List of geotopes in the district of Kulmbach

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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 Steinerner Vogelherd Kulmbach (1) .JPG
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 Weihersbrunnen (Alladorf) .JPG
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 Friesenquelle1.jpg
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) Teufelsfelsen west of Veitlahm.JPG
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 Waterfall in the Vatsbrunn Graben near Veitlahm.JPG
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 Steinachklamm rock massif.jpg
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 Sanspareil Split Rock.JPG
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 Sanspareil rock garden Zschokkefelsen 001.JPG
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 Peterleinstein.JPG
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

Individual evidence

  1. 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