List of geotopes in Middle Franconia

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The list of geotopes in Middle Franconia automatically includes the following lists of geotopes in Middle Franconian counties and cities from the article namespace:

The selection corresponds to the administrative region Middle Franconia .

This list is incomplete. Around 3,400 geotopes are recorded in the Bavarian geotope register. The Bavarian State Office for the Environment (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 Quarry on the Hesselberg NE of Gerolfingen 2017 Hesselberg 03.jpg
571A001 Gerolfingen
position
Southwest Albrand region The quarry on the Hesselberg opens up the border between Malm Gamma and Beta and is rich in fossils. 5000
100 × 50
Type: Layer sequence, Animal fossils
Type: Limestone
Quarry precious Landscape protection area, FFH area Bavaria's most beautiful geotopes No. 28
Quarry NE of Wittelshofen 571A002 Wittelshofen
position
Southwest Albrand region In the quarry, the layer sequence Posidonia slate / Jurensis marl / Opalinus Clay is exposed. The outcrop is fenced in to prevent the overexploitation of fossils. Information boards are set up. Fossil-rich Posidonia schist fragments can also be found outside the fence. 10000
200 × 50
Type: Layer sequence, Animal fossils
Type: Mudstone
Clay pit / clay pit / marl pit precious Natural monument, landscape protection area
Former SSE quarry in Illenschwang 571A003 Wittelshofen
position
Southwest Albrand region Former quarry on the edge of a rubble dump that opens up the border between ariet sandstone and angulate sandstone . The Angulate sandstone here is rich in rounded concretions that are locally called Swedish spheres. 1200
40 × 30
Type: Layer sequence
Type: Sandstone
Quarry precious Natural monument
Former Quarry SE from Wilburgstetten 571A004 Weiltingen
position
Southwest Albrand region Former break in ariet sandstone, today almost completely overgrown. 10000
100 × 100
Type: Rock
Type: Sandstone
Quarry precious Natural monument
Former sand pit NE von Winden 571A005 Leutershausen
position
Sandstone Keuper Region Former sand pit near Winds , on the outcrop wall of which sedimentary structures in the bubble sandstone are clearly visible. 40
20 × 2
Type: Rock
Type: Sandstone
Gravel pit / sand pit significant Landscape component, landscape protection area, nature park
Former quarry NW of Vorbach 571A006 Rothenburg ob der Tauber
position
Eastern Franconian Plates The quarry near Vorbach provides an insight into the rock sequence of the Upper Muschelkalks at the transition to the rectangular limestone facies. 15000
150 × 100
Type: Rock
Type: Limestone
Quarry precious FFH area, bird sanctuary, nature park
Gypsum break SSE from Endsee Gypsum break Endsee.JPG
571A007 Steinsfeld
position
Gypsum Keuper Region The lower myophoric layers are exposed in the gypsum quarry , it is one of the “100 most beautiful geotopes in Bavaria” . Marl banks and plaster layers follow over base gypsum (7 m). Haunschild described here galena Bank as light gray, fossil-free stone marl location with Kalkspatdrusen . 16000
200 × 80
Type: Rock type, tunnels, carts / fields, folds / troughs / saddles
Type: plaster, mudstone
Quarry significant Landscape component, landscape protection area, FFH area Bavaria's most beautiful geotopes No. 10
Marl pit N of Cadolzhofen 571A008 Windelsbach
position
Gypsum Keuper Region In the marl pit north of Cadolzhofen , layers of estheria are exposed . The rock consists mainly of dark gray clays and marls with white plaster strings. 3000
150 × 20
Type: Rock
Type: Marlstone
Clay pit / clay pit / marl pit precious Nature reserve, landscape protection area, FFH area
Former clay pit N of Burghausen 571A009 Windelsbach
position
Gypsum Keuper Region In the former clay pit north of Burghausen , mainly gray to greenish black clay stones and marls from the Estherian layers have been developed. Plaster layers are occasionally turned on in the lower area. 3000
100 × 30
Type: Rock
Type: Clay Marlstone
Clay pit / clay pit / marl pit significant Landscape component, landscape protection area, nature park
Former Clay pit NE of Bellershausen 571A010 Diebach
position
Gypsum Keuper Region In the clay pit near Bellershausen , the border between myophoria and estheria layers is exposed. 3000
100 × 30
Type: Layer sequence
Type: Mudstone
Clay pit / clay pit / marl pit significant Landscape protection area, nature park
Former clay pit N von Gastenfelden 571A011 Book at the forest
position
Gypsum Keuper Region In the former clay pit near Gastenfelden , a displacement of approx. 150 cm can be seen in the outcrop in the Lehrberg layers . 4000
200 × 20
Type: Rock type, Fault
type: Clay marl
Slope crack / rock wall precious Nature reserve, landscape protection area, FFH area
Street outcrop N of Seitendorf 571A012 Heilsbronn
position
Sandstone Keuper Region The road outcrop near Seitendorf shows the type locality of the Seitendorf intermediate layers. According to Fuchs (1959) this is a sequence of bubble sandstone in which sandstone and Latvian layers alternate. 150
50 × 3
Type: Standard / Reference Profile
Type: Sandstone
embankment precious Natural monument
Former marl pit SW of Auerbach 571A013 Colmberg
position
Sandstone Keuper Region In the overgrown part of the Auerbach marl pit , the "Frommetsfeldener fault" was previously exposed, where the Lehrberg layers bordered on sandstone reeds. Today only Lehrberg layers are recognizable, in 2010 only the northern part was preserved. The rest is completely overgrown and partly recultivated. 40
20 × 2
Type: fault, rock
type: marlstone
Clay pit / clay pit / marl pit precious Natural monument, landscape protection area, nature park
Former sand pit NE of Rühlingstetten 571A014 Wilburgstetten
position
Southwest Albrand region Former sand pit near Rühlingstetten , in which white to reddish, mostly unsolidified sandstones with kaolinized feldspars from the Upper Castle sandstone are exposed . 10000
100 × 100
Type: Rock
Type: Sandstone
Slope crack / rock wall significant Natural monument
Gorge SE from Schlierberg 571A015 Ehingen
position
Southwest Albrand region In the valley of the Kesselbach , the complete sequence of layers of the hettangium (psilonate layer, angulate sandstone) is exposed. The outcrops are easily accessible on the upper stream, but are partly covered by debris. The lower stream is heavily overgrown. Some of the outcrops are rich in fossils. 15000
150 × 100
Type: Rock type, stream / river course
Type: Sandstone
Impact slope / river bed / stream profile precious Natural monument
Clay pit NNE by Schwand 571A016 Leutershausen
position
Gypsum Keuper Region In the clay pit near Schwand , the Lehrberg layers are open. They are up to 10 m thick here, and their benches are easily recognizable over a length of 100 m. The pit is used by the city of Leutershausen. 2000
100 × 20
Type: Rock
Type: Marlstone
Clay pit / clay pit / marl pit precious Landscape protection area, nature park
Bubble sandstone outcrop at Rüdern 571A017 Dietenhofen
position
Sandstone Keuper Region In the case of Rüdern , inclined sandstone is exposed in alternation with clay stones. 80
20 × 4
Type: sedimentary structures, rock
type: sandstone, mudstone
embankment precious Natural park
Dogger outcrop on Hesselberg NW of Wittelshofen 571A018 Gerolfingen
position
Southwest Albrand region In the middle part of the geological nature trail on the Hesselberg, a small dig opens up the approximately 1 m thick sand-lime brick of the Dogger Gamma, including the overlying and underlying layers. Information boards point out the fossils in the sand-lime brick. 12
6 × 2
Type: Layer sequence
Type: sandstone, marlstone
Schurf precious Landscape protection area, FFH area
Castle sandstone outcrop NE of Fürnheim 571A019 Wassertrüdingen
position
Southwest Albrand region At the outcrop near Fürnheim you can see coarse-grained, sloping upper castle sandstone with numerous mudstone rubble. 200
40 × 5
Type: sedimentary structures, rock
type: sandstone, gravel
embankment precious no protected area
Road exposure SSE from Oberoestheim 571A021 Diebach
position
Gypsum Keuper Region High road embankment near Oberoestheim , where layers of plaster of paris are exposed . Easily accessible for good excursions because of the parking lot opposite. 250
50 × 5
Type: Rock
Type: Marl, Gypsum
embankment precious Landscape protection area, nature park
Gypsum karst spring Bottomless hole Bottomless Hole2.JPG
571Q002 Diebach
position
Gypsum Keuper Region The karst spring Bodenlos Loch SW of Unteroestheim lies in the area of ​​the base gypsum. It is a 15 m wide spring pot with a depth of approx. 6 m. 300
20 × 15
Type: Constriction Source
Type: Plaster of Paris
no information precious Natural monument, landscape protection area, nature park Bavaria's most beautiful geotopes No. 40
Hill slide W from Obergailnau 1295 landslide at GC170M0 = PAN, SHI = MTI = GPH.jpg
571R002 Wettringen
position
Gypsum Keuper Region In February 1958 there was a landslide west of Obergailnau below the Schloßberg . An approximately 120 m long and 20 m wide floe made of sandstone reed slid about 10 m. The reed sandstone is strongly fissured, which is why seeping water soaked the layers of estheria and myophoria underneath, which then served as a sliding surface. 7500
150 × 50
Type: landslide, rock
type: claystone
Slope crack / rock wall precious Natural monument, landscape protection area, FFH area
Malmkalkscholle Turtelberg W from Ostheim 571R003 Wassertrüdingen
position
Southwest Albrand region Distinctive little knoll west of Ostheim from Malmkalk on Bunter Breccia . The limestone clod was thrown into this place by the Ries event . 400
20 × 20
Type: Ejecta Material (Impact)
Type: Limestone
Slope crack / rock wall especially valuable no protected area
Doline N by Bettenfeld 571R004 Rothenburg ob der Tauber
position
Eastern Franconian Plates Ponordoline north of Bettenfeld (Rothenburg ob der Tauber) , which is only temporarily active. It is located in the Lower Keuper , in the subsoil there is karstified shell limestone . 80
10 × 8
Type: sinkhole
Type: mudstone, limestone
no information precious Natural park


Shift level NE from Rathsberg Wilderness at Rathsberg 008.JPG
562R001 Bubenreuth
position
Northern Albrand region Striking layer of the Rhätolias sandstone near Rathsberg . In the south the step breaks up into many small knolls and valleys. In the north exposure of the profile on a ten meter high rock face. Below is a rock fall with large sandstone blocks. 200000
2000 × 100
Type: Layer level, layer sequence
Type: sandstone, claystone
Slope crack / rock wall precious Nature reserve, landscape protection area
Former Sandstone quarries on the Hinteren Giesberg E von Dechsendorf Erlangen-Höchstadt district Hinterer Giesberg quarries 009.jpg
572A001 Mark
position
Sandstone Keuper Region Several old quarries in the Middle Burgsandstein near Dechsendorf . The walls are partly used for climbing. 250000
500 × 500
Type: Rock
Type: Sandstone
Quarry significant Landscape reserve, bird sanctuary
Former clay pit N von Marloffstein Marloffstein clay pit 005.JPG
572A002 Marloffstein
position
Northern Albrand region Disused clay pit in the Lias Delta with numerous fossils, e.g. B. Pyritized cephalopods . In Toneisensteinknollen also are barite , galena , pyrite and sphalerite find. 112500
450 × 250
Type: Standard / Reference Profile, Animal Fossils
Type: Clay Marlstone
Clay pit / clay pit / marl pit especially valuable no protected area
Exposure at the Wunderburg E von Marloffstein Wunderburg (Marloffstein) outcrop 001.JPG
572A003 Marloffstein
position
Northern Albrand region Old quarry in the Rhaetian sandstone , with plant clays on its west side. In the upper part, ariet sandstone has been developed in places. 700
70 × 10
Type: Layer sequence
Type: Sandstone
Quarry significant no protected area
Former Sand pit W of Kleinseebach 572A004 Möhrendorf
position
Sandstone Keuper Region Former sand pit in the castle sandstone and its base. Loose sandstone with quartz pebbles and sandstone pebbles. 37500
250 × 150
Type: Rock
Type: Sand
Gravel pit / sand pit significant Bird sanctuary
Lias outcrop in the Teufelsgraben S of Oedhof 572a005-Lias-Aufschluss-Teufelsgraben-Oedhof-3855.jpg
572A005 Eckental
position
Northern Albrand region Outcrop of rocks of the Lias Delta and Epsilon over a length of approx. 50 m. From bottom to top: approx. 1.3 m Lias Epsilon, the Amaltheenton Formation (Lias Delta), approx. 0.4 m marl slate with calcareous Siemensi tubers, three approx. 10 cm thick limestone banks separated by equally thick layers of marl slate , another 30 cm marl slate, 5 cm thick fossil-rich marl limestone (so-called belemnite battlefield ). 150
50 × 3
Type: Layer sequence, Animal fossils
Type: Mudstone, Marlstone
Impact slope / river bed / stream profile precious no protected area
Teufelsbadstube gorge in SW Kalchreuth Teufelsbadstube 05.jpg
572R001 Kalchreuther Forst
position
Northern Albrand region Gorge in the Rhätsandstein. Good outcrops at a waterfall, otherwise strongly overgrown. 37500
500 × 75
Type: Canyon, Rock
Type: Sandstone
Impact slope / river bed / stream profile significant Part of the landscape, bird sanctuary
Gründlach (stream bed) SW of Heroldsberg Gründlach 01.jpg
572R002 Kalchreuther Forst
position
Sandstone Keuper Region Meander , impact and sliding slopes of the green roof in its natural state. 150,000
1000 × 150
Type: meander, stream / river course, impact slope
Type: silt, sand
Impact slope / river bed / stream profile significant Part of the landscape, bird sanctuary


Former Quarries in the Fürth city forest W of Fürth Fürth quarry 05.jpg
563A001 Fürth
position
Sandstone Keuper Region The Lower Burgsandstein is developed in the still available outcrops in the Nuremberg facies. This consists of medium to coarse-grained sandstones, some of which are only slightly resistant to weathering. The sometimes very thick sandstone banks show oblique layers and show signs of cutting. 10000
100 × 100
Type: Rock
Type: Sandstone
Quarry significant Natural monument, landscape protection area, FFH area


Former clay pit E von Langenzenn 573A001 Langenzenn
position
Sandstone Keuper Region Stone marl banks and a red Letten parcel in the Lehrbergschichten are open-minded. There are several clay pits in the vicinity of the geotope, some of which are still in operation and some of which are in danger of being lost due to subsequent uses. During an inspection in 2010, the geotope was completely overgrown and the rock was only visible in erosion channels. 2000
100 × 20
Type: Layer sequence
Type: Clay marlstone
Slope crack / rock wall significant no protected area
Former Quarries at Druidenstein SE von Keidenzell 573A002 Langenzenn
position
Sandstone Keuper Region Several historical sandstone quarries in the Middle Burgsandstein, which also contains uranium-containing active agents. Nearby, a memorial stone reminds of the former rock formation. 1000
50 × 20
Type: Rock
Type: Sandstone
Quarry significant no protected area
Fault near Banderbach Banderbacher warping.jpg 573A003 Zirndorf
position
Sandstone Keuper Region The artificial embankment on the northeastern edge of the village opens up poorly consolidated clay and sandstones in the bubble sandstone. As a special feature, several fault areas can be seen here. A small floe was lifted about three meters between two closely spaced faults dipping northeast. An information board explains the geology at the outcrop. 30
15 × 2
Type: fault, rock
type: sandstone, mudstone
embankment precious Natural monument


Eastern quarry WNW of Obernzenn Illesheim Eastern Quarry Fingals Cave 002.JPG
575A002 Illesheim
position
Gypsum Keuper Region A red to brown reed sandstone with red iron stone lumps, pebbles and sediment structures is exposed. 6250
125 × 50
Type: Rock type, Sedimentary structures
Type: Sandstone
Quarry significant Landscape protection area, FFH area, nature park
Former Reed sand quarry NW of Obernesselbach 575A003 Neustadt an der Aisch
position
Gypsum Keuper Region It is one of the largest and best-preserved sandstone quarries in the district. It lies in the upper half of the reed sandstone layers, which are present here in the so-called flood formation. It shows many details that give clues to the formation of the reed sandstone (e.g. breaches with sliding folds). The quarry is also of historical value, as numerous buildings were built from the material of this quarry in the surrounding villages. 32500
250 × 130
Type: sedimentary structures, quarry / pit, rock
type: sandstone
Quarry precious Landscape reserve, bird sanctuary, nature park
Former Reed sand quarry SW of Humprechtsau 575A004 Market Nordheim
position
Gypsum Keuper Region In this quarry one finds negatives of silicified primitive coniferous plants from the Mesozoic. The break lies in the lower half of the reed sandstone layers in the so-called flood formation. 15000
300 × 50
Type: Vegetable Fossils, Quarry / Pit, Sedimentary Structures, Rock
Type: Sandstone
Quarry especially valuable Landscape reserve, bird sanctuary, nature park
Gypsum quarry on the Häfringsberg near Wüstphül 575A006 Market Nordheim
position
Gypsum Keuper Region The gypsum quarry on the Häfringsberg is still well preserved. It is a continuation of a drainage ditch of the fields further to the west (subrosion basin!). 1500
50 × 30
Type: Rock, Trench, Canal
Type: Gypsum
Quarry precious FFH area, nature park
Former plaster quarry Katzenloch near Bad Windsheim Former-Gipsbruch-Katzenloch-Bad-Windsheim.jpg
575A007 Bad Windsheim
position
Gypsum Keuper Region The former break gives a good insight into the sequence of layers of the base plaster. The stone was also used to build houses, for example the town hall in Bad Windsheim was built from Bad Windsheim plaster, known under the trade name. The area is fenced. 25000
200 × 125
Type: Standard / Reference Profile
Type: Plaster of Paris
Quarry precious Part of the landscape, nature park
Exposure wall in the ravine S from Untertief 575A008 Bad Windsheim
position
Gypsum Keuper Region The outcrop lies in the middle part of the myophoric layers. The missing galena bank is represented by a 0.30 m thick slate of gypsum. 400
40 × 10
Type: Layer sequence
Type: claystone, plaster
embankment significant Landscape protection area, nature park
Slope outcrop N of Unteresselbach 575A009 Neustadt an der Aisch
position
Gypsum Keuper Region In the slope outcrop near Unteresselbach, the border between the middle layers of estheria and the hanging sandstone reed is exposed. It is characterized by a breach layer of resident, mostly angular, fine sandstone and siltstone chunks. 1500
75 × 20
Type: Layer sequence
Type: claystone, sandstone
embankment significant Natural park
Oyster reef near Langensteinach 575A015 Uffenheim
position
Eastern Franconian Plates The oyster reef in the Upper Main Muschelkalk is designated as a protected part of the landscape. It is mentioned as an excursion point in numerous publications. In the otherwise well-banked limestone there is an approximately 3 m wide and 2 m high reef body, which consists almost entirely of oyster shells (Placunopsis). The oysters, which hindered each other's growth due to the dense population, are only about 1 cm in size. 400
40 × 10
Type: Standard / Reference Profile, Animal Fossils
Type: Limestone
Quarry especially valuable Part of the landscape, nature park
Former clay pit SE from Gunzendorf 575A017 Emskirchen
position
Sandstone Keuper Region The largely dilapidated outcrop opened up the upper part of the Lehrberschichten up to the first boundary bank of the bubble sandstone. 1000
50 × 20
Type: Layer sequence
Type: claystone, sandstone
Clay pit / clay pit / marl pit inferior Landscape protection area
Former quarry NE of Scheinfeld 575A018 Apparent field
position
Sandstone Keuper Region The surrounding rock is mostly thin banked and z. Sometimes developed in a slate manner, sedimentary structures (oblique stratification) are also evident. It is a typical channel formation, as there are layers of estheria 75 m to the west at the level of the upper edge of the break! On the western wall of the quarry, coal-like layers with chopped plants are exposed. 2500
50 × 50
Type: Rock type, Vegetable fossils, Sedimentary structures
Type: Sandstone
Quarry precious Natural park
Hohlweg and former quarry SE from Nenzenheim 575A019 Sugenheim
position
Gypsum Keuper Region Above the leveling of the Acrodus-Corbula horizon, the steep ascent through the Estheria layers begins at the level of the Judensee, which is covered by the channel filling of the reed sandstone. In the hollow path (quarry path) the typical features of the reed sandstone, such as ripple marks, oblique stratification and angle discordances, can be seen. 50000
500 × 100
Type: Rock type, Sedimentary structures
Type: Sandstone
embankment significant Landscape protection area, FFH area, bird sanctuary
Former quarry W von Birnbaum 575A021 Gerhardshofen
position
Sandstone Keuper Region The heavily buried wall shows the lower part of the lower castle sandstone. Beyond the road, the baselets of the Lower Burgsandstein spread out. There is a small cave at the foot of the quarry wall. 150
15 × 10
Type: Layer sequence, tunnel
type: Sandstone
Quarry significant no protected area
Street section SW of Uehlfeld 575A022 Uehlfeld
position
Sandstone Keuper Region This road exposure is suitable for placing the otherwise poorly exposed bubble sandstone under protection, as it is repeatedly released in the course of mowing work. 500
50 × 10
Type: Rock
Type: Sandstone
embankment significant Natural park
NNE reed sand quarry in Oberaltenbernheim 575A024 Obernzenn
position
Sandstone Keuper Region Red to brown colored massive reed sandstone, which merges into the teaching layers (Ansbacher sandstone) in the hanging wall, is open. 2000
100 × 20
Type: Layer sequence
Type: sandstone, clay marlstone
Quarry precious Landscape protection area, nature park
Former Gypsum break in Bad Windsheim Ost Former-Gipsbruch-Bad-Windsheim-Ost.jpg
575A026 Bad Windsheim
position
Gypsum Keuper Region The disused gypsum quarry is located in the middle of a new development area and has been converted into my biotope. The dismantling walls are z. Some of them are in very good condition and show large folds of swelling. The easily accessible break offers a good excursion point. 10000
200 × 50
Type: fold / trough / saddle, rock
type: plaster of paris
Quarry precious Natural park
Exposure ENE from Weimersheim 575A027 Ipsheim
position
Sandstone Keuper Region Just below the steep slope of the plateau, bubble sandstone is exposed here, partly clayey and partly sandy. In addition to quartz pebbles, the sandstone layers also contain deformed pebbles of clay marl up to about 2 cm in size. The layer boundary to the underlying Lehrberg layers lies in the lowest, heavily decayed part of the profile. 30
15 × 2
Type: sequence of layers, sediment structures
Type: claystone, sandstone
embankment significant no protected area
Former quarry Fingalshöhle WNW von Obernzenn Illesheim Fingals cave near Obernzenn 009.JPG
575G001 Illesheim
position
Gypsum Keuper Region In 1806, the former quarry served as field quarters for an Imperial French regiment for several months. French inscriptions as well as names of Seckendorff families are carved on the walls. In the protected part of the landscape, red reed sandstone with red iron stone lumps and pebbles (gutter filling) are exposed. Opposite the road there is an old quarry in a wood with traces of mining and sediment structures in the sandstone. 5000
100 × 50
Type: Quarry / Pit, Rock
Type: Sandstone
Quarry especially valuable Part of the landscape, ground monument
Felsenkeller SSE by Marktbergel 575G002 Marktbergel
position
Gypsum Keuper Region In a small space there are a total of 5 entrances to underground storage rooms in the reed sandstone. Three of them are solidly closed with grids, one is open and can be walked around 15 m. The deepest is about half filled with mud, its portal bears the year 1863. 90
30 × 3
Type: rock cellar, gallery
type: sandstone
Rock cellar significant Landscape protection area, FFH area, nature park
Gypsum cave Höllern S from Markt Nordheim Gypsum cave Höllern 02.jpg
575H001 Market Nordheim
position
Gypsum Keuper Region The corridors of the labyrinthine cave system are based on the fracture system in the base plaster and show the typical forms of the plaster solution. Depending on the groundwater level, the lower parts of the cave are more or less flooded. 450 000
1250 × 360
Type: Karst horizontal cave, sinkhole
Type: Gypsum
cave especially valuable Nature reserve, landscape protection area, FFH area
Source pot Walsbrunnen NE from Sontheim Walsbrunnen.JPG
575Q001 Illesheim
position
Gypsum Keuper Region The source pot is located in the myophoric layers. Due to the surrounding agricultural use, the spring pot shows a strong growth of algae. 28
7 × 4
Type: Constriction Source
Type: Plaster of Paris
no information precious Natural monument, landscape protection area, nature park
Häfeleinsbrunnen N gypsum karst spring from Bad Windsheim Häfeleinsbrunnen.JPG
575Q002 Bad Windsheim
position
Gypsum Keuper Region The small spring (a few l / s) rises from several water catchments in the immediate vicinity. The high electrical conductivity indicates a high proportion of dissolved gypsum in the water. 6
6 × 1
Type: Constriction Source
Type: Plaster of Paris
no information significant Natural park
Origin of the Aisch WSW from Illesheim Aischquelle1.JPG
575Q003 Burgbernheim
position
Gypsum Keuper Region The pooled spring at the resting place with the numerous side outlets in the vicinity represent a very important gypsum karst spring area. 12000
300 × 40
Type: Constriction Source
Type: Plaster of Paris
no information significant no protected area
Sandheidehügel WNW from Obernzenn Illesheim Sandheidehügel near Obernzenn 001.JPG
575R001 Illesheim
position
Gypsum Keuper Region The sand heather hill is a hardy made of reed sandstone. At the east end of the hill this was also dismantled. 2250
75 × 30
Type: Hardening
Type: Sandstone
Slope crack / rock wall precious Natural monument, landscape protection area, nature park
Sinkhole at Häfringsberg SE von Wüstphül 575R003 Market Nordheim
position
Gypsum Keuper Region It is an active sinkhole over a karst system in the base gypsum. Several small sinkholes are spread over the hill. Smaller caves have been explored. 100
10 × 10
Type: sinkhole
Type: clay marlstone
other information precious Natural monument, landscape protection area, FFH area
Külsheimer Hirtenhügel NE of Külsheim 575R004 Ipsheim
position
Gypsum Keuper Region Small, non-agricultural area. The wavy surface was created by leaching base plaster. 20000
200 × 100
Type: subrosion landscape, sinkhole
Type: plaster
no information significant Natural monument, FFH area, nature park
Gypsum hill Sieben Buckel W from Krautostheim Gypsum hill seven humps 04.jpg
575R005 Market Nordheim
position
Gypsum Keuper Region The gypsum hills seven humps represent a sinkhole landscape in the base gypsum with numerous small caves. To the north is the gypsum cave Höllern, a branched cave system that lies just below the surface and traces the rift pattern in the base gypsum (approx. 360 × 1250 m area). 150,000
500 × 300
Type: subrosion landscape, sinkhole, karst horizontal cave
Type: plaster of paris
other information especially valuable Nature reserve, landscape protection area, FFH area
Sinkhole on Hundsücken NW of Berolzheim 575R006 Bad Windsheim
position
Gypsum Keuper Region The relatively steep active sinkhole is already mentioned by Emmet (1969). It lies in the middle of a field and is open, although there is at least a small amount of backfilling (corn chaff, broken bricks, etc.). 64
8 × 8
Type: sinkhole
Type: mudstone, plaster
Sinkhole / sinkhole significant Natural park
Bach infiltration SE from Burgbernheim 575R007 Burgbernheim
position
Gypsum Keuper Region A small valley ends blindly in a large, approximately 10 m deep meadow hollow with a small ponordoline. Plaster of paris and clay stones of the myophoria layers are here. 400
20 × 20
Type: Ponor
Type: Plaster of Paris
Slope crack / rock wall precious Landscape protection area, nature park
Ponordoline SW from Marktbergel 575R008 Marktbergel
position
Gypsum Keuper Region A wide inlet ditch with several subsidence fields leads into a deep ponordoline with pending plaster of paris. It is the largest of its kind in the area. The inflow is at times over 10 l / s. 25000
250 × 100
Type: sinkhole, ponor
Type: plaster of paris
no information precious Landscape protection area, nature park
Külsheimer gypsum hill SE from Erkenbrechtshofen NSG Külsheimer Gipshügel 2.jpg
575R009 Bad Windsheim
position
Gypsum Keuper Region The Külsheim gypsum hills protrude gently over the terrain and are arranged in one or two rows. 62500
250 × 250
Type: Subrosion landscape
Type: Plaster of Paris
no information significant Nature reserve, FFH area, nature park
Witness mountain landscape ENE from Erkenbrechtshofen Zeugenbergandschaft-ENE-Erkenbrechtshofen.jpg
575R010 Bad Windsheim
position
Gypsum Keuper Region The witness mountains of the Vorderer and Hinterer Berg protrude from the Windsheimer Bucht by approx. 60 m. The base lies in the myophoria layers, the top layers are formed by the estheria layers. The summit plateau of the west-east facing double summit consists of the Acrodus-Corbula bank. 1050000
1500 × 700
Type: Inselberg / Zeugenberg, type of layers
: claystone
Rock slope / cliff precious Landscape protection area, nature park
Spring pot Königsbrunnen N from Schwebheim 575Q004 Burgbernheim
position
Gypsum Keuper Region The source pot of the Königsbrunnen is located below the Schwarzenbuck near Schwebheim and is used to hold fish. Further to the east there are further, partly enclosed springs, including the Rangau spring, a medicinal and mineral spring around 650 m away, and the abandoned water protection area of ​​Wiebelsheim. The spring water, which is already recognizable as having a high mineral content due to its characteristic color, comes from the myophoric layers, which explains increased sulfate concentrations. The Königsbrunnen feeds the heavily modified (straightened) flood ditch. Just a few meters west of the spring pot is a small rest area with a seating area. 125
25 × 5
Type: Constriction Source
Type: Plaster of Paris
no information significant no protected area


Maximiliansgrotte E from Krottensee (show cave) 2016 Maximiliansgrotte 03.jpg
371H001 Neuhaus an der Pegnitz
position
Northern Franconian Alb In the Franconian dolomite there is a widely branched floor system of corridors, chambers and halls. There are various sinter formations. Guided tours have been held here for the public since 1852. 10400
130 × 80
Type: Karst shaft & horizontal cave
Type: Dolomite stone
cave significant Natural monument, FFH area, nature park
Road cut below the town hall in Burgthann 2015 Geotop Burgthann 03.jpg
574A002 Burgthann
position
Southwest Albrand region Sandstones with a thickness of 4 m are exposed. The lower half is assigned to the Rhaetian transition layers, the hanging wall consists of ariet sandstone (Lias alpha 3). 375
75 × 5
Type: Layer sequence
Type: Sandstone
embankment significant no protected area
Former clay pit E from Reichenschwand 574a003-Tongrube-Reichenschwand.jpg
574A003 Reichenschwand
position
Northern Albrand region The clay pit opens up 8 m of Amaltheenton. Clay iron lumps up to a size of a few decimeters are particularly abundant. 14400
120 × 120
Type: Rock, Animal Fossils
Type: Mudstone
Clay pit / clay pit / marl pit precious Natural park
Former quarry N von Vorra 574A006 Forward
position
Northern Franconian Alb In the old quarry you can see the transition from factory limestone to sponge stump as well as clay-filled karst crevices. 30000
250 × 120
Type: Rock type, karst chimney, karst crevice
Type: Limestone
Quarry significant Landscape protection area, nature park
Former quarry NE of Schupf 574A007 Happurg
position
Middle Franconian Alb It is the only quarry in the district in which the fossil-rich Malm Gamma stratum facies is accessible. The break is used by sport shooters as a shooting range. 7000
100 × 70
Type: Rock, Animal Fossils
Type: Limestone
Quarry significant Landscape protection area, FFH area
Quarry NE of Happurg Quarry Happurg 03.jpg
574A009 Happurg
position
Middle Franconian Alb In this quarry, only the short east and north walls are accessible, as the remaining part is used by a rifle club. 4000
100 × 40
Type: Rock
Type: Limestone
Quarry inferior Landscape protection area, FFH area
Former quarry NW of Hartmannshof Hartmannshof 03.jpg
574A010 Pommelsbrunn
position
Northern Franconian Alb In the disused western part of the huge Hartmannshof quarry, there is a Malm standard profile. Resumption of mining is planned in the eastern part of the quarry. 22500
300 × 75
Type: Standard / Reference Profile
Type: Limestone
Quarry especially valuable Natural park
Former NNW quarry in Oberndorf 574A011 Simmelsdorf
position
Northern Franconian Alb The quarry is at risk from unauthorized backfilling. 15000
300 × 50
Type: Rock
Type: Limestone
Quarry significant Landscape protection area, nature park
Embankment on the Ludwig-Danube-Main Canal E from Dörlbach LMDK 18.jpg
574A012 Burgthann
position
Southwest Albrand region The canal embankments, especially at the canal bridge, give an insight into the sequence of layers of the Lower (Lias) to the Middle Jura (Dogger) from the Amaltheenton Formation to the Opalinus Clay Formation. At the time of the canal construction (1840–1841), this was the first major outcrop in these rocks in Franconia. Since then, it has been a classic reference profile. Many fossil finds have been made here, e. B. the 1.6 m long skull of the ichthyosaur Temnodontosaurus, which was found during the construction of the canal. After landslides in 2005 and 2008, the embankment was extensively renovated in 2010–2012. The fresh findings gave rise to a new scientific investigation. The embankment is on the Nuremberg - Kelheim cycle path, which runs along the canal here. 15000
500 × 30
Type: standard / reference profile, animal fossils, layer sequence, sediment structures
Type: clay marlstone
embankment especially valuable Landscape protection area
Former quarry SW of Regelsmühle 574A013 Alfeld
position
Middle Franconian Alb In the abandoned quarry, 2 reef pillars are exposed in the stratified limestone of the Lower Malm. The break has already been partially filled. 12500
250 × 50
Type: sedimentary structures, rock
type: limestone
Quarry precious Landscape protection area
Former quarry in the SW of Oberrieden Oberrieden quarry 04.jpg
574A014 Altdorf near Nuremberg
position
Middle Franconian Alb The walls of the quarry have partly collapsed here, which makes access to the outcrops much easier. 1500
50 × 30
Type: Rock
Type: Limestone
Quarry inferior Landscape protection area
Sand pits and dunes SW of Weißenbrunn NSG lichen 13.jpg
574A016 Winkelhaid
position
Southwest Albrand region The area west of Weißenbrunn is characterized by large deposits of Quaternary flying sands, some of which are underlain by terrace sands. The sands form elongated, mainly north-south running dunes. The landscape shows the typical vegetation of drift sand areas with sparse pine forests and blueberry and heather bushes. In the past, the sands were mined in many pits, today the area is designated as a nature reserve and partly as a water protection area. In the north and south there are two abandoned, very large sand pits. These pits, which are up to 40 meters deep, still have some free sand areas, but the internal sediment structures of the dunes and the underlay of the drift sand with terrace sand (with small pebbles) are no longer recognizable. The scenic area is accessible by several paths. A signposted cycle path leads past in the west (with a view of the southern sand pit), in the south and east the Franconian Dune Path leads through. 1200000
1500 × 800
Type: rock type, dune
type: sand
Gravel pit / sand pit precious Nature reserve, bird sanctuary, water reserve
Outcrop in the Steingraben W of Engelthal Exposure at Engelthal A017 01.JPG
574A017 Engelthal
position
Southwest Albrand region The limestone banks of the Lias Epsilon are exposed above the Amaltheenton. 1
2 × 0
Type: stream / river course, type of layers
: limestone
Impact slope / river bed / stream profile precious Landscape protection area
Former ESE quarry in Weißenbrunn 2018 Quarry in the corridor Kesselgrub 05.jpg
574A018 Leinburg
position
Middle Franconian Alb In the abandoned quarry in the Kesselgrub corridor there is one of the few still generally accessible outcrops of sponge limestone from the Oxford strata in the southern part of the district. Due to decay, vegetation and partial backfilling, only a seven by three meter part of the outcrop wall of an upper excavation cable is preserved. In the area of ​​the top, the formation of fragments caused by the weather can be seen. The outcrop is on a supraregional hiking trail (Frankenweg). 2500
50 × 50
Type: Rock
Type: Limestone
Quarry significant Landscape protection area
Felsenkeller S von Altdorf (Löwengrube near Prackenfels) Loewengrube 01.jpg
574G001 Altdorf near Nuremberg
position
Southwest Albrand region Originally an overgrown quarry, from which the sandstone for the university buildings in Altdorf was broken in the 16th century, the place was rediscovered by students 100 years later and prepared for happy festivities. At the beginning of the 19th century, the University of Altdorf closed and Altdorf citizens built a beer cellar and a bowling alley as a gallery. The large rock cellar offers good outcrops in the Rhaetian sandstone, especially with charred woods. 400
20 × 20
Type: Rock Cellar, Rock Type , Vegetable Fossils
Type: Sandstone
Rock cellar precious Landscape protection area
Rhätschlucht Teufelskirche SE von Weinhof Grünsberg Devil's Church 03.jpg
574G002 Altdorf near Nuremberg
position
Southwest Albrand region The Teufelskirche is a Rhätsandstein gorge with a waterfall at the beginning of the gorge. The fall originated from the contact of the coarse-grained, weather-resistant arietes sandstones with the softer Rhätolias sandstones and clay horizons. Already in the years 1525, 1600 and 1720 mining on coal and silver (in pebbles) was attempted. Urlichs (1966) reported 6 m long charred tree trunks. 35000
350 × 100
Type: Tunnels, Plant Fossils, Layer Sequence, Gorge, Minerals
Type: Sandstone, Lignite
Tunnel / gallery / shaft especially valuable Natural monument, landscape protection area, FFH area
Former Heidenloch N silver sand mining from Weißenbrunn Heidenloch 01.jpg
574G003 Leinburg
position
Southwest Albrand region In earlier centuries, the so-called silver sand (light-colored areas in the Dogger sandstone) was popular for scrubbing wooden floors and tables. The Heidenloch is the largest known mining site for this material. Access to the underground passages is blocked by a grille after the ceiling has been demolished (Fig. 4). The Heidenloch is bat winter quarters. 450
30 × 15
Type: Stud
Type: Sandstone
Tunnel / gallery / shaft precious Landscape protection area
Mine field at Moritzberg ENE von Diepersdorf Moritzberg 07.jpg
574G004 Röthenbach on the Pegnitz
position
Southwest Albrand region The Moritzberg is a witness mountain separated from the Alb. From its base to the summit, the sequence of layers from the upper Keuper to the lower Malm is open. The summit is formed by a remnant of the Franconian Alb plateau, which has been heavily ransacked by quarries (gravel, scouring lime) and excavation pits (probably floor ore). 20000
200 × 100
Type: Pinge / nfeld, Inselberg / Zeugenberg, type of layer sequence
: Limestone
Ping precious Landscape protection area
Rock apartment in Thalheim (E 80) 574G005 Happurg
position
Middle Franconian Alb About four meters above the state road, between two residential buildings, there is a no longer used rock cellar carved into the Doggerstein. The property is under protection as a monument (monument no. D-5-74-128-60). 10
5 × 2
Type: rock cellar
Type: sandstone
Rock cellar significant Monument protection
Devil's Cave SW of Altdorf Devil's Cave 03.jpg
574H001 Altdorf near Nuremberg
position
Southwest Albrand region The cave (consisting of a single large room) was artificially expanded by extracting parlor sand and a thin coal seam. The regulation of fossil woods on the cave ceiling was examined by Ulrichs (1966). 750
25 × 30
Type: eruption / weathering cave, plant fossils, sedimentary structures, tunnels, rock
type: sandstone, lignite
cave precious Landscape protection area
Distlergrotte ENE by Finstermühle Distlergrotte 05.jpg
574H003 Neuhaus an der Pegnitz
position
Northern Franconian Alb From the entrance hall, two 90 m long corridor systems lead downwards. One corridor reaches a groundwater lake, another ends at a sandstone filling. In the winter months the entrance is closed to protect bats. 450
90 × 5
Type: Karst horizontal cave, rock wall / slope
Type: Dolomite stone
cave significant Natural monument, landscape protection area, nature park
Cave system The wind hole SSW of Kauerheim Wind hole E 11 05.jpg
574H005 Alfeld
position
Middle Franconian Alb The length of the cave is approx. 2000 m, the depth approx. 52 m. In the wind hole there is a stone structure called the table. A documentation about this cave is currently being worked on. 40000
1000 × 40
Type: Karst Shaft & Horizontal Cave
Type: Limestone, Marlstone
cave precious Natural monument, landscape protection area, FFH area
Geißloch E from Krottensee Geissloch near Krottensee 02.jpg
574H010 Neuhaus an der Pegnitz
position
Northern Franconian Alb The shaft cave has a total length of 25 m and a maximum depth of 7 m. 125
25 × 5
Type: Karst shaft & horizontal cave
Type: Dolomite stone
cave significant Landscape protection area, nature park
Geißlochhöhle NNE by Münzinghof Geisloch near Münzinghof (D 16) 002.jpg
574H011 Velden
position
Northern Franconian Alb The shaft cave has a total length of 25 m and a maximum depth of 7 m. 725
145 × 5
Type: Karst horizontal cave
Type: Dolomite stone
cave significant Soil monument, landscape protection area, FFH area
Andreaskirche N of Rupprechtstegen Andreas Church 01.jpg
574H012 Velden
position
Northern Franconian Alb The spacious rock hall has three entrances. 220
11 × 20
Type: Karst horizontal cave
Type: Dolomite stone
cave significant Natural monument, landscape protection area, nature park
Large Rohenloch (D18) NE of Viehhofen Rohenloch (D 18) .jpg
574H013 Velden
position
Northern Franconian Alb In the cave you can see ceiling and wall plungers, pressure pipe and leaching forms. A Pleistocene fauna and prehistoric finds have been excavated. 335
67 × 5
Type: Karst horizontal cave
Type: Dolomite stone
cave significant Soil monument, landscape protection area, nature park
Wind hole (A5) SSE from Großmeinfeld Wind hole (A5) 02.jpg
574H015 Hartenstein
position
Northern Franconian Alb A shaft 28 m deep and 10–12 m in diameter follows the 8 m deep collapse doline. This is often visited by cave tourists. 150
15 × 10
Type: karst shaft cave, sinkhole
Type: dolomite stone
cave precious Landscape protection area, FFH area, nature park
Appenloch (Michelhöhle, Friedrichshöhle) D150 SSW from Münzinghof Michel Cave 01.jpg
574H016 Velden
position
Northern Franconian Alb The short horizontal cave in the folded limestone and dolomites of the middle Malm impresses with its imposing (15 m wide, 3 m high) entrance hall. Finds of large Pleistocene fauna were also made there. 300
20 × 15
Type: Karst horizontal cave
Type: Dolomite stone, limestone
Slope crack / rock wall significant Soil monument, landscape protection area, nature park
Kühloch (A67) NW of Hartenstein 574H017 Hartenstein
position
Northern Franconian Alb 25 m long passage cave with finds of Pleistocene fauna as well as prehistoric finds from the Neolithic and La Tène periods. 38
25 × 2
Type: Karst horizontal cave
Type: Dolomite stone
Slope crack / rock wall significant Soil monument, landscape protection area, FFH area
Sophienquelle S from Grünsberg Sophienquelle 10.jpg
574Q001 Altdorf near Nuremberg
position
Southwest Albrand region The staircase around the Sophienquelle was built in 1720. The Sophienquelle is a typical example of a shift spring. It rises on the border between Feuerletten-Rhätolias, its discharge is approx. 4 l / s. 100
10 × 10
Type: Layer Source
Type: Sandstone, Mudstone
Slope crack / rock wall precious Landscape protection area, FFH area
Sprosselbrunnen SW from Schönberg Sprosselbrunnen in summer.jpg
574Q002 Run at the Pegnitz
position
Southwest Albrand region The Sprosselbrunnen (or Spratzelbrunnen) is a spring pouring up to several liters per second, which rises from adjacent sandstone just below the layer of the Rhätolia. In the coarse-grained sandstone, numerous round tubular holes with a diameter of 5 - 30 cm have been weathered over an area of ​​about 2 × 2 m, some of which are water-flowing. 5
5 × 1
Type: layer source, layer level, rock
type: sandstone, claystone
Slope crack / rock wall precious Landscape protection area
Siebenquellental SW of Thalheim 574Q003 Happurg
position
Middle Franconian Alb In the Siebenquellental southwest of Thalheim there are numerous springs on the stratum boundary from the Malm to the underlying clayey Dogger. The source outlets are natural and scenic. There are even small natural outcrops of marl limestone from Malm Alpha. 50
10 × 5
Type: film source
type: Bricks, Kalkmergelstein
other information precious Landscape protection area
Schwarzachschlucht SW from Schwarzenbruck Schwarzach Gorge 29.jpg
574R001 Schwarzenbruck
position
Sandstone Keuper Region The Schwarzach Gorge offers the hiker typical outcrops of the Middle Burgsandstein. Scouring, erosion caves, rocky slopes and honeycomb-like weathering forms are striking. On the northern bank of the gorge, a hiking trail leads from Gsteinach over the Gustav-Adolfs-Höhle and Karlshöhle to the west. 400000
2000 × 200
Type: Tafoni / honeycomb weathering, type of rock, bank / surf cave
Type: sandstone
Impact slope / river bed / stream profile especially valuable Nature reserve, FFH area, bird sanctuary Bavaria's most beautiful geotopes No. 22
Röthenbachklamm NW of Röthenbach Rumpelbach Gorge 02.jpg
574R002 Winkelhaid
position
Southwest Albrand region The Röthenbach Gorge (also popularly known as the Rumpelbach Gorge) is a Rhätsandstein gorge that is accessible to those looking for relaxation through hiking trails and resting places. At the entrance to the gorge designated as ND stands an old, half-decayed oak with a trunk circumference of 6.30 m. 30000
300 × 100
Type: Canyon
Type: Sandstone
Impact slope / river bed / stream profile significant Natural monument, bird sanctuary
NNE gorge from Sendelbach 574R003 Ottensoo's
position
Southwest Albrand region The Rhätschlucht gorge offers outcrops in the Rhaet-Lias transition layers, which are, however, partially covered by debris deposits. 23000
460 × 50
Type: Canyon
Type: Sandstone
Impact slope / river bed / stream profile significant Landscape protection area
Wolfsschlucht NE from Wallersberg Wolfsschlucht Altdorf 09.jpg
574R004 Schwarzenbruck
position
Southwest Albrand region A waterfall in the west forms the best end to the deep, small Rhätsandstein Gorge. 12500
250 × 50
Type: Canyon
Type: Sandstone
Impact slope / river bed / stream profile significant Natural monument, landscape protection area, FFH area
Bowl stone N by Fischbach Bowl stone 07.jpg
574R005 Laufamholzer Forst
position
Sandstone Keuper Region The conspicuously weathered rock knoll made of middle castle sandstone is comparable to granite knolls weathered like wool sack. With the Celts these rocks had a cultic meaning. 100
10 × 10
Type: Ridge
Type: Sandstone
Slope crack / rock wall significant Ground monument, bird sanctuary
Castle sandstone cliffs in Rummelsberg 2015 Rummelsberg rocks 10.jpg
574R006 Schwarzenbruck
position
Southwest Albrand region The hilltop gives an insight into the composition and structure of the Upper Burgsandstone. 100
10 × 10
Type: Ridge
Type: Sandstone
Rock slope / cliff significant no protected area
Hohler Fels SE from Happurg Hollow Rock (E 2) .jpg
574R007 Happurg
position
Middle Franconian Alb Stone Age cave finds were made on the Hohlen Fels. On the cliffs above the Malm Gamma, thick limestone of the Malm Delta (with marl slab) is exposed. Above the cave there is thick-banked dolomite with chert stones. 14000
200 × 70
Type: rock wall / slope, karst horizontal cave
Type: dolomite stone, limestone
Slope crack / rock wall precious Soil monument, landscape protection area, FFH area
Riffelfelsen E by Alfalter 574R008 Forward
position
Northern Franconian Alb The reef rock, divided by several vertical fissures, is often visited by climbers. 2500
50 × 50
Type: Rock Tower / Needle
Type: Limestone
Slope crack / rock wall significant Natural monument, landscape protection area, FFH area
God's finger on Langenstein NW of Vorra God's finger on Langenstein NW from Vorra-3944.jpg
574R009 Forward
position
Northern Franconian Alb The rugged rock tower, split in the upper part, is difficult to find on a wooded hilltop. It consists of very porous dolomite. 25
5 × 5
Type: Rock tower / needle
Type: Dolomite stone
Slope crack / rock wall significant Natural monument, landscape protection area, nature park
Sounding waterfall NNE from Haimendorf Sounding waterfall 01.jpg
574R011 Röthenbach on the Pegnitz
position
Southwest Albrand region The Rhaetian transition layers are outstandingly open at the Klingenden Wasserfall. The hard sandstones form a layer on the edge of which the waterfall lies. 75
15 × 5
Type: waterfall, layer sequence, layer level
Type: sandstone, claystone
Impact slope / river bed / stream profile precious no protected area
Bastei at Zankelstein E from Pommelsbrunn Zankelstein 01.jpg
574R012 Pommelsbrunn
position
Northern Franconian Alb On the south and south-east side of the Zankelstein, three rock towers protrude from the forest, which serve as popular observation rocks. 400
20 × 20
Type: Group of rocks
Type: Dolomite stone
Slope crack / rock wall significant Natural monument, landscape protection area, FFH area
Spurzelgrub rock group NW of Hofstetten Spurzlgrou 01.jpg
574R013 Pommelsbrunn
position
Middle Franconian Alb Rock group in the massive Franconian dolomite with a spacious half cave. The partly massive, partly thick-banked dolomite traces a reef dome. 70
7 × 10
Type: rock group, karst horizontal cave
Type: dolomite stone
Slope crack / rock wall significant Natural monument, ground monument, landscape protection area
Düsselbacher Wand SE from Düsselbach Düsselbacher Wall 04.jpg
574R014 Forward
position
Northern Franconian Alb The rock face is on the left slope of the Pegnitz. 1500
50 × 30
Type: Rock Wall / Slope
Type: Limestone
Slope crack / rock wall significant Natural monument, ground monument, landscape protection area
Enzendorfer Felsen E from Enzendorf 574R018 Hartenstein
position
Northern Franconian Alb Two high rocks protrude from the wooded area. The rock faces are popular with climbers. 400
20 × 20
Type: Rock Wall / Slope
Type: Limestone
Slope crack / rock wall significant Natural monument, landscape protection area, FFH area
Jump stone (sole stone) NE of Fischbrunn 574R020 Pommelsbrunn
position
Northern Franconian Alb The reef dolomite protrudes from the Jura slope. 100
10 × 10
Type: Rock tower / needle
Type: Limestone, dolomite stone
Slope crack / rock wall significant Natural monument, landscape protection area, nature park
Huberfelsen near Alfeld Huberfelsen 01.jpg
574R021 Alfeld
position
Middle Franconian Alb The group of three rocks dominates the landscape of Alfeld. 1800
60 × 30
Type: Felsburg
Type: Dolomite stone
Slope crack / rock wall significant Natural monument
Ponor Bachloch in Großengsee 574R022 Simmelsdorf
position
Northern Franconian Alb The ponor was used to drain the village. A corridor leading down to WNW connects to the three m deep Ponor shaft. 4
2 × 2
Type: Ponor, karst horizontal cave
Type: Dolomite stone
cave significant Natural park
Felsburg Teufelskanzel WSW von Mittelburg Teufelskanzel near Mittelburg 02.jpg
574R023 Happurg
position
Middle Franconian Alb The chunky cliff has the shape of a pulpit. 150
15 × 10
Type: Felsburg
Type: Dolomite stone
Slope crack / rock wall significant Natural monument, landscape protection area, FFH area
Stream with limestone terrace W from Kainsbach Kainsbach limestone tufa terrace 03.jpg
574R024 Happurg
position
Middle Franconian Alb Small stream lined with tufa, which has formed mossy sintered terraces on a slope. 16
4 × 4
Type: sintered terraces, streams / rivers
Type: limestone, tufa
no information precious Landscape protection area
Stone channel W from Schrotsdorf Stone channel Engelthal 13.jpg
574R026 Offenhausen
position
Southwest Albrand region On the northeast slope of the Buchenberg, a small stone channel has formed below a spring, directly on a supraregional hiking trail (Frankenweg). Their formation is based on abiogenic (pressure relief, temperature increase, carbon dioxide release to the ambient air) and biogenic (algae and moss get their carbon dioxide needs from the water, not from the atmosphere) precipitation of tufa. The feeding source rises in the border area of ​​Dogger and Malm. The channel was damaged several times by vandalism. To protect them, a wooden walkway with a railing was made, and an information board explains the mechanism behind it. In addition to the original stone channel, which has fallen dry due to the damage, a new one is already being built. 30
30 × 1
Type: Stone gutter
Type: Tufa limestone
other information significant Landscape protection area
Stone channel SW from Raschbach Channel Raschbach 09.jpg
574R027 Altdorf near Nuremberg
position
Middle Franconian Alb Approx. 500 m SW of Raschbach, one of the very rare stone channels has formed at one of the numerous sources of the stream of the same name. The ornate tone separates the groundwater bodies of Dogger and Malm and represents an important source horizon. The source is popularly known as the aster or Easter fountain. The formation of the stone channel is based on two factors. Abiogenic causes of the precipitation of tufa are pressure relief, temperature increase and the release of carbon dioxide in the area close to the source. Algae and moss do not meet their carbon dioxide requirements from the ambient air, but from the calcareous water (biogenic factors). After a few tens of meters, the lime content of the water has decreased so much that the separation of tufa comes to a standstill. Obviously, the water flow was interrupted at least temporarily, so that only a small part of the water flows over the stone channel, while a new watercourse has formed to the left of it, in which the precipitation of tufa is already starting. The stone channel is a protected part of the landscape and is under special protection. 20
20 x 1
Type: Stone gutter
Type: Tufa limestone
no information significant Landscape component, landscape protection area


Sandstone rocks near the Nuremberg Imperial Castle Imperial Castle Nuremberg 5.JPG
564A002 Nuremberg
position
Sandstone Keuper Region The type locality of the widespread castle sandstone is at the Imperial Castle in Nuremberg. The castle sandstone is a fine to medium-grained sandstone. In addition to quartz grains, it contains a considerable proportion of feldspar. The building block of Nuremberg was once widely known. 51000
170 × 300
Type: Type locality
Type: Sandstone
Slope crack / rock wall precious Ground monument Bavaria's most beautiful geotopes No. 11
Nuremberg rock cellar Nuernberg Felsengaenge 001.JPG
564G001 Nuremberg
position
Sandstone Keuper Region Not specified 0
not specified
Type: rock cellar
Type: sandstone
Rock cellar precious no protected area
Historic sandstone quarries at Schmausenbuck E in Nuremberg Schmausenbuck quarry 04.jpg
564G002 Nuremberg
position
Sandstone Keuper Region There are extensive areas around the Schmausenbuck with numerous historical mining sites for castle sandstone. The sandstones were built in Nuremberg. Today they form elements that shape the landscape inside and outside the zoo. The geotope is under protection as a ground monument (monument no. D-5-6532-0558). 150,000
500 × 300
Type: Quarry / Pit
Type: Sandstone
Quarry precious Soil monument, landscape protection area, FFH area


Historic stone quarries SE von Wernsbach Quarries Wernsbach 09.jpg
576A001 Georgensgmünd
position
Sandstone Keuper Region The abandoned quarries near Wernsbach comprise the largest contiguous quarry area in the Upper Burgsandstein of the district. They provide impressive evidence of the importance of this natural stone in the construction industry. The year 1895 is engraved over a tunnel. The high break walls are visited intensively by climbers (numerous hooks!). A hiking trail leads through the area. 125000
500 × 250
Type: rock type, quarry / pit, tunnel
type: sandstone, mudstone
Quarry significant Landscape protection area Bavaria's most beautiful geotopes No. 95
Former quarry NE of Kühedorf 2016 Kühedorf quarry 06.jpg
576A002 Büchenbach
position
Sandstone Keuper Region Several historical quarries (strongly overgrown). The western part of the outcrop offers good outcrops in the Upper Burgsandstein, in which intermediate laces are occasionally turned on. 50000
250 × 200
Type: Rock
Type: Sandstone
Quarry significant Landscape protection area
Former quarry in the SW of Greding 2017 Greding Quarry 06.jpg
576A003 Greding
position
Southern Franconian Alb The outcrop provides the best insight into the Oxford strata in Roth County. 12500
250 × 50
Type: Layer sequence
Type: Limestone
Quarry significant Landscape protection area, FFH area, nature park
Rock-forming sponge banks in the Kaising Valley SSE of Kaising Kaising 04.jpg
576A004 Greding
position
Southern Franconian Alb At the upper edge of the valley there are rocks made of fossil-bearing, stratified sponge limestone of the Malm Gamma. 600
30 × 20
Type: Type of rock, rock face / slope
Type: Dolomite stone
Slope crack / rock wall significant Landscape protection area, FFH area, nature park
Former quarry W of Götzenreuth 576A005 Büchenbach
position
Sandstone Keuper Region In the historical quarries, Unterer Burgsandstein is open. 10000
200 × 50
Type: Rock
Type: Sandstone
Quarry significant Landscape protection area
Former Offenbau WNW quarry 576A006 Thalmassing
position
Southwest Albrand region The lower marl limestone of the Malm Alpha is developed in this fracture. 400
20 × 20
Type: Rock
Type: Limestone
Quarry significant Landscape protection area, nature park
Outcrop SW of Esselberg 576A007 Greding
position
Southern Franconian Alb The outcrop runs along the east side of the dry valley. The grasslands above are grazed. 14000
350 × 40
Type: Rock
Type: Limestone, Marlstone
embankment significant Landscape protection area, nature park
ESE cave system from Euerwang Euerwanger Bühl 01.jpg
576H001 Greding
position
Southern Franconian Alb During the mining of dolomite gravel, a paleo cave system was uncovered on the southern slope of the Euerwanger Bühl. 15 find horizons were located over a height difference of 30 m. A rich fauna as well as stone tools and artfully worked bones have been found during the excavations. 150
30 × 5
Type: Karst shaft & horizontal cave
Type: Dolomite stone
Slope crack / rock wall precious Landscape protection area, FFH area, nature park
Massendorfer Schlucht NNE from Spalt Massendorfer Gorge 03.jpg
576R001 Gap
position
Southwest Albrand region The narrow gorge has some good outcrops in the Upper Burgsandstein. The Deutsche Bahn had the trees in the gorge cut down to secure their electricity pylons. The geotope was also affected. 15000
300 × 50
Type: Canyon, Rock
Type: Sandstone
Impact slope / river bed / stream profile significant Landscape protection area
Gorge Schnittlinger Loch ENE from Fünfbronn Schnittlinger Loch (1) .jpg
576R002 Gap
position
Southwest Albrand region The approx. 50 m deep gorge begins in the west with a narrow gorge. It opens up the Upper Burgsandstein, and sediment structures are also clearly visible. 250
50 × 5
Type: Gorge, Gorge, Rock
Type: Sandstone
Impact slope / river bed / stream profile precious Natural monument, landscape protection area
Sinter terraces in Heinrichsgraben SE von Untermässing Sinterterrassen Untermässing 08.jpg
576R003 Greding
position
Southern Franconian Alb A lime-rich spring rises in Heinrichsgraben at the Malm lower limit, which feeds the small stream in the ditch. Due to the high lime content, tuff precipitates in small mossy cascades over a length of approx. 100 m. 15000
300 × 50
Type: sintered terraces, stratified spring
type: limestone, tufa
Impact slope / river bed / stream profile precious Landscape component, landscape protection area, FFH area
Druid stone NE from Untersteinbach Mäbenberg4.JPG
576R004 Georgensgmünd
position
Sandstone Keuper Region The large rock, weathered on all sides, lies on a wooded knoll. 10
5 × 2
Type: Ridge
Type: Sandstone
Rock slope / cliff significant Landscape protection area


Former quarry SW of Bieswang 577A001 Pappenheim
position
Southern Franconian Alb The large, abandoned quarry provides a particularly good insight into the changeable sponge reef facies of the Mörnsheim reef range. Small independent reef domes build up in the Malm Epsilon over the Dolomites of the Malm Delta. In the Malm Zeta the reefs died and were mixed with plate dolomites. 40000
200 × 200
Type: standard / reference profile, sedimentary structures
Type: dolomite stone, limestone
Quarry precious Natural park
Former quarry W of Osterdorf 577A002 Pappenheim
position
Southern Franconian Alb The large, abandoned break is still well preserved and shows a profile through the Treuchtlinger marble. Numerous karst cavities filled with reddish clay are exposed on the break walls. 20000
200 × 100
Type: sequence of layers, karst chimney, karst crevice
Type: limestone
Quarry significant Natural park
Former quarry N of Osterdorf 577A003 Pappenheim
position
Southern Franconian Alb Treuchtlinger marble is very open in the disused, fossil-rich quarry. Old fracture systems and sinter formations can be studied in the northern quarry wall. 10000
100 × 100
Type: Rock
Type: Limestone
Quarry significant Landscape protection area, nature park
Former quarry SE from Weißenburg Former quarry in the Weißenburger Stadtwald.jpg
577A004 Weißenburg in Bavaria
position
Southern Franconian Alb Good exposure of Treuchtlingen marble. It is planned to connect this former quarry with the active quarry in the north. 20000
100 × 200
Type: Rock
Type: Limestone
Quarry significant Landscape protection area, nature park
Former quarry S von Rothenstein 577A005 Weißenburg in Bavaria
position
Southern Franconian Alb The disused quarry opens up the Treuchtlinger marble (from bank 25 to around bank 9). Clay-filled karst chutes and horizontal leaching horizons are impressively cut into the quarry walls. 5000
100 × 50
Type: Rock type, karst chimney, karst crevice
Type: Limestone
Quarry precious Natural park
Abandoned quarry E von Ursheim 577A007 Polesingen
position
Riesalb The abandoned quarry opens up well-banked and fossil-rich Lower Malm. Above the Malm Gamma there is a polished surface and colorful breccia of the giant event. In the lower eastern part of the break, short horizontal shifts can be observed in the autochthonous Malm limestone. 20000
200 × 100
Type: Polished surface (impact), animal fossils, layer sequence
Type: Limestone
Quarry especially valuable Landscape protection area, nature park
Former quarry SE of Langenaltheimer Haardt 08060046 - Langenaltheim - Quarry - 2004.jpg
577A008 Langenaltheim
position
Riesalb This is the only disused quarry in which Solnhofen limestone is still well exposed. Most active quarries are backfilled with excavated material during or after their exploitation. The fracture is considered to be the type locality of the plate limestone. In 1992 another specimen of the ancient Archeopteryx was found near this break. 10000
100 × 100
Type: Type locality, Animal Fossils
Type: Limestone
Quarry precious FFH area, bird sanctuary, nature park Bavaria's most beautiful geotopes No. 71
Former suevite quarry SW of Polsingen 577A009 Polesingen
position
Nördlinger Ries The small quarry is located within the Ries crater and is developing massive suevite (4 m thick). It consists mainly of red, vesicular melt rock that includes numerous crystalline fragments (mainly granites). This suevite differs from the normal formation in the appearance of a coherent, void-rich melt rock and thus inspired the assumption of a melt layer at the crater floor, which was not confirmed, however. 200
20 × 10
Type: Type locality
Type: Suevite
Quarry especially valuable Natural park
Exposure WNW from Weimersheim 577A010 Weißenburg in Bavaria
position
Southwest Albrand region On both sides of the mountain cut, the Upper Aalen layers are exposed with thin iron ore seams. 5000
100 × 50
Type: Rock
Type: Sandstone
embankment significant Soil monument, landscape protection area, nature park
Huns Church NE of Weissenburg 577A011 Höttingen
position
Southwest Albrand region Below the Bismarck Tower, several Great Dane rocks have been thundered out of their surroundings in the forest. What is striking is the holey weathering of the sandstone layers that were once clayey. 625
25 × 25
Type: Rock type, Tafoni / honeycomb weathering, rock wall / slope
Type: Sandstone
Slope crack / rock wall significant Landscape protection area, nature park
Hill on the Hüssinger Berg 577A012 Westheim
position
Nördlinger Ries The western tip of the Hüssinger Berg marks the boundary of the outer, heavily fragmented zone of the Ries crater against the Alb in the northeast. The summit is formed by the severely broken limestone and marl of the Lower Malm. A notice board explains the special feature. 4900
70 × 70
Type: Rock type, ejecta material (impact)
Type: Limestone marl
Slope crack / rock wall significant Landscape protection area, nature park
Hollow road near Hechlingen Hohlweg Hechlingen 07.jpg
577A014 Heidenheim
position
Southwest Albrand region The ravine-like ravine offers a very good outcrop of Doggersandstein with its ore horizons. Disturbances parallel to the slope offset the sequence of shifts several times. The ravine is part of a local and natural history educational trail. 1500
150 × 10
Type: Rock
type: Sandstone, iron / manganese ore
embankment significant Landscape protection area, nature park
Iron sandstone outcrop NE of Hohentrüdingen 577A015 Heidenheim
position
Southwest Albrand region Diagonally layered Doggersandstein with iron oid layers is exposed in the former sand pit directly on the road. 150
30 × 5
Type: Rock
Type: Sandstone
Gravel pit / sand pit significant Landscape protection area, nature park
Former quarry NE of Hürth 577A017 Treuchtlingen
position
Riesalb The former quarry near Hürth opens up a profile from the middle Malm Gamma to the lower Malm Delta in stratified facies: at the bottom, 7 m of gray bench limestone are exposed, followed by about 2 m of Crussoliensis marl and 4 m of banked Uhlandi limestone. The bottom three benches of Treuchtlingen marble form the end. 300
30 × 10
Type: Layer sequence, Animal fossils
Type: Limestone, Marlstone
Quarry significant Landscape protection area, nature park
Felsenkeller in Thalmannsfeld 577A018 Bergen
position
Southwest Albrand region There are approx. 25 cellars along the street that are a few meters deep. The upper ones are filled. The sandstone is unlocked at the entrances, e.g. T. with traces of weathering. The cellars are used. 1650
110 × 15
Type: Sedimentary structures, rock cellars
Type: Sandstone
Rock cellar significant Natural park
Quarry W von Fuchsmühle 577A019 Treuchtlingen
position
Riesalb In the now disused quarry, the top two meters of the Upper Marl Limestone (Arzberg Formation, Malm Gamma) are exposed on the bottom of the entrance area. Above it is more than 30 meters of Treuchtlinger marble (Treuchtlingen formation, Malm Delta). The formation boundary is particularly easy to see here. 30000
200 × 150
Type: sequence of layers, rock
type: limestone, marlstone
Quarry precious Landscape protection area, nature park
Former Juramarmorbruch Stiegler NW of Solnhofen 577A020 Solnhofen
position
Riesalb Treuchtlinger bank lime was mined in the abandoned Stiegler quarry. 7000
100 × 70
Type: Type of rock, sequence of layers, quarry / pit
type: Limestone
Quarry precious Landscape protection area, FFH area, bird sanctuary
Hobby quarry ESE von Langenaltheim 577A021 Langenaltheim
position
Riesalb In the separately traced western part of the geotope 577A008, at the Urvogel discovery site Hobbysteinbruch Langenaltheim, fossils can be collected in thin-plate Solnhofen limestone for a small fee from April 1 to October 31. 3500
70 × 50
Type: Rock type, Layer sequence, Animal fossils, Quarry / Pit
Type: Limestone
Quarry precious FFH area, bird sanctuary, nature park
Quarry area at Schrandelberg SE from Langenaltheim 577A022 Langenaltheim
position
Riesalb The abandoned quarry on Schrandelberg opens up unusually thin-plate Solnhofen limestone. 4000
100 × 40
Type: Type of rock, sequence of layers, quarry / pit
type: Limestone
Quarry precious Landscape protection area, FFH area, bird sanctuary
Former Iron ore mine Grubschwart NE von Rothenstein Grubschwart tunnel entrance 02.jpg
577G001 Raitenbuch
position
Southern Franconian Alb Funnel pits, mine shafts and tunnels are reminiscent of the former iron ore mining. These were stored as floor ore in the clay filling of an extensive karst system. An educational trail about the history of mining with 21 stations clearly leads through the area. An audio guide can also be downloaded as an app for smartphone or tablet from www.infofeld.de/grubschwart.html. 5000
1000 × 5
Type: tunnel, karst shaft & horizontal cave, pinge field
Type: limestone, clay
Tunnel / gallery / shaft especially valuable Soil monument, landscape protection area, nature park
Karlsgraben Fossa Carolina.jpg
577G003 Treuchtlingen
position
Southwest Albrand region The Karlsgraben testifies to one of the greatest engineering achievements of the early Middle Ages. Charlemagne wanted to connect the Rhine with the Danube through a navigable canal between the Swabian Rezat and the Altmühl, as the rivers approach here at almost 1800 m. After 1,400 m had been excavated (approx. 6,000 workers and 780,000 m³ of earth), supply bottlenecks presumably led to the abandonment of the canal project. The geotope is one of Bavaria's hundred most beautiful geotopes and is explained on site with a corresponding information board. 50000
1000 × 50
Type: Trench, Canal
Type: Gravel
no information especially valuable Soil monument, landscape protection area, nature park Bavaria's most beautiful geotopes No. 34
Hell funnel NW of Osterdorf 577G005 Pappenheim
position
Southern Franconian Alb There are numerous former quarrying sites in a confined space, where floor ores were extracted from tertiary karst fillings. What remained were heaps, funnel pits and some 10 m deep exhumed karst shafts. 45000
300 × 150
Type: Pinge field, sinkhole, karst shaft cave
Type: Limestone, clay
Ping precious Soil monument, landscape protection area, nature park
Hollow hole SW from Raitenbuch Hollow hole 02.jpg
577H001 Raitenbuch
position
Southern Franconian Alb The hollow hole opens up the dolomites of the Malm Delta. With the ordinance of the LRA WUG of May 20, 1980, the hollow hole was placed under protection as a natural monument (§ 28 BNatSchG). Because of the risk of accidents and to protect the native bats (including Myotis myotis), the natural monument is fenced in and cannot be entered. 1000
100 × 10
Type: Karst shaft & horizontal cave
Type: Dolomite stone
Slope crack / rock wall precious Natural monument, FFH area, landscape protection area
Devil's Cave W by Bieswang 577H002 Pappenheim
position
Southern Franconian Alb The approx. 100 m long horizontal cave has two entrances that lead into a vestibule. 200
100 × 2
Type: Karst horizontal cave
Type: Limestone, dolomite stone
Slope crack / rock wall significant Landscape protection area, nature park
Source outlet The seven sources SW of Heidenheim Seven sources Heidenheim 05.jpg
577Q001 Heidenheim
position
Southwest Albrand region At the border between Opalimus Clay and Doggersandstein lies a spring horizon from which the seven springs arise. 100
10 × 10
Type: Layer Source
Type: Sandstone
no information significant Landscape protection area, nature park
Source outlet Steinbrunnen ESE von Göhren 577Q002 Pappenheim
position
Southern Franconian Alb Several small spring outlets arise in a spring niche set in sandstone. The stone fountain rises on the otherwise arid karst plateau on a remnant of the Upper Freshwater Molasse. The year 1706 is indistinctly visible on the stone arch of the fountain. 1
1 × 1
Type: Layer Source
Type: Sandstone
no information significant Monument protection, ground monument, landscape protection area
Gorge Teufelsbackofen NW of Fiegenstall 577R001 Höttingen
position
Southwest Albrand region The narrow gorge in the Upper Burgsandstein shows only a few outcrops. Feuerletten is waiting at the entrance. Fallen trees make inspection more difficult, especially in the central area. 18750
250 × 75
Type: Canyon, Rock
Type: Sandstone
Impact slope / river bed / stream profile significant Landscape protection area, nature park
Stone channel SW from Wolfsbronn Rinne Wolfsbronn 01.jpg
577R002 Meinheim
position
Riesalb The course of the stream lies in an approximately 130 m long and up to 160 cm high tufa dam, which is interrupted by several waterfalls. Despite the protection status, the property is to be regarded as largely destroyed, as the channel was artificially walled up with stones and concrete over its entire length as a maintenance measure. A negative example! 130
130 × 1
Type: Stone gutter, layer source
Type: Tufa-lime
no information significant Nature reserve, landscape protection area, FFH area
Stone gutter SE from Spielberg 2014 Stone gutter from Buckmühle 09.jpg
577R003 Gnotzheim
position
Riesalb The stream is approx. 20 m long and a maximum of 10 cm high. The channel is deepened and lined with a little lime. The small groove is in the development stage. 6
20 × 0
Type: Stone gutter, layer source
Type: Tufa-lime
no information significant Landscape protection area, FFH area, nature park
Stone channel S from Rohrbach Channel 05.jpg
577R004 Etten instead of
position
Southern Franconian Alb The stone channel near Rohrbach is approx. 60 m long and up to 1 m high. A wooden walkway was installed next to the gutter. The source of the channel arises between Opalinus Clay and iron sandstone, the channel grows by 2 to 3 cm annually. This channel was also partly artificially walled up. A natural development is no longer given. The red gorge with the sintered formations of the so-called Junge Steinerne Rinne also belongs to the property. 18
60 × 0
Type: Stone gutter, layer source
Type: Tufa-lime
no information significant Natural monument, landscape protection area, FFH area
Stone channel NNE from Hechlingen Stone gutter Hechlingen 03.jpg
577R005 Heidenheim
position
Southwest Albrand region The channel is approx. 10 m long and a maximum of 30 cm high; it has so far been largely preserved in its natural form. A notice board clarifies the specialty of the property. 10
10 × 1
Type: Stone gutter, layer source
Type: Tufa-lime
no information significant Landscape protection area, nature park
Stone gutter SE from Oberweiler Stone gutter Oberweiler 02.jpg
577R006 Meinheim
position
Riesalb The stream, lined with tufa, is about 50 m long. The tufa excretions have not yet been anthropogenically changed. 30
30 × 1
Type: Stone gutter, layer source
Type: Tufa-lime
no information significant Landscape protection area, nature park
Dachsbaufelsen SE from Dettenheim 577R007 Weißenburg in Bavaria
position
Southern Franconian Alb The Dachsbaufelsen was shown on the geological map as sponge reef limestone in the area of ​​Treuchtlinger marble. The rock is heavily mossed and deeply weathered in places, smaller caves lead into the rock. 100
10 × 10
Type: Dome, Rock, Fissure / Tectonic Cave
Type: Limestone
Slope crack / rock wall significant Soil monument, landscape protection area, nature park
Rock group Twelve Apostles N of Esslingen Altmuehltal3.JPG
577R008 Solnhofen
position
Southern Franconian Alb The Twelve Apostles belong to the Mörnsheimer Riffzug. The picturesque rocks are built up from the sponge algae limestone of the Middle Malm Delta. The rock group is geomorphologically classified as an ensemble, as the numerous isolated rocks represent a coherent range of reefs, which can be recognized by the garland-like coves that run from rock to rock. 60000
600 × 100
Type: rock group, rock tower / needle, rock castle, sedimentary structures
Type: dolomite stone
Slope crack / rock wall precious Nature reserve, natural monument, landscape protection area Bavaria's most beautiful geotopes No. 62
Hilltop of the Bubenheimer Berg E von Bubenheim Bubenheimer Berg.jpg
577R009 Treuchtlingen
position
Southwest Albrand region On the top of the Bubenheimer Berg, Malm limestone and dolomite clods form hard blocks of up to several cubic meters in size. These hardlings are allochthonous clods that were blasted out of the area of ​​the crater during the Ries disaster. The Malmschollen are usually intensely buried and z. Sometimes baked again, so that they weathered out of the environment as hardened people. 20000
200 × 100
Type: Ejecta (impact), rocky dome
Type: Limestone
Slope crack / rock wall precious Landscape protection area, nature park
Teufelskanzel SE from Solnhofen Teufelskanzel Solnhofen 01.jpg
577R010 Solnhofen
position
Riesalb The Teufelskanzel rock summit is built up from the bench-top Dolomites of the Malms. 20000
200 × 100
Type: Crag
Type: Dolomite stone
Slope crack / rock wall significant Landscape protection area, nature park
Ponordoline E by Göhren 577R011 Pappenheim
position
Southern Franconian Alb The Ponor trench is 200 m long, 25 m wide and has a maximum depth of 6 m in the western trench area. In the trench, a small stream flows to the mouth that was flooded with quarry rubble many years ago. 5000
200 × 25
Type: Ponor, sinkhole
Type: Breccia, dolomite stone
no information precious Landscape protection area, nature park
Dolinenfeld E von Göhren 577R012 Pappenheim
position
Southern Franconian Alb Group of several sinkholes, some of which act as ponors in heavy rain. The largest of the sinkholes has a diameter of approx. 20 m and a depth of approx. 10 m. Another very large sinkhole, in which current subsidence is taking place, is 200 m WNW of the intersection and has not yet been protected as an ND. 40000
200 × 200
Type: Dolinenfeld
Type: Dolomite stone, limestone
no information precious Landscape protection area, nature park
Quartzite blocks E from Döckingen 577R013 Polesingen
position
Riesalb Various theories exist about the age and the cause of the accumulation of quartzite blocks around Döckingen. There are 8 blocks to the east of the village. The z. Blocks of several cubic meters consist of medium-grain, quartzite cemented sandstones. Fissure structures are characteristic of the quartzites, which can possibly be traced back to the Ries event. 20000
200 × 100
Type: Type locality, relict rocks
Type: Sandstone
block especially valuable Natural park
Ponordolinen NE from Kohnhof 577R014 Polesingen
position
Riesalb In a small wood there are three large ponordolines with a temporary flow of water in a confined space. Fresh, steep subsidence in the washed-in clay is evidence of recent activity. 22500
150 × 150
Type: Ponor
Type: Limestone, Loess Loam
Sinkhole / sinkhole precious Landscape protection area, nature park
Döckingen sinkhole SSE 577R015 Polesingen
position
Riesalb The large sinkhole is in the area of ​​allochthonous rift clods. Fresh subsidence is evidence of the ongoing subsidence processes. 2000
50x40
Type: sinkhole
Type: limestone
no information precious Natural park
Hunnenstein WSW from Markt Berolzheim 577R016 Market Berolzheim
position
Riesalb These are two blocks of quartz sandstone, the assignment of which has not yet been clarified. 1
1 × 1
Type: Relic Rocks
Type: Sandstone
no information significant Landscape protection area, FFH area, nature park
Stream with sinter basin WNW Wolfsbronn Wolfbronn stream 01.jpg
577R017 Meinheim
position
Riesalb Small sinter basins have been formed along the course of the stream over a length of 100 m. 100
100 × 1
Type: Sinter formation, stream / river course
Type: Limestone, sandstone
no information significant Landscape protection area, FFH area, nature park
Stone channel NNW from Heidenheim Cheese gutter 13.jpg
577R018 Heidenheim
position
Southwest Albrand region The small but beautiful Steinerne Rinne has not yet been developed for tourism. The natural development of the channel is partially disturbed by attempts to accelerate its growth. 150
150 × 1
Type: Stone Gutter
Type: Limestone, Sandstone
no information significant Landscape protection area, FFH area, nature park
Hohler Stein NW from Stahlmühle 577R019 Heidenheim
position
Southwest Albrand region The limestone rock wall of the lower Malm lies just outside the edge of the Ries, which is noticeable in the intense fissures. Several small caves with beautifully washed-out profiles start here, but narrow quickly. 500
50 × 10
Type: Rock Castle
Type: Limestone
Slope crack / rock wall precious Landscape protection area, nature park
Dolinenfeld in the Maierholz WSW of Döckingen 577R020 Polesingen
position
Riesalb In the forest area there are numerous sinkholes in a small space, including the Ponordoline Fuchsbau. In some sinkholes there are large blocks of sandstone that resemble the Döckinger quartzites. 300000
600 × 500
Type: Dolinenfeld, Ponor, relict rocks
Type: Limestone, sandstone
Sinkhole / sinkhole significant Landscape protection area, nature park
Ponordoline SW from Rothenstein 577R023 Pappenheim
position
Southern Franconian Alb Large ponordoline with temporary tributaries from two tapering trenches. In the deepest part of the sinkhole you can also see large blocks and rock that may be standing under the clay cover. 2000
50x40
Type: Ponor
Type: Limestone
Slope crack / rock wall precious Landscape protection area, nature park

See also

Individual evidence

  1. LfU, Geotopes in Middle Franconia ( Memento of the original from September 23, 2015 in the Internet Archive ) Info: The archive link was inserted automatically and has not yet been checked. Please check the original and archive link according to the instructions and then remove this notice. (accessed on August 30, 2015) @1@ 2Template: Webachiv / IABot / www.bestellen.bayern.de

Web links

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