List of geotopes in the Lichtenfels district
This list contains the geotopes of the Upper Franconian district of Lichtenfels in Bavaria . The list contains the official names and numbers of the Bavarian State Office for the Environment (LfU) as well as their geographical location. This list may not be complete. Around 3,400 geotopes (as of March 2020) are recorded in the Bavarian geotope register. The LfU does not consider some geotopes suitable for publication on the Internet. For example, some objects are not safely accessible or may only be entered to a limited extent for other reasons.
Surname | image | Geotope ID | Municipality / location | Geological unit of space | description | Area m² / extension m | geology | Digestion type | value | Protection status | comment |
---|---|---|---|---|---|---|---|---|---|---|---|
Impact slope of the Main SW of Nedensdorf (Trimeusel) |
![]() |
478A001 |
Relay stone position |
Northern Albrand region | The main slope on the Trimeusel is probably the most impressive Lias outcrop in Northern Bavaria. Here you can find the most powerful Posidonia slate formation in all of Northern Bavaria. Striking layers are the monotony bench and the dinosaur layer THEODORIS. The outcrop is known as a fossil site, but collection is prohibited. | 150 50 × 3 |
Type: Standard / Reference Profile, Animal Fossils Type: Mudstone |
Impact slope / river bed / stream profile | especially valuable | Natural monument, FFH area, bird sanctuary | |
Street embankment SE from Oberlangheim | 478A002 |
Lichtenfels position |
Northern Albrand region | The road outcrop near Oberlangheim opens up an excellent profile from Malm Alpha to Beta. A parking bay is available. | 1000 100 × 10 |
Type: Rock Type: Limestone |
embankment | significant | Natural park | ||
Profile in the ravine in Kirchlein | 478A003 |
Burgkunstadt position |
Obermain-Bruchschollenland | The ravine in the village of Kirchlein contains v. Gümbels famous little church profile. The outcrop, designated as a natural monument, shows the transition from the Rhätolias strata to the Lias strata. Unfortunately, despite being under protection, the site is very overgrown and the rock is practically impossible to find. | 900 300 × 3 |
Type: Layer sequence Type: Sandstone |
embankment | significant | Landscape component | ||
Former quarry E von Meuselsberg | 478A004 |
Burgkunstadt position |
Obermain-Bruchschollenland | The abandoned break near Meuselsberg is strongly overgrown, z. Partly filled with dead wood and garden waste. He develops sandstones of the Rhätolia, which were quarried as stone. | 1200 40 × 30 |
Type: Rock Type: Sandstone |
Quarry | significant | no protected area | ||
Embankment at the railway bridge WNW von Horb | 478A005 |
Market position |
Northern Albrand region | The road outcrop directly on the B289 contains the only outcrop in the Coburg sandstone in the Lichtenfels district. It is overlaid by the Quaternary central terrace. Greening the embankment was avoided in order to preserve the outcrop as an excursion destination. In the meantime, however, it has grown together strongly. Further cuts are located on the northern accompanying path near the railway bridge. | 770 110 × 7 |
Type: Rock Type: Sandstone, Sand |
embankment | significant | no protected area | ||
Rodachprallhang on the Großer Kulbitz near Marktzeuln | 478A007 |
Market position |
Northern Albrand region | The Rodachprallhang near Marktzeuln offers an excellent geological profile from the Lower (Lower to Upper Heldburgstufe) to the Middle Burgsandstein (Sandstone Keuper). | 500 100 × 5 |
Type: Rock Type: Mudstone, Sandstone |
Impact slope / river bed / stream profile | significant | FFH area, bird sanctuary | ||
Road access B289 near Weidnitz-Burgkunstadt | 478A008 |
Burgkunstadt position |
Northern Albrand region | The road sections between Weidnitz and Theisau, which are spread over a stretch of more than 3 km, open up rocks from the Middle Burg sandstone with caliche formations. | 6000 2000 × 3 |
Type: Rock Type: Sandstone |
embankment | significant | no protected area | ||
Felsenkeller in Marktzeuln | 478A009 |
Market position |
Northern Albrand region | On the way to Rodach you will find 14 rock cellars over a length of 200 meters, some of which are more than 10 m long, which are mostly closed. | 20 10 × 2 |
Type: rock type, tunnel type: sandstone |
Tunnel / gallery / shaft | significant | Natural monument | ||
Digging point at Kordigast SE in Burkheim |
![]() |
478A011 |
Altenkunstadt position |
Northern Franconian Alb | An official fossil tapping site has been set up in the embankment of an old material extraction point in Malm Alpha Bankkalk. | 100 20 × 5 |
Type: Animal Fossils, Rock Type: Limestone, Marlstone |
other information | significant | Landscape protection area, nature park | |
Aufgel. Quarries on the Krappenberg WSW of Degendorf | 478A012 |
Lichtenfels position |
Northern Albrand region | On the ridge between Krappenberg and Fuchsgrund there are numerous abandoned quarries in the Rhätolias sandstone. Most of them show little or no information. The most instructive one is right next to the Prälatenweg hiking trail, approx. 600 m wsw from Degendorf. It measures approx. 35 × 15 × 6 m and shows beautiful outcrops and typical weathering structures. | 40000 400 × 100 |
Type: Quarry / Pit, Rock Type: Sandstone |
Quarry | precious | Natural park | ||
Aufgel. Limestone quarry on the western slope of the Old Staffelberg | 478A013 |
Relay stone position |
Northern Franconian Alb | The quarry on the western slope of the Old Staffelberg is one of the few large-scale outcrops in the factory limestone (Malm Beta) in the area of the Staffelberg. The quarry was in operation until the 1950s. | 1400 70 × 20 |
Type: Type of rock, type of layer sequence : Limestone |
Quarry | significant | Landscape protection area, nature park | ||
Former iron ore mining on the Kordigast SW of Altenkunstadt |
![]() |
478G001 |
Altenkunstadt position |
Northern Albrand region | Two dilapidated tunnels with heaps at Kordigast (south of Pfaffendorf and Burkheim) document the mining of iron ore in the 19th century. At that time, the iron oliths in the upper seam of the Dogger Beta were very popular. | 1 1 × 1 |
Type: Stud Type: Sandstone |
Tunnel / gallery / shaft | significant | Landscape protection area, nature park | |
Ebnether Keller NW of Ebneth |
![]() |
478G002 |
Burgkunstadt position |
Obermain-Bruchschollenland | The natural conditions at the Rhätolias stratification were used to create the spacious rock cellar. The rock is well exposed inside and outside the facilities. | 12500 250 × 50 |
Type: rock cellar, rock wall / slope, layer type: sandstone |
Slope crack / rock wall | significant | Natural monument | |
Dismissed Schönthalzeche S by Vierzehnheiligen | 478G003 |
Relay stone position |
Northern Franconian Alb | From the numerous mining sites for iron ore of the Dogger Beta in the valley head of the Schönthal a mine dump was cleared. The rolled mouth hole of the tunnel has been partially opened up and lined with door frames. The ore mining, which had been in operation since the middle of the 19th century, was only stopped in 1941 due to a lack of profitability. | 2100 70 × 30 |
Type: Mine Type: Iron ore, sandstone |
no information | precious | Landscape protection area, nature park | ||
Karst spring Stierfessel E from Oberküps |
|
478Q001 |
Ebensfeld position |
Northern Franconian Alb | The bullfetter near Oberküps is a so-called famine well, where the spring discharge varies greatly depending on the season. | 1 1 × 1 |
Type: Layer Source Type: Limestone |
no information | significant | Natural monument, landscape protection area, FFH area | |
Karst spring E from Großziegenfeld |
|
478Q002 |
Weismain position |
Northern Franconian Alb | The karst spring rises in a mighty spring pot on the natural spring horizon of the Malm Gamma. The north side of the source pot is built in. | 50 5 × 10 |
Type: Constriction Source Type: Limestone |
no information | precious | Natural monument, landscape protection area, nature park | |
Dolinenfeld WSW von Weiden | 478R001 |
Weismain position |
Northern Franconian Alb | The area west of Weiden, designated as Brunnenerdfall on the topographical map, contains isolated sinkholes of the karstified Malm Gamma and Delta. | 30000 300 × 100 |
Type: Dolinenfeld Type: Dolomite stone |
no information | significant | Landscape protection area, nature park | ||
Hohe Wand NE by Wallersberg | 478R002 |
Weismain position |
Northern Franconian Alb | The imposing Hohe Wand rock face in the Kleinziegenfelder Tal nature reserve consists of massive dolomite from the Malm Gamma and Delta. | 30 10 × 3 |
Type: Rock wall / slope Type: Dolomite stone |
Slope crack / rock wall | significant | Natural monument, landscape protection area, FFH area | ||
Suttenstein E from Wallersberg | 478R003 |
Weismain position |
Northern Franconian Alb | The imposing Suttenstein rock lies in the Kleinziegenfelder valley. It consists of massive dolomite from the Malm Gamma and Delta. | 20 10 × 2 |
Type: Rock wall / slope Type: Dolomite stone |
Slope crack / rock wall | significant | Natural monument, landscape protection area, FFH area | ||
Felsturm flower vase NE by Wallersberg | 478R004 |
Weismain position |
Northern Franconian Alb | The imposing rock flower vase is located in the Kleinziegenfelder valley. It consists of massive dolomite from the Malm Gamma and Delta. | 225 15 × 15 |
Type: Rock tower / needle Type: Dolomite stone |
Slope crack / rock wall | significant | Natural monument, landscape protection area, FFH area | ||
Dolomite tower NW of Kleinziegenfeld | 478R005 |
Weismain position |
Northern Franconian Alb | The dolomite tower designated as ND on the quarry area of Firm Diroll (Burgkunstadt) consists of secondary dolomitized reef limestone of the Malm Gamm and Delta. | 100 10 × 10 |
Type: Rock tower / needle Type: Dolomite stone |
Slope crack / rock wall | significant | Natural monument, FFH area, bird sanctuary | ||
Rote Wand NNE from Kleinziegenfeld | 478R006 |
Weismain position |
Northern Franconian Alb | The Rote Wand rock face in the Kleinziegenfelder valley consists of massive dolomite from the Malm Gamma and Delta. | 50 10 × 5 |
Type: Rock wall / slope Type: Dolomite stone |
Slope crack / rock wall | significant | Natural monument, landscape protection area, FFH area | ||
Rock tower Mönch N von Kleinziegenfeld | 478R007 |
Weismain position |
Northern Franconian Alb | The Mönch rock tower is located in the Kleinziegenfelder valley. It consists of massive dolomite from the Malm Gamma and Delta. | 50 10 × 5 |
Type: Rock tower / needle Type: Dolomite stone |
Slope crack / rock wall | significant | Natural monument, landscape protection area, FFH area | ||
Felsburg Viktoriastein SE from Arnstein |
![]() |
478R009 |
Weismain position |
Northern Franconian Alb | At the Victoriastein south of Weihersmühle, sections of the interlocking between bench limestone, sponge limestone banks and reef limestone of the Malm Gamma and Delta are accessible. | 5000 100 × 50 |
Type: rock castle, rock type: dolomite stone |
Slope crack / rock wall | significant | Natural monument, landscape protection area, FFH area | |
Rocks below the castle ruins NE of Niesten |
![]() |
478R010 |
Weismain position |
Northern Franconian Alb | The rocks consist of rocks from the Lower Malm and contain the Eselsloch cave. | 30000 300 × 100 |
Type: rock wall / slope, karst halfway / natural bridge Type: limestone |
Slope crack / rock wall | significant | Landscape protection area, FFH area, bird sanctuary | |
Karsttal Blade SW from Ehrhardsmühle |
![]() |
478R011 |
Weismain position |
Northern Franconian Alb | The short dry valley is framed by imposing rocks. On its north side there are mighty reef blocks that are free from vegetation and are used as a climbing garden. The thick banked and massive dolomites form up to 8 m wide overhangs above thin banked dolomite layers. | 10000 100 × 100 |
Type: Kerbtal, rock face / slope, rock type: dolomite stone |
Slope crack / rock wall | especially valuable | Natural monument, landscape protection area, nature park | |
Dolinenfeld between Arnstein and Bojendorf | 478R012 |
Weismain position |
Northern Franconian Alb | The doline field between Arnstein and Bojendorf reveals the karstified dolomite of the Malm Gamma and Delta, which is in the subsoil. | 150 10 × 15 |
Type: Dolinenfeld Type: Dolomite stone |
no information | significant | Natural park | ||
Rock tower Rauhenstein NW from Wallersberg | 478R013 |
Weismain position |
Northern Franconian Alb | The Rauhenstein, designated as a natural monument, is a rock tower in the spongy limestone of the Malm Gamm and Delta. | 500 25 × 20 |
Type: Rock Tower / Needle Type: Limestone |
Slope crack / rock wall | precious | Natural monument, landscape protection area, FFH area | ||
The Rauhen Felsen SW of Mosenberg | 478R014 |
Weismain position |
Northern Franconian Alb | The rough rocks, designated as a natural monument, consist of sponge limestone from the Malm Gamma and Delta. | 200 20 × 10 |
Type: Group of rocks Type: Limestone |
Slope crack / rock wall | significant | Natural monument, landscape protection area, FFH area | ||
Pfersag waterfall NE from Ebneth |
|
478R016 |
Burgkunstadt position |
Obermain-Bruchschollenland | The Pfersag waterfall is about 2 m high and marks the layer of the Rhätolias sandstone. The water comes from the wet well, which rises from several sources in Lias Alpha 3. | 10 5 × 2 |
Type: Waterfall, Layer Source Type: Limestone, Sandstone |
Impact slope / river bed / stream profile | precious | Natural monument | |
WNW rock group from Ebneth | 478R017 |
Burgkunstadt position |
Obermain-Bruchschollenland | The rock group consists of Rhaetian sandstone rocks with typical cross-layering. The stratification breaks up into large boulders along wide open fissures. There are also several rock cellars here. | 60 15 × 4 |
Type: Rock wall / slope, layer step, boulder Type: Sandstone |
Slope crack / rock wall | precious | Natural monument | ||
Rock group near Wildenroth | 478R018 |
Burgkunstadt position |
Obermain-Bruchschollenland | The Rhätsandsteinfelsen in Wildenroth are marked on the map as Hans-Ulrich-Felsen (natural monument). They became known through evidence of a prehistoric forge. | 120 30 × 4 |
Type: Rock Wall / Slope Type: Sandstone |
Slope crack / rock wall | significant | Natural monument | ||
Bärental NE from Wunkendorf |
![]() |
478R019 |
Weismain position |
Northern Franconian Alb | The nature reserve Bärental near Wunkendorf opens up layers of the Malm Alpha to Gamma, whereby the rocks are in the area of the sponge facies. Numerous different geotope types, such as B. the Krassach spring as a typical karst spring, a creek, several karst caves with sinter formations and a rock gate, increase the tourist attraction of this area. Bones of the Ice Age cave bear were found in one of the caves (fox hole). | 1200000 3000 × 400 |
Type: Kerbtal, karst halftone / natural bridge, karst horizontal cave, layer spring, stream shrinkage, rock wall / slope Type: limestone |
Slope crack / rock wall | precious | Landscape protection area, FFH area, bird sanctuary | |
Rock clearance oven ESE from Oberküps | 478R020 |
Ebensfeld position |
Northern Franconian Alb | The oven is a rock with a half-cave in the sponge lime of the Malm Gamma. | 8 4 × 2 |
Type: rock wall / slope, karst halfway / natural bridge Type: limestone |
Slope crack / rock wall | significant | Natural monument, landscape protection area, nature park | ||
Rock group on the Great Kordigast |
![]() |
478R021 |
Altenkunstadt position |
Northern Franconian Alb | The impressive rock formations on the east summit of the Great Kordigast provide a wonderful view. The rocks consist of reefs of the Malm Delta and are very rich in fossils (silicified sponges, trochite rubble limestone, shells). | 5000 100 × 50 |
Type: Group of rocks Type: Limestone |
Slope crack / rock wall | precious | Natural monument, landscape protection area, nature park | |
Uhufelsen ENE from Serkendorf | 478R022 |
Relay stone position |
Northern Franconian Alb | The Uhufelsen near Serkendorf consists of sponge limestone from the Malm Gamma and Delta. | 50 10 × 5 |
Type: Rock Wall / Slope Type: Limestone |
Slope crack / rock wall | significant | Natural monument, FFH area, bird sanctuary | ||
Rock with half-cave Botzenkapelle SE from Serkendorf | 478R023 |
Relay stone position |
Northern Franconian Alb | The Botzenkapelle near Serkendorf is an impressive half-cave in the sponge limestone of the Malm Gamma and Delta. | 50 10 × 5 |
Type: rock wall / slope, karst halfway / natural bridge Type: limestone |
Slope crack / rock wall | significant | Natural monument, nature park | ||
Rock tower Hohler Stein ESE from Schwabthal |
![]() |
478R024 |
Relay stone position |
Northern Franconian Alb | The hollow stone towering over the Alb plateau with the eponymous half-cave consists of secondary dolomitized limestone from the Malm Gamma and Delta. | 100 10 × 10 |
Type: rock tower / needle, karst halfway / natural bridge Type: dolomite stone |
Slope crack / rock wall | significant | Natural monument, FFH area, bird sanctuary | |
Dolinen NW of Eichig | 478R028 |
Lichtenfels position |
Northern Franconian Alb | The row of sinkholes northwest of Eichig has its origin in the karstification of the Malm Gamma and Delta. Several sinkholes are lined up in NE-SW direction along the lineament that runs parallel to the Köttler Grund. Bales of grass are stored at the sinkhole, which is designated as a natural monument. | 2500 50 × 50 |
Type: Dolinenfeld Type: Limestone |
no information | significant | Natural monument, landscape protection area, nature park | ||
Staffelberg SE from Staffelstein |
![]() |
478R029 |
Relay stone position |
Northern Franconian Alb | The summit of the Staffelberg with the Scheffelfelsen is a striking landmark of the Main Valley. It forms the northwesternmost branch of the Franconian Alb. There are several small caves below the summit plateau. The summit area was released in 2001. | 30000 150 × 200 |
Type: Inselberg / Zeugenberg Type: Dolomite stone, limestone |
Rock slope / cliff | precious | Nature reserve, landscape protection area, FFH area | Bavaria's most beautiful geotopes No. 74 |
Ponordoline SE from Görau | 478R030 |
Weismain position |
Obermain-Bruchschollenland | The relatively large sinkhole right next to the Görau cemetery chapel is located in the area of an agricultural area, is free of disruptive vegetation and therefore very noticeable. In contrast to some water-filled depressions in the inflow area, the sinkhole floor is relatively dry, which speaks for an active ponor (swallow hole), since the surface water evidently seeps away very quickly. | 800 40 × 20 |
Type: Ponor Type: Limestone |
Sinkhole / sinkhole | precious | Landscape protection area, nature park |
See also
- List of nature reserves in the Lichtenfels district
- List of landscape protection areas in the Lichtenfels district
- List of FFH areas in the Lichtenfels district
Individual evidence
- ↑ Data source: Bavarian State Office for the Environment, www.lfu.bayern.de, Geotoprecherche (accessed on September 16, 2017)
Web links
Commons : Geotopes in the Lichtenfels district - collection of images, videos and audio files