1264:limestone
1252:sediments
1053:Mountain
1045:sea level
976:Black Sea
972:North Sea
970:from the
968:watershed
954:Haidenaab
875:Steinwald
857:Waldstein
698:Münchberg
658:Fuchsmühl
650:Erbendorf
569:with its
567:Wunsiedel
440:does not
421:Geography
405:with the
388:St. Veith
382:with the
259:does not
240:Etymology
97:Geography
88:Elevation
3472:Spessart
3376:Odenwald
3255:Soonwald
3244:Hunsrück
3135:Kohlwald
2986:Feldberg
2741:Archived
2299:Weißdorf
2259:Sparneck
2219:Podhradí
2099:Bindlach
2055:sledding
2032:A 9
1791:Nußhardt
1776:as well;
1762:feldspar
1756:and the
1754:Kösseine
1690:feldspar
1673:porphyry
1579:Pliocene
1570:layers.
1568:tectonic
1500:tectonic
1480:rhyolite
1468:platform
1424:medieval
1351:Devonian
1347:Silurian
1279:pressure
1271:Cambrian
1192:Kohlberg
1108:Kösseine
1088:Nußhardt
1059:Remarks
1012:Bayreuth
1008:Waldnaab
1002:and the
904:and the
885:mountain
883:Kohlberg
869:Kornberg
850:Kösseine
727:and the
721:Bavarian
694:Weißdorf
678:Bindlach
670:Bayreuth
609:and the
560:Bayreuth
212:and the
3536:Lemberg
3484:Sudetes
3460:Solling
3441:Himberg
3017:Deister
2505:Sources
2279:Tröstau
2209:Neusorg
2154:Kemnath
2149:Hranice
2129:Gefrees
2084:Arzberg
1957:Bourbon
1902:Arzberg
1881:uranium
1869:diabase
1843:By the
1770:biotite
1740:Arzberg
1700:Gefrees
1678:biotite
1650:of the
1618:Granite
1603:plateau
1538:as the
1528:Miocene
1522:in the
1492:neogene
1490:In the
1462:of the
1442:Permian
1400:Varisci
1367:fossils
1317:again.
1303:schists
1233:orogeny
1229:granite
1203:Geology
1128:Hohberg
974:to the
852:massif,
686:Gefrees
666:Creußen
646:Kemnath
638:Neusorg
603:Tröstau
583:Arzberg
497:scholar
461:removed
446:sources
364:Kemnath
316:scholar
280:removed
265:sources
224:to the
222:Bavaria
210:Germany
204:) is a
202:Smrčiny
144:11°51′E
141:50°03′N
120:Bavaria
3555:Taunus
3542:Randen
3519:Süntel
3405:Kalmit
3345:Homert
3129:Platte
2692:
2661:
2647:
2633:
2619:
2605:
2585:
2571:
2557:
2543:
2518:
2472:
2451:
2404:
2254:Skalná
2229:Röslau
2214:Plesná
2159:Krásná
2139:Hazlov
2114:Ebnath
2063:hiking
2053:, and
1873:marble
1861:basalt
1831:facies
1766:quartz
1708:Saxony
1684:) and
1680:(dark
1670:. The
1668:Haslau
1660:Röslau
1626:granum
1599:uplift
1589:, the
1564:nappes
1552:Weiden
1532:basalt
1458:. The
1382:gneiss
1293:. The
1248:rivers
1082:1,024
1047:(NN):
1030:Fleckl
998:, the
994:, the
948:: the
900:, the
835:massif
823:. The
654:Wiesau
611:Röslau
587:Röslau
556:Weiden
499:
492:
485:
478:
470:
411:Fichte
407:German
318:
311:
304:
297:
289:
232:. The
190:German
122:&
3316:Knüll
3053:Eifel
3022:Bröhn
2348:B 303
2336:Road:
2327:Rail:
2224:Rehau
2204:Nagel
1698:near
1634:peaks
1630:grain
1622:Latin
1408:folds
1402:) of
1396:Hof's
1328:near
1295:shale
1069:1,051
933:Saale
706:Rehau
634:Nagel
504:JSTOR
490:books
409:word
323:JSTOR
309:books
198:Czech
116:State
3412:Rhön
3220:Hils
3196:Harz
2825:Brdy
2690:ISBN
2684:and
2672:Maps
2659:ISBN
2645:ISBN
2631:ISBN
2617:ISBN
2603:ISBN
2583:ISBN
2569:ISBN
2555:ISBN
2541:ISBN
2516:ISBN
2470:ISBN
2449:ISBN
2402:ISBN
2375:Air:
2366:and
2364:A 93
2352:B 15
2350:and
2249:Selb
2169:Luby
2011:and
2005:Selb
1947:The
1915:the
1857:iron
1849:gold
1768:and
1722:Selb
1704:Selb
1682:mica
1628:for
1556:lava
1508:Alps
1353:and
1301:and
1277:and
1262:and
1260:sand
1256:clay
1196:632
1186:675
1163:798
1153:813
1143:827
1133:863
1122:877
1112:939
1102:946
1092:972
1034:Æsir
1014:and
1000:Ohře
946:Naab
939:Ohře
912:and
877:and
867:and
819:and
799:and
708:and
702:Selb
680:and
656:and
607:Ohře
601:and
554:and
476:news
444:any
442:cite
295:news
263:any
261:cite
184:The
77:Peak
3268:Ith
3089:Elm
2368:A 9
2362:):
2346:):
1963:).
1853:tin
1688:of
1518:or
1416:ore
1363:ore
1173:758
1169:Háj
1016:Hof
710:Hof
552:Hof
455:by
274:by
208:in
3683::
3514:))
3132:,
2089:Aš
2061:,
2049:,
1900:,
1896:,
1875:,
1867:,
1863:,
1855:,
1851:,
1764:,
1710:/
1624::
1510:,
1482:.
1349:,
1266:.
1258:,
1018:.
863:,
795:,
712:.
704:,
696:,
692:,
688:,
676:,
672:,
668:,
664:,
652:,
648:,
644:,
640:,
636:,
632:,
628:,
624:,
617:.
615:Aš
597:,
593:,
589:,
585:,
581:,
577:,
562:.
397:A
200::
196:,
192::
3550:)
3539:(
3503:(
3492:(
3263:)
3252:(
3143:)
3121:(
3072:)
3061:(
3012:)
3001:(
2948:e
2941:t
2934:v
2792:e
2785:t
2778:v
2522:.
2496:.
2476:.
2455:.
2408:.
1742:/
1738:/
1658:/
1620:(
1506:(
1494:(
1444:(
1332:)
526:)
520:(
515:)
511:(
501:·
494:·
487:·
480:·
463:.
449:.
345:)
339:(
334:)
330:(
320:·
313:·
306:·
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