List of geotopes in the district of Kulmbach
This list contains the geotopes of the Upper Franconian district of Kulmbach 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 |
---|---|---|---|---|---|---|---|---|---|---|---|
Former Basalt quarry on Patersberg NNE by Veitlahm | 477A001 |
Kulmbach position |
Obermain-Bruchschollenland | In the former quarry in the tertiary basalt, a 4–5 m wide basalt dike and in the contact zone fritted Opalinus Clay of Dogger Alpha are exposed. | 1500 50 × 30 |
Type: Contact, Rock Type: Basalt, Mudstone |
Quarry | significant | Landscape protection area | ||
Former Sand pit NW of Burghaig, Lindig | 477A002 |
Kulmbach position |
Obermain-Bruchschollenland | The former sand pit is laid out in the Rhaetian sandstone, lively cross-stratification can be seen in places, and plant fossils can be found in clay lenses. In the non-filled areas there is heather-like succession vegetation. | 6000 150 × 40 |
Type: Rock Type: Sandstone |
Gravel pit / sand pit | significant | no protected area | ||
Former Muschelkalkbruch SE from Herlas | 477A003 |
Kulmbach position |
Obermain-Bruchschollenland | In the abandoned quarry in the main Muschelkalk, the kinking of the layers by 90 degrees, contrary to the original location, can be seen due to the action of the Kulmbach disturbance. The strata are rich in fossils. Access to the quarry is blocked by a gate. | 4800 120 × 40 |
Type: Flexure, Animal Fossils, Rock Type: Limestone |
Quarry | especially valuable | Landscape protection area, natural monument | ||
Former Sand pit NNE from Kessel | 477A004 |
Kulmbach position |
Obermain-Bruchschollenland | The former sand pit is located in the lower red sandstone, the hanging wall is formed by Kulmbach conglomerate. Well recognizable cross stratification and clay barrels, isolated basement gravel. | 900 30 × 30 |
Type: Layer sequence Type: Sandstone |
Gravel pit / sand pit | significant | no protected area | ||
Sandstone rocks at the Küfner inn in Buchau | 477A005 |
Mainleu's position |
Obermain-Bruchschollenland | The Rhaetian sandstone rocks are in the garden of the Küfner inn. | 200 40 × 5 |
Type: Rock Type: Sandstone |
Slope crack / rock wall | significant | no protected area | ||
Former Sandstone quarry at Veitsgraben (southern part) | 477A008 |
Ködnitz position |
Obermain-Bruchschollenland | Abandoned quarry in the upper (light) slab sandstone. | 1000 50 × 20 |
Type: Rock Type: Sandstone |
Quarry | significant | no protected area | ||
Former Sandstone quarry at Veitsgraben (northern part) | 477A009 |
Ködnitz position |
Obermain-Bruchschollenland | Abandoned quarry in the lower and upper slab sandstone, upward transition to the myophoric layers. | 3000 100 × 30 |
Type: Layer sequence Type: Sandstone |
Quarry | significant | no protected area | ||
Former Shell limestone quarry NE of Feuln | 477A010 |
Trebgast position |
Obermain-Bruchschollenland | In the disused, partially overgrown quarry, Upper Muschelkalk is pending. Trace fossils (bioturbation) are common. Occasionally, signs of (paleo -?) Karst phenomena, such as B. sinter formation can be observed (Fig. 3: Calcite crystals in a crevice). The break became particularly important in 1910, when parts of the skull of the dinosaur Placodus gigas were found here. From 1895 to 1987 the lime was processed into building material and fertilizer lime in two directly adjacent lime kilns. The Trebgast-Feuln geo-path created as part of a school project leads, among other things, to the break ground (geo-point no. 6 - Fig. 4). | 3000 100 × 30 |
Type: Animal Fossils, Trace Fossils, Lime Kiln, Rock Type: Limestone |
Quarry | precious | no protected area | ||
Former Sand pit SW of Pechgraben (Meyersche Sandgrube) | 477A013 |
Neudrossenfeld position |
Obermain-Bruchschollenland | In the vicinity of the abandoned sand pit there are others, e.g. Some sand pits are still being mined. | 20000 200 × 100 |
Type: Rock Type: Sandstone |
Gravel pit / sand pit | significant | Landscape protection area | ||
Former Sand pit N of Sandreuth | 477A014 |
Harsdorf position |
Obermain-Bruchschollenland | The only outcrop in the Lower Buntsandstein in the district of Kulmbach is in the abandoned sand pit. | 3000 100 × 30 |
Type: Rock Type: Sandstone |
Gravel pit / sand pit | significant | Landscape protection area | ||
Road outcrop between Gumpersdorf and Untersteinach | 477A015 |
Below by position |
Obermain-Bruchschollenland | The corrugated limestone outcrop is located on a road embankment. | 150 30 × 5 |
Type: Rock Type: Limestone |
embankment | precious | no protected area | ||
Former Quarry NE of Gumpersdorf | 477A016 |
Below by position |
Obermain-Bruchschollenland | Old quarry in the Wellenkalk. | 200 20 × 10 |
Type: Rock Type: Limestone |
Quarry | significant | no protected area | ||
Outcrop at the Rauschenhammermühle | 477A018 |
Schwarzenbach am Wald position |
Franconian Forest | Greywacken and slate alternation with slip folds and sliding bodies of different ages. Fossil finds are possible in the lower graptolite schists. A large sandstone block probably comes from the Ordovician . | 250 50 × 5 |
Type: Standard / Reference Profile, Animal Fossils Type: Mudstone |
embankment | especially valuable | Landscape protection area, nature park | ||
Former Limestone quarry E from Köstenhof | 477A019 |
Presseck position |
Franconian Forest | The former quarry in the Upper Devonian Flaserkalk shows a cephalopod and conodont fauna. The lime is covered by sub-carbon clay slates (with fauna). | 10000 100 × 100 |
Type: Rock, Animal Fossils Type: Limestone |
Quarry | especially valuable | Landscape protection area, nature park | ||
Pinging of the Carl Wilhelm colliery at the Forstmeister jump | 477A020 |
Stadtsteinach position |
Franconian Forest | The Schurf lies above the Forstmeistersprung rock. Between the scrape and the rock there is a complete profile with diabastuff, red iron border camp, lime tuber slate and lime. | 2000 100 × 20 |
Type: Sequence of layers, Pinge / nfeld Type: Limestone |
Ping | especially valuable | Nature reserve, landscape protection area, FFH area | ||
Weinleite E from Burghaig | 477A021 |
Kulmbach position |
Obermain-Bruchschollenland | The impact slope and an old quarry are in the area of the lower and middle castle sandstone and are strongly overgrown and collapsed. | 6000 150 × 40 |
Type: Sequence of layers, impact slope Type: Sandstone |
Slope crack / rock wall | significant | no protected area | ||
Former Diabase quarry Schindelbachtal NE from Unterauberach | 477A022 |
Stadtsteinach position |
Franconian Forest | The former diabase quarry opens up massive diabase sandstone, some sections with pillows and a storage area for scarf stones. | 22500 150 × 150 |
Type: Rock Type: Basalt |
Quarry | significant | Natural park | ||
Rocks below the Nordeck ruins | 477A023 |
Stadtsteinach position |
Franconian Forest | The reference profile of the cephalopod stratigraphy of the Upper Devonian in the Franconian Forest is open. An approximately 1 km long hiking trail leads to the ruin, which has now been exposed. On the northeast side there is access to a short karst cave. | 500 50 × 10 |
Type: Standard / Reference Profile, Animal Fossils, Karst Horizontal Cave Type: Limestone |
Slope crack / rock wall | especially valuable | Nature reserve, landscape protection area, FFH area | ||
Pinge E of the Nordeck ruin | 477A024 |
Stadtsteinach position |
Franconian Forest | In the partially overgrown and dilapidated outcrop, the transgressive overburden with chute fillings of carbonic coal lime on lime lime of the deeper Upper Devonian is exposed. | 35 7 × 5 |
Type: sequence of layers, pinge field, karst chimney, karst crevice Type: limestone |
Ping | significant | Nature reserve, landscape protection area, FFH area | ||
Street embankment at the blast furnace NE of Stadtsteinach | 477A025 |
Stadtsteinach position |
Franconian Forest | The profile of the Thuringian Ordovician, which is now heavily overgrown with trees, can still be seen in numerous outcrops. | 2000 200 × 10 |
Type: Layer sequence Type: Mudstone |
embankment | precious | Landscape protection area, nature park | ||
Former Keratophyrbruch on Torkel NW of Vogtendorf | 477A026 |
Guttenberg position |
Franconian Forest | The heavily fissured rock is quite fresh and shows typical feldspars. | 150 15 × 10 |
Type: Rock Type: Trachyte |
Quarry | precious | Natural park | ||
Profile in Streichengrund SE from Guttenberg | 477A027 |
Guttenberg position |
Franconian Forest | The profile shows diabase overlaid with dark slates and greenish sandstones (with Lower Devonian fauna and microflora). | 5000 250 × 20 |
Type: Layer sequence Type: Basalt |
Slope crack / rock wall | precious | Natural park | ||
Cambrian on Galgenberg S of Premeusel | 477A028 |
Presseck position |
Franconian Forest | The Central Cambrian Galgenberg Strata are among the oldest fossil-bearing rocks in Bavaria. They are only known on Galgenberg. Small pits are here z. Currently still kept open by collectors. | 500 50 × 10 |
Type: Type locality, Animal Fossils Type: Mudstone |
Schurf | especially valuable | Natural park | ||
Elbersreuther Orthoceratenkalk S from Schübelhammer | 477A029 |
Presseck position |
Franconian Forest | The profile includes strata from the Silurian to the Upper Devonian in patchy threshold facies. Only the fossil-rich Orthoceratenkalk is visible today, but the profile could easily be excavated. | 50 10 × 5 |
Type: Type locality, Animal Fossils Type: Limestone |
Quarry | precious | Landscape protection area, nature park | ||
Former Quarry in the Flemersbachtal SW of Elbersreuth | 477A030 |
Presseck position |
Franconian Forest | The former quarry shows a profile in overturned storage, which contains the following layers: tuffites with graptolites with silica slate concretions, Silurian orthocerate limestone, vents in orthocerate limestone filled with black silica limestone and fossil-rich tentaculite limestone. | 8 4 × 2 |
Type: Standard / Reference Profile, Animal Fossils, Karst Vent, Karst Fissure Type: Limestone, Mudstone |
Quarry | especially valuable | Landscape protection area, nature park | ||
Quarries in the Trebgaster Buntsandstein | 477A031 |
Harsdorf position |
Obermain-Bruchschollenland | On the hilltop between Trebgast and Harsdorf there are several quarries in the Trebgaster Buntsandstein (Upper Slab Sandstone) with partly very good, otherwise hardly any outcrops. | 3000 150 × 20 |
Type: type locality, rock type, layer sequence type: sandstone |
Quarry | precious | Landscape protection area | ||
Amphibolite quarry in Schorgasttal | 477A032 |
Wirsberg position |
Münchberger Gneissasse | In the Schorgasttal east of Wirsberg, coarse-grained Rand amphibolite was mined as gravel and for masonry until 1960. The abandoned quarry is located on the geological nature trail through the Schorgasttal and was released in 2011. This is the best exposure in the coarse-grained variety of the Rand amphibolite in the entire Münchberg mass. | 5000 100 × 50 |
Type: Rock type, Metamorphic structure Type: Amphibolite |
Quarry | precious | Landscape protection area, nature park | ||
Prasinitbruch in Schorgasttal | 477A033 |
Wirsberg position |
Münchberger Gneissasse | At the entrance of the Schorgasttal there is a small former quarry in Prasiniten der Münchberger Masse. Today the area has been redesigned into a park, a plaque commemorates the Wirsberg honorary citizen Johannes Rode. The break is on the geological nature trail through the Schorgasttal and shows the Prasinite in well-preserved outcrops. | 200 20 × 10 |
Type: Rock type, Metamorphic structure Type: Prasinite |
Quarry | precious | Landscape protection area, nature park | ||
Algae lime clod in the Rauschbachtal S Heinersreuth | 477A034 |
Presseck position |
Franconian Forest | At the foot of the slope east of the Rauschbach there is a hardling rib with sparse outcrops of dark gray, laminated limestone. Sub-Cambrian archaeocyathids were found in this rock, which only occurs here in Bavaria in the form of a sliding block. These are the oldest macrofossils in Bavaria. The subcarbone matrix (Grauwacken clay slate series) can only be guessed from a few reading stones. About 50–100 m north and south there are small outcrops and frequent reading stones from coarse Heinersreuth block conglomerate. This is also on the opposite side of the stream in the embankment of a new forest road. The property is particularly protected as a natural monument (ordinance of the Kulmbach District Office of June 6, 2016, Az .: SG 34-1733-518 / pü). Damage or changes (including the taking of samples) will be punished as an administrative offense with a fine of up to 50,000 euros. | 5 5 × 1 |
Type: Standard / reference profile, layer sequence, sediment structures, animal fossils Type: Limestone, breccia, conglomerate |
Slope crack / rock wall | especially valuable | Natural monument, nature park | ||
Meta-gabbronorite on the cairn NW of Höflas | 477A035 |
Marktschorgast position |
Münchberger Gneissasse | The cairn near Streitau is built from Meta-Gabbronorite, which is interpreted as an intrusive body in the paragneiss of the reclining series. This extremely hard and weather-resistant rock forms a sea of boulders in the summit area of the stone hill, which is, however, heavily overgrown. There is a small quarry on the western slope of the summit. This is the only good outcrop in this rare rock of the Münchberg mass. The outcrop is remote and can only be reached without paths. | 600 30 × 20 |
Type: Rock, Sea of Boulders Type: Meta-Gabbro |
Quarry | precious | Natural park | ||
Keratophyrtuff in Wirsberg | 477A036 |
Wirsberg position |
Franconian Forest | Directly on the hiking trail KU14 of the Franconian Forest Association there is a scenic outcrop in Keratophyrtuffen of the marginal slate series on the outskirts of Wirsberg. This is the best outcrop of these rocks in a wide area. | 150 15 × 10 |
Type: Rock type, rock wall / slope Type: Meta-Trachyte, Meta-Tuffit |
Rock slope / cliff | precious | Natural park | ||
Quarry south of Tannfeld | 477A037 |
Thurnau position |
Northern Franconian Alb | Limestone blocks were mined in the small, abandoned quarry south of Tannfeld. The sponge limes of the Lower Malm are exposed in the quarry. | 900 30 × 30 |
Type: Rock Type: Limestone |
Quarry | significant | Natural park | ||
Gäbelein-Schmiedel gallery in Kulmbach | 477G001 |
Kulmbach position |
Obermain-Bruchschollenland | The medieval tunnel system in the Kulmbach conglomerate was built as a beer cellar. | 4000 80 × 50 |
Type: rock cellar, tunnel, rock type: sandstone |
Tunnel / gallery / shaft | precious | no protected area | ||
Steinerner Vogelherd NE from Leuchau |
|
477G002 |
Kulmbach position |
Obermain-Bruchschollenland | The age and function of the anthropogenic, circular depressions with steps in the rock sandstone is unknown. | 9 3 × 3 |
Type: Wrought Rock Type: Sandstone |
Schurf | significant | no protected area | |
The Langheimer Amtshof gallery in Kulmbach | 477G003 |
Kulmbach position |
Obermain-Bruchschollenland | The medieval tunnel system in the Kulmbach conglomerate is located under the Langheimer Amtshof in Kulmbach. It is a main corridor with 7 secondary tunnels (walkable corridor length 250 m), which were created largely following the natural fissures. | 500 250 × 2 |
Type: rock cellar, tunnel, rock type: sandstone |
Tunnel / gallery / shaft | precious | no protected area | ||
Engelhardt tunnel system, Schwanenbräukeller, in Kulmbach | 477G004 |
Kulmbach position |
Obermain-Bruchschollenland | The old tunnel system in the main red sandstone was used to mine sand and sandstone and as a cellar. It is one of 70 tunnels in Kulmbach. | 540 90 × 6 |
Type: rock cellar, tunnel, rock type: sandstone |
Tunnel / gallery / shaft | precious | no protected area | ||
Adventure mine St.-Veit-Zeche Kupferberg | 477G007 |
Kupferberg position |
Franconian Forest | This new show mine will open in April 2015 in the area of the historic St. Veit - colliery of the copper mining area Kupferberg-Wirsberg. | 0 not specified |
Type: Stollen Type: non-ferrous metal ore, slate, meta-basalt |
Tunnel / gallery / shaft | precious | Natural park | ||
Karst spring Weihersbrunnen N of Alladorf |
|
477Q001 |
Thurnau position |
Northern Franconian Alb | The karst spring from the lower Malm shows strong fluctuations in discharge (average approx. 50 l / s). | 100 10 × 10 |
Type: layer source, rock type: limestone |
Slope crack / rock wall | precious | Natural monument, landscape protection area, nature park | |
Friesenquelle SW of Kasendorf |
|
477Q002 |
Kasendorf position |
Northern Franconian Alb | There is little tufa formation below the strong karst spring from the lower Malm. | 100 10 × 10 |
Type: Layer Source Type: Limestone |
no information | precious | Natural monument, FFH area, nature park | |
Teufelsfelsen WNW von Veitlahm (Big Stone) |
|
477R001 |
Mainleu's position |
Obermain-Bruchschollenland | The Teufelsfelsen show limonite rinds and Tafoni weathering. | 600 30 × 20 |
Type: Rock wall / slope, Tafoni / honeycomb weathering Type: Sandstone |
Slope crack / rock wall | precious | Landscape protection area | |
Waterfall NW from Veitlahm |
|
477R002 |
Mainleu's position |
Obermain-Bruchschollenland | A 5 m high waterfall falls over a steep step in the Rhätsandstein. By fluvial erosion, harder layers were prepared here, so that covings were created. | 90 3 × 30 |
Type: Waterfall, Rock Type: Sandstone |
Impact slope / river bed / stream profile | precious | Landscape protection area | |
Steinachklamm SSW from Wildenstein |
|
477R003 |
Presseck position |
Franconian Forest | To the south of Wildenstein there is a large quartz keratophyr slide within the sub-carbonic sediments. The gorge represents the breakthrough of the Steinach through the hard quartz keratophyr. | 3750 150 × 25 |
Type: Klamm Type: Meta-Rhyolite, Meta-Trachyte |
Impact slope / river bed / stream profile | precious | Natural monument, landscape protection area, FFH area | Bavaria's most beautiful geotopes No. 64 |
Waterfall E from Eggenreuth | 477R004 |
Kulmbach position |
Obermain-Bruchschollenland | In the lower flat sandstone (Kulmbacher facies) a steep step is formed, over which a small waterfall pours. | 15 3 × 5 |
Type: Waterfall, Rock Type: Sandstone |
Impact slope / river bed / stream profile | precious | no protected area | ||
Schwedenschanze SE rock slope from Höfstätten | 477R005 |
Kulmbach position |
Obermain-Bruchschollenland | The rock formation in the Rhätsandstein shows a fissure spring and cavernous weathering forms. | 400 40 × 10 |
Type: rock wall / slope, Tafoni / honeycomb weathering, constriction source Type: sandstone |
Slope crack / rock wall | precious | Landscape protection area | ||
Dolinenfeld on the Great Espich NW of Untersteinach | 477R006 |
Below by position |
Obermain-Bruchschollenland | The sinkhole field consists of several sinkholes of various sizes. The largest (Hutweiher) is filled with water and has a biotope function. | 90000 300 × 300 |
Type: Dolinenfeld Type: Limestone |
no information | precious | no protected area | ||
Hollow road near Menchau | 477R007 |
Thurnau position |
Obermain-Bruchschollenland | Iron-bearing horizons and limonite rinds can be seen in the ravine in the Dogger beta sandstone. It is planned to protect the ravine as a LB. | 1000 50 × 20 |
Type: Rock Wall / Slope Type: Sandstone |
Pit / canal / ravine | significant | Natural park | ||
Sanspareil rock garden |
|
477R008 |
Wonsee's position |
Northern Franconian Alb | The rock area contains several caves, is developed for tourists and is a listed building. | 10500 700 × 15 |
Type: rock wall / slope, karst horizontal cave Type: dolomite stone |
Slope crack / rock wall | significant | Monument protection, landscape protection area, nature park | |
Long stone (Zschokke rock) SE from Sanspareil |
|
477R009 |
Wonsee's position |
Northern Franconian Alb | The rock tower in the spongy limestone of the Middle Kimmeridge strata shapes the landscape. | 600 20 × 30 |
Type: Rock Tower / Needle Type: Limestone |
Slope crack / rock wall | significant | Natural monument, landscape protection area, nature park | |
Rock slope E by Wonsees | 477R010 |
Wonsee's position |
Northern Franconian Alb | The distinctive rocky slope in the massive dolomite of the Middle Kimmeridge Strata (Malm Delta) characterizes the eastern valley slope. Bank joints suggest a dome-shaped reef structure. | 2100 70 × 30 |
Type: Rock wall / slope Type: Dolomite stone |
Slope crack / rock wall | significant | Landscape component, landscape protection area, nature park | ||
Rocks and caves in the NSG Kainachtal S of Wonsees | 477R011 |
Wonsee's position |
Northern Franconian Alb | The valley is bordered by rocks made of massive dolomite of the Middle Kimmeridge layers (Malm Delta), in which small karst caves and karst forms are formed. | 40000 400 × 100 |
Type: rock wall / slope, karst horizontal cave Type: dolomite stone |
Slope crack / rock wall | significant | Nature reserve, landscape protection area, FFH area | ||
Losauer Felsen NW of Losau | 477R012 |
Rugendorf position |
Franconian Forest | The Losau rock allows a very nice view of the foreland. | 2500 50 × 50 |
Type: Rock wall / slope Type: Basalt |
Slope crack / rock wall | precious | Natural monument, landscape protection area, nature park | ||
Schwalbenbachtal NNE from Schirradorf | 477R013 |
Wonsee's position |
Northern Franconian Alb | The Jura dry valley is very scenic due to its rocks. The karst treasure trove also includes hunger wells and caves (e.g. bell hole cave). | 100000 500 × 200 |
Type: dry valley, rock tower / needle, karst horizontal cave, narrowing source Type: dolomite stone |
Slope crack / rock wall | precious | Landscape protection area, nature park | ||
Serpentinitkuppe Peterleinstein NE by Kupferberg |
|
477R014 |
Kupferberg position |
Münchberger Gneissasse | The Peterleinstein is a predominantly wooded rocky hilltop, which, however, offers good outcrops of serpentinite in the summit area. Various mineral finds, such as bronzite and chrysotile, have been described from the dark green rock. The name of the Peterleinstein can be traced back to the paterln (glass beads for rosaries), which were previously made from the stone. | 5000 100 × 50 |
Type: Crag, Type of Rock, Mineral Type: Serpentinite |
Rock slope / cliff | precious | Landscape component, FFH area, nature park | |
Prasinite rocks at Kosereck NE of Wirsberg | 477R015 |
Wirsberg position |
Münchberger Gneissasse | Along the steep slopes in the area of the Kosereck north of Wirsberg there are numerous natural rock formations in green schists of the prasinite-phyllite series. The area is crossed by the hiking trail KU 14 of the Franconian Forest Association. At the southwestern end of the area there are large outcrops of massive prasinites directly on the hiking trail and on a newly built forest road (2015). Rock varieties, layer structures and fold formation can be studied particularly well here. These are the best freely accessible prasinite outcrops in the entire Münchberger mass. | 22500 450 × 50 |
Type: rock wall / slope, rock type, metamorphic structure, type: prasinite |
Rock slope / cliff | especially valuable | Landscape protection area, nature park | ||
Ilsestein NE from Wirsberg | 477R016 |
Wirsberg position |
Münchberger Gneissasse | Around the Ilsestein above the Golden Eagle Hut, there are several rock formations and outcrops in green schists of the Prasinit-Phyllit series. The rock pulpit of the Ilsstein offers a beautiful view of the Kosertal. | 100 20 × 5 |
Type: Ridge Type: Greenschist |
block | significant | Landscape protection area, nature park | ||
Phyllite rock Adlerstein NE from Wirsberg | 477R017 |
Wirsberg position |
Münchberger Gneissasse | To the northeast of Wirsberg is the rock castle of the Adlerstein on the slope of the Kosertal. It consists of phyllites of the prasinite-phyllite series and forms one of the few good outcrops of this rock in the entire Münchberg mass. The circular hiking trail KU12 (Goldener Falk Weg) of the Franconian Forest Association leads past the Geotop. | 300 30 × 10 |
Type: rock castle, rock type, metamorphic structure, type: phyllite |
Rock slope / cliff | precious | Landscape protection area, nature park | ||
Görauer Anger SE from Görau | 477R018 |
Kasendorf position |
Obermain-Bruchschollenland | The northeastern edge of the Franconian Jura forms a distinctive eaves along the Weismain Fault in the mass limestone of the Lower White Jura (Oxfordium), with a jump height of more than 50 m. The high plateau shows typical karst flora and numerous outcrops in the Malm limestone. The foot of the nw-se-running Görauer Angers is formed by Doggersandstein (Middle Jura, Upper Aalen layers). Iron ore was mined here in early and prehistoric times. The supraregional Frankenweg hiking trail runs right on the edge of the plateau. Numerous recesses on the hiking trail approx. 1000 m north of Zultenberg are of anthropogenic origin: After the end of the Second World War, explosive remains of the Wehrmacht were blown up in a controlled manner by the occupying forces. Several information boards provide information about geology, biology and history. | 960000 3200 × 300 |
Type: Layer level, Fault type: Limestone |
Slope crack / rock wall | precious | Landscape component, landscape protection area, FFH area | ||
Köstlerberg (Inselberg) SW of Trebgast | 477R019 |
Trebgast position |
Obermain-Bruchschollenland | The Köstlerberg in the Lindau basin SW of Trebgast is a morphologically striking relic of the otherwise uninstructive Pleistocene gravel terraces in the Trebgasttal. The shape and position of the mountain clearly show its origin. Today's Trebgasttal was created in the Pleistocene by the Steinach, which at that time still flowed north to the White Main. The Steinach initially formed a meander arch extending to the west, which was later cut off east of the Köstlerberg. The Köstlerberg was eroded as an island mountain out of the ice age gravel, which was up to 25 m high. The vegetation (forestry use) additionally increases the morphological conspicuousness of the property. Some small-scale, rolled and overgrown extraction points (Fig. 3) are former extraction points for deposited sand. | 30000 200 × 150 |
Type: Umlauf- / breakthrough mountain Type: Sand, gravel |
no information | especially valuable | Landscape protection area, FFH area |
See also
- List of nature reserves in the district of Kulmbach
- List of landscape protection areas in the district of Kulmbach
- List of FFH areas in the district of Kulmbach
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 district of Kulmbach - collection of images, videos and audio files