Geography
[edit]
Franconian Switzerland is the northern part of the Franconian Jura. It is often loosely defined as the region bounded by the Main to the north, Regnitz to the west and Pegnitz to the east, or by the A 70 motorway to the north, the A 9 to the east and the A 73 to the west. However, the actual region of Franconian Switzerland is only the catchment area of the River Wiesent.
The region covers parts of the counties of Bamberg, Bayreuth and Forchheim. Its best known settlements include Pottenstein, Gößweinstein, Muggendorf, Ebermannstadt, Streitberg, Egloffstein, and Waischenfeld.
Its boundaries are Obermainland (north), Erlangen (south), Bayreuth (east), Forchheim (west), and Bamberg (northwest).
Information about Franconian Switzerland may be found in the Franconian Switzerland Museum in Tüchersfeld with its comprehensive regional collections. It is housed in the so-called Jew's Court (Judenhof), below two steep rock pinnacles.
Franconian Switzerland Trade Association[edit]
The following 18 municipalities across 2 counties belong to the Franconian Switzerland Trade Association (Wirtschaftsverband Fränkische Schweiz):
County of Bayreuth:
Ahorntal
Betzenstein
Creußen
Gesees
Haag
Hummeltal
Pegnitz
Plech
Pottenstein
Prebitz
Schnabelwaid
County of Forchheim:
Egloffstein
Gößweinstein
Gräfenberg
Hiltpoltstein
Igensdorf
Obertrubach
Weißenohe
Geology[edit]
Tower karst rocks in Tüchersfeld, 2008
In the White Jurassic period, about 161 million to 150 million years ago, a shallow sea lay across southern Germany. During this period, thick rock sequences were deposited on the seabed as the Earth's crust continued to sink. The limestone and dolomite rocks that formed during this time period, along with the deeply incised river valleys and dry, arid plateaus, characterize this karst landscape. Many fossils, most typically ammonites, may be found in the limestone strata.
In the late Jurassic period, the sea receded with the shifting of European continental plate, allowing larger areas of land to emerge and form at the beginning of the Cretaceous period. During this time, the region had a tropical climate, and limestone and dolomite rocks underwent intense weathering. During the Cretaceous, a sea once again covered much of the region.
In the Tertiary period, the sea receded a second time, partially exposing the Jurassic landscape.
Mountains and hills[edit]
The double-peaked Ehrenbürg
The most prominent peak in this region is the Ehrenbürg, commonly known as Walberla, a table hill east of Forchheim. It consists of two peaks, the Rodenstein (532 m) and the Walberla (512 m). On the hilltop is its namesake, the small Walburgis Chapel, first mentioned in a 1360 manuscript. There is an annual festival on the hilltop on 30 April, the birthday of Saint Walburga, which attracts thousands of people.
Other popular peaks:
Leienfels (near Pottenstein), 590 m
Spiegelfels along with the Pfarrfelsen near Affalterthal, Markt Egloffstein, 468 m
Wichsenstein (near Gössweinstein), 587 m
Signalstein (near Wolfsberg, Obertrubach), 582 m
Little Kulm (near Körbeldorf), 623 m
Hohenmirsberger Plateau (near Pottenstein), 614 m
Neubürg (near Wohnsgehaig), 587 m
Tannenberg, 599 m
Graubühl (near Creussen), 569 m
German rock climber Alexander Megos at Action Directe
The rocks of Franconian Switzerland's mountains and hills are popular for rock climbing. With more than 6,500 routes, it is one of the best developed climbing areas in the world.
Important climbing areas:
Trubach Valley
Walberla
Wiesent Valley
Leinleiter Valley
Püttlach Valley
Aufseß Valley
Caves[edit]
Stalagmite in the Binghöhle
There are countless caves in Franconian Switzerland, of which the Devil's Cave (Teufelshöhle) near Pottenstein is the most famous. The region is an example of karst topography.
Accessible caves:
Binghöhle (near Streitberg)
Teufelshöhle (near Pottenstein)
Sophienhöhle (in the Ailsbach valley)
Oswaldhöhle (near Muggendorf)
Rosenmüllershöhle (near Muggendorf)
Quackenschloss (near Engelhardsberg), cave ruin
Zoolithenhöhle (near Burggailenreuth)
Esperhöhle (near Gössweinstein)
Förstershöhle (in the Zeubach valley)
Schönsteinhöhle (in the Long Valley)
Klauskirche (near Betzenstein)
Riesenburg (near Doos)
Hasenlochhöhle (near Pottenstein), known for having housed people during the Stone Age.
Castles[edit]
Greifenstein Palace
The ruins of Neideck Castle
Franconian Switzerland is located along the so-called Castle Road (Burgenstraße), which connects more than 70 castles, palaces, and fortresses between Mannheim and Prague. Most of these castles were constructed in the Middle Ages.
The following castles and castle ruins can be visited:
Egloffstein Castle
Gössweinstein Castle
Schloss Greifenstein, seat of the Stauffenberg family.
Rabeneck Castle
Rabenstein Castle
Pottenstein Castle
Unteraufseß Castle
Waischenfeld Castle
Bärnfels Castle ruins
Hollenberg Castle ruins
Leienfels Castle ruins
Neideck Castle ruins
Neidenstein Castle ruins
Streitburg Castle ruins (Markt Wiesenttal)
Stierberg Castle ruins
Wildenfels Castle ruins
Wolfsberg Castle ruins