List of geotopes in the Bad Kissingen district
This list contains the geotopes of the Lower Franconian district of Bad Kissingen 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 Sodenberg SW von Diebach |
|
672A001 |
Hammelburg position |
Western Franconian Plates | A chimney filling was deeply dismantled on the Sodenberg. There is a columnar, secreting basalt covered with a mantle of tuffy breccia. The numerous extensive spoil heaps testify to an unfavorable (i.e. high) spoil / usable rock ratio. The extraction from the very deep pit floor is unclear, as there is no entry / exit. The mining had developed into a narrow hole with steep, no longer stable embankments. | 21600 180 × 120 |
Type: Rock, Quarry / Pit Type: Basalt |
Quarry | precious | Nature reserve, FFH area | |
Former Basalt quarry Knürzchen NE from Schildeck | 672A003 |
Schondra position |
Rhön | The small quarry is located in a basalt chimney. The small columnar secretion leads to angular to rounded blocks that are weathered in a spherical shell. A vent breccia is exposed at the edge, formerly also areas with adjacent rock breccia. | 225 15 × 15 |
Type: Rock Type: Basalt |
Quarry | precious | Landscape protection area, nature park | ||
Former Rudelberg E quarry by Schondra | 672A004 |
Schondra position |
Rhön | In the abandoned quarry, layers of the lowest lower shell limestone are pending. Typical of this section is the high proportion of marly areas as well as conglomerate benches and benches with sea lily stems. The border limestone (the border bank to the Upper Buntsandstein) can be found twice in the path below the quarry. | 800 100 × 8 |
Type: Layer sequence Type: Limestone |
Quarry | significant | Landscape protection area, FFH area, nature park | ||
Former Clay pit SE from Untereschenbach | 672A005 |
Hammelburg position |
Western Franconian Plates | The abandoned clay pit opens up the upper parts (approx. 5 m) of the lower red clay stones in the lower part of the pit wall (red-brown clay silt stones with gray-green reduction horizons) as well as excellently preserved white-gray red quartzite (at the top) 2.5-3.0 m thick with bleached layers below its base. A special geotope due to the rarity of outcrops in red quartzite. | 4000 100 × 40 |
Type: Layer sequence Type: claystone, sandstone |
Clay pit / clay pit / marl pit | precious | no protected area | ||
Former Ofenthaler Berg quarry near Hammelburg | 672A006 |
Hammelburg position |
Western Franconian Plates | The abandoned quarry is divided into a lower and an upper area. In the lower area of the myophoric layers of the uppermost red sandstone are the red intermediate and the hanging part of the myophoric layers, followed by the basal layers of the lower shell limestone. The upper area opens up the layers to below the terebratel benches in a dismantling wall. The oolite bank is visible in the upper third. | 36000 300 × 120 |
Type: Standard / Reference Profile, Disturbance Type: Limestone, Claystone |
Quarry | precious | Landscape protection area, nature park | ||
Former Quarry SE from Stralsbach | 672A007 |
Burkardroth position |
Rhön | In two quarries near Stralsbach, there is a lot of sloping lower Muschelkalk in great thickness in a trench-like fault system. Here it is lowered to the level of the upper red sandstone. Due to its higher resistance to weathering, the red sandstone forms a morphological high area (relief reversal). | 120 20 × 6 |
Type: Fault, Rock Type: Limestone |
Quarry | precious | Landscape protection area, nature park | ||
Former Quarry Kehlmetze E von Nüdlingen | 672A008 |
Nüdlingen position |
Northern Franconian Plates | In the former small quarry, Wellenkalk is exposed to the Beta 2 oolite bank. The bench is oolithic-fine conglomerate with a characteristic wavy surface. Best exposure from this bank in the whole region and easily accessible. | 8000 200 × 40 |
Type: Layer sequence, Animal fossils, Rock type: Limestone |
Quarry | precious | no protected area | ||
Former Quarry Höret SE von Arnshausen | 672A009 |
Bad Kissingen position |
Western Franconian Plates | Folded corrugated limestone from the foam limestone region is exposed in the Höret quarry. In the west, the folded layers change into undeformed limestone. In the east, the folds are limited by a fault that shifts the Lower Muschelkalk to the Upper Muschelkalk with a jump height of approx. 100-130 m. In the meantime, only a very small wrinkled area can be seen at the Bruch entrance. The exposed sloping layer surfaces are still impressive. | 3600 60 × 60 |
Type: fold / trough / saddle, fault, rock type: limestone |
Quarry | significant | Landscape protection area | ||
Former Quarry at the Platzer Kuppe NE of Geroda | 672A011 |
Geroda position |
Rhön | In a small quarry on the northwest side of the Platzer Kuppe, Unterer Muschelkalk (wave limestone) was mined, namely Unterer Muschelkalk 1 with a conglomerate bank and (above) a prominent oolite bank. The profile connects stratigraphically to the Schondra profile at the top. | 900 30 × 30 |
Type: Rock Type: Limestone |
Quarry | significant | Nature reserve, landscape protection area, FFH area | ||
Former Bellevue SE basalt quarry from Wildflecken |
|
672A012 |
Wildspot position |
Rhön | The abandoned quarry shows beautifully formed basalt columns on various levels. | 54000 180 × 300 |
Type: Rock type, Basalt columns Type: Basalt |
Quarry | significant | Landscape protection area, FFH area, bird sanctuary | |
Former Basalt quarries at Hegkopf S from Schönderling | 672A013 |
Geiersnest-East position |
Rhön | The former main quarry on basalt is completely overgrown and can be addressed as a biotope through the formation of a lake. A small shallow pit southwest of the former main quarry shows overburden and overgrowth as well as basalt with numerous weathered olivine tubers. | 3600 60 × 60 |
Type: Rock Type: Basalt |
Quarry | significant | Natural park | ||
Basaltsee am Farnsberg (inkwell) ESE von Riedenberg |
|
672A014 |
Riedenberg position |
Rhön | A lake has formed in a crater-shaped former basalt quarry. There are still old factories on the western edge of the lake. A house for friends of nature makes the geologically and ecologically interesting quarry accessible for leisure purposes. The quarry shows basalts in predominantly columnar formation. Location of the former Spitzer Steinküppel quarry. | 40000 200 × 200 |
Type: basalt columns, quarry / pit, rock type: basalt |
Quarry | precious | Nature reserve | |
Volcanic crater on the ESE mountain rock in Oberbach |
|
672A017 |
Wildspot position |
Rhön | Abandoned basalt quarry, on the walls of which the contact between black basalt columns and red slag is repeatedly opened up. This interface dips towards the center of the fracture. Obviously lava has filled a depression in the slag here. The basalt columns that were mined here may have been created as a filling of a lava lake within the crater of a small cinder cone. | 16000 200 × 80 |
Type: Contact, Igneous Structure, Basalt Columns, Type of Rock Type: Basalt, Tuff / Tuffite |
Quarry | especially valuable | Nature reserve, landscape protection area, FFH area | Bavaria's most beautiful geotopes No. 84 |
Chirotherien sandstone NE from Euerdorf | 672A018 |
Your village position |
Rhön | At the Saalrangen northeast of Euerdorf, tread seals of dinosaur precursors were uncovered, which can be assigned to the Thuringian chirotheria sandstone. The way through the time from Bad Kissingen to the Terra Triassica Museum in Euerdorf leads past the geotope. | 400 20 × 20 |
Type: trace fossils, sequence of layers, rock type: sandstone |
other information | especially valuable | Landscape protection area, nature park | Bavaria's most beautiful geotopes No. 98 | |
Aufgel. Shell limestone quarry NE from Rannungen | 672A020 |
Rannungen position |
Northern Franconian Plates | The easily accessible abandoned quarry opens up Lower Muschelkalk (mostly wavy limestone), which occasionally contains fossils, both traces of bioturbation and fauna. | 500 50 × 10 |
Type: Type of rock, sequence of layers, trace fossils, animal fossils Type: Sandstone |
Quarry | significant | no protected area | ||
Aufgel. Muschelkalkbruch SE from Ramsthal |
|
672A021 |
Ramsthal position |
Western Franconian Plates | In the abandoned quarry, shell pavement and a lime bank with a stromatolithic character are exposed. There are opportunities to find fossils. | 600 30 × 20 |
Type: Type of rock, sequence of layers, trace fossils, animal fossils Type: Limestone |
Quarry | precious | Landscape component | |
Aufgel. Arnshausen quarry NE | 672A022 |
Bad Kissingen position |
Rhön | Rock sandstone was extracted from the abandoned quarry. Above the rock sandstone, layers of carnelian dolomite and Thuringian chirotheria sandstone are exposed. The violet-brown color in the upper section of the carnelian-dolomite layers is interpreted as soil formation (violet horizon). Occasionally clay siltstone layers are interposed. | 0 not specified |
Type: layer sequence, fossil soil, rock type: sandstone |
Quarry | especially valuable | Natural park | ||
Aufgel. Limestone quarry Kalkofen W von Poppenlauer | 672A024 |
Maßbach position |
Northern Franconian Plates | In the extensive quarry area, Lower Muschelkalk is exposed, which occasionally shows ripples. | 21000 300 × 70 |
Type: Type of rock, sequence of layers, sedimentary structures Type: Limestone |
Quarry | significant | Nature reserve, FFH area | ||
Aufgel. Limestone quarry S of Münnerstadt | 672A025 |
Münnerstadt position |
Northern Franconian Plates | The partially overgrown break opens up Lower Muschelkalk (wave limestone series, mu2) and is difficult to access. | 1200 60 × 20 |
Type: sequence of layers, type of rock, sedimentary structures Type: limestone |
Quarry | significant | Nature reserve | ||
Aufgel. Limestone quarry in the former StOÜbPl E von Reiterswiesen | 672A026 |
Bad Kissingen position |
Northern Franconian Plates | The relatively well preserved, easily accessible and little overgrown quarry opens up Lower Muschelkalk (Terebratel and foam limestone banks). | 3200 80 × 40 |
Type: quarry / pit, rock type, layer sequence type: limestone |
Quarry | precious | Nature reserve, FFH area | ||
Aufgel. ESE limestone quarry in Reiterswiesen | 672A027 |
Bad Kissingen position |
Northern Franconian Plates | The small quarry, located right next to a forest path in the nature reserve, opens up Lower Muschelkalk (mu2 - mu3). | 400 40 × 10 |
Type: quarry / pit, rock type, layer sequence type: limestone |
Quarry | precious | Nature reserve, FFH area | ||
Former Barite mine, Grube Marie SW in Wildflecken | 672G001 |
Wildspot position |
Rhön | In a total of 3 old tunnels, one of which was blasted (two are still accessible but secured by grids), barite was mostly mined before the war. Stratigraphically, the barite deposits are located in the Middle Buntsandstein, their formation is probably of a hydrothermal type. A viewing gallery can be viewed by appointment (information in the House of the Black Mountains in Oberbach). | 100 50 × 2 |
Type: Tunnels, Minerals Type: Vein mineralization , sandstone |
Tunnel / gallery / shaft | precious | Landscape protection area, nature park | ||
Kothener Sauerbrunnen NE by Kothen | 672Q001 |
Moth position |
Rhön | The Kothener Sauerbrunnen is freely accessible. It is framed and covered with a brick pavilion. | 1 1 × 1 |
Type: Mineral Spring Type: Sandstone, Basanite |
no information | especially valuable | Landscape protection area, nature park | ||
Volcanic cone Mettermich NNW from Schondra |
|
672R001 |
Schondra position |
Rhön | Above a relatively small central cone, the two closely adjacent peaks of the volcanic cone rise approx. 5 m above the surrounding area with the columnar basalt. There is a wide sea of blocks around it. At the top of the protected part of the landscape there is a ring wall from early human history, as well as a wide driveway and other peculiarly arranged basalt walls. | 40000 200 × 200 |
Type: volcanic vent Type: basalt |
no information | precious | Landscape protection area, nature park | |
Dreistelz WNW volcanic cone from Oberleichtersbach |
|
672R002 |
Dreistelzer forest position |
Rhön | The Dreistelz is the highest volcanic cone in the region. The steep central area is oriented EW like a walkway. It has small rock formations at the top (right next to the observation tower) and a small basalt quarry at the western end of the steep area. Remnants of Lower Muschelkalk are present around the edge of the cone. On the east side of the cone, enormous areas of basalt rubble have started to slide down to the Dreistelz-Modlos road. | 160000 400 × 400 |
Type: volcanic vent Type: basalt |
Rock slope / cliff | precious | Landscape protection area, nature park | |
Basalt quarry on the stump of lime tree N of Schondra |
|
672R003 |
Schondra position |
Rhön | The quarry was created solely for the purpose of supplying the A7 motorway construction. A whole basalt cone was artificially removed except for a kind of crater wall. The different types of basalt secretion are interesting, especially the fan-shaped basalt columns (piles) at the quarry entrance. As the occurrence of a clod of pyroclastic rocks shows, the columnar basalts arose from a former lava lake. | 70,000 350 × 200 |
Type: basalt columns, volcanic vent, rock type: basalt |
Quarry | precious | Landscape component, landscape protection area, FFH area | Bavaria's most beautiful geotopes No. 7 |
Pilster stone NE from Kothen |
|
672R004 |
Moth position |
Rhön | To the north-east of Kothen is the scenic Pilsterstein, a morphologically carved out from weathering, running east-west, like volcanic vent. The rock here does not show the typical formation of mostly six-sided basalt columns typical of basaltic rocks, but rather it exudes more irregularly and sometimes rather in platy layers. Since a platy segregation is typical for the likewise volcanic rock phonolite, it was at times assumed that the pilster stone would consist of this rock, which is widespread in the Hessian Rhön. In fact, it is a basalt-like basanite. | 3600 60 × 60 |
Type: rocky dome, volcanic vent, basalt columns Type: basanite |
Rock slope / cliff | especially valuable | Landscape protection area, nature park | |
Falkenwand WSW from Elfershausen | 672R005 |
Elfershausen position |
Western Franconian Plates | The Höhenweg (circular route 5 of the Rhön Nature Park) runs below the wave limestone-Saaleprallhangs always in red tone on the rubble (border yellow limestone) of the Lower Muschelkalk. Thanks to the landscape management of the Bad Kissingen care association and the Bad Kissingen section of the DAV, the Falkenwand is easily accessible and visible again. There is constant traffic noise from the nearby motorway. | 360000 1200 × 300 |
Type: Impact slope, type of layers : dolomite stone, limestone |
no information | precious | Landscape protection area, FFH area, nature park | ||
Long stones NW of Riedenberg |
|
672R007 |
Römershager Forst-Nord position |
Rhön | Blocks of the rock sandstone of the uppermost Middle Buntsandstein, which forms a step in the terrain about 20 m higher, have gravitationally slid down the slope. The largest block of the medium to coarse-grained to fine gravel rock sandstone is 15 m long (without transverse fissures) and up to 2 m thick and its longitudinal axis is adjusted in the direction of the slope. About 100 m above is the rock group Steinhaufen | 400 40 × 10 |
Type: landslide, rock type: sandstone |
other information | precious | Landscape protection area, FFH area, bird sanctuary | |
Rock group The large stones NW of Riedenberg |
|
672R008 |
Great Auersberg position |
Rhön | The large stones consist of white, medium to coarse-grained to fine gravel rock sandstone from the uppermost middle colored sandstone. The striking inclined stratification was removed by the weathering. The rocky sandstone at the upper edge of the valley forms a mighty block flow down the slope that extends down to the bottom of the valley. In the gorge, sections of the deeper Middle Buntsandstein are exposed. | 7500 50 × 150 |
Type: rock group, rock type: sandstone |
Slope crack / rock wall | precious | Landscape protection area, FFH area, bird sanctuary | |
Steinernes Meer at Berghaus Rhön SE von Riedenberg | 672R009 |
Riedenberg position |
Rhön | The basalt block field consists partly of blocks without intermediate substance (sea of blocks), partly of blocks that float in a loamy base. The consistently sharp-edged blocks indicate short hiking trails (i.e. the place of origin of the blocks very close). The restless surface morphology speaks for sliding masses. The block field is located directly above the Berghaus Rhön car park. | 10000 100 × 100 |
Type: Sea of Boulders, Basalt Columns, Type of Rock Type: Basalt |
Quarry | precious | Natural park | ||
Vulkanschlot Lösershag SE from Oberbach | 672R010 |
Wildspot position |
Rhön | The summit structure of the Lösershag consists of a steep summit (volcanic vent made of adjacent basalt columns). Several impressive block seas at the foot of the slope, very scenic. Remote, but easy to reach via hiking trails. Small, abandoned quarry on the north-western slope of the mountain with radial basalt columns. | 160000 400 × 400 |
Type: volcanic chimney, basalt columns, sea boulders, rock type: basalt |
Rock slope / cliff | precious | Nature reserve, landscape protection area, FFH area | ||
Buntsandsteinschlucht Dörflinger Ruh SSW from Bad Brückenau | 672R012 |
Bad Brückenau position |
Rhön | The upcoming occurrence of large clods (blocks and slabs) of rock sandstone in the gorge is due to a tectonic subsidence within an approximately north-south-facing ditch. | 10000 200 × 50 |
Type: Canyon, Rock Type: Sandstone |
Impact slope / river bed / stream profile | significant | Landscape protection area, nature park | ||
Sinkhole SW of Maßbach | 672R013 |
Maßbach position |
Northern Franconian Plates | The circular hole is about 10 m deep and overgrown with old trees. Presumably this collapse doline results from leaching in the underlying Lower Muschelkalk. | 225 15 × 15 |
Type: sinkhole Type: Limestone |
no information | precious | Landscape component | ||
Wichtelhöhlen SW of Bad Kissingen | 672R014 |
Your village position |
Rhön | On the Alte Euerdorfer Straße, in the area of the Saale-Prallhangs Batzenleite, there is a larger outcrop in the rock sandstone. Individual blocks up to 10 m in size that have been detached from the association also occur. Pronounced gaps and cavities between the blocks represent the legendary Wichtelhöhlen. The way through the time from Bad Kissingen to the Museum Terra Triassica in Euerdorf leads past the geotope. | 15000 300 × 50 |
Type: rock wall / slope, boulder sea, tafoni / honeycomb weathering, sedimentary structures, type of rock type: sandstone |
Slope crack / rock wall | precious | Landscape component, landscape protection area, nature park | ||
Neuwiesgraben-Schlucht S from Dittlofsroda | 672R015 |
Wartmannsroth position |
Rhön | The Neuwiesgraben has partly deepened like a gorge into the red sandstone of the Röt succession and occasionally forms small waterfalls. | 5000 500 × 10 |
Type: Canyon, Waterfall Type: Sandstone |
Impact slope / river bed / stream profile | precious | Landscape protection area, nature park | ||
Rock clearance Wildweibstein N von Völkersleier | 672R016 |
Forst Detter-Süd position |
Rhön | On the Wildweibstein there are extensive rock exposures and rock seas in the rock sandstone of the Hardegsen range. | 0 not specified |
Type: Felsburg, Blockmeer Type: Sandstone |
Rock slope / cliff | precious | Landscape protection area, nature park | ||
A crack of the Schindeller fountain ENE from Kleinbrach | 672R017 |
Bad Kissingen position |
Rhön | The Schindeller Graben, which slopes steeply west to the Franconian Saale, has dug itself deep into the intensely red-brown sandstone of the Hardegsen range, which forms striking banks (thicknesses in the dm area). Several waterfalls up to two meters high were created. The water flow varies greatly depending on the weather. | 1500 100 × 15 |
Type: Storage conditions, rock type, sequence of layers, waterfall Type: sandstone |
Slope crack / rock wall | precious | Landscape protection area, nature park |
See also
- List of nature reserves in the Bad Kissingen district
- List of landscape protection areas in the Bad Kissingen district
- List of FFH areas in the Bad Kissingen district
Individual evidence
- ↑ Data source: Bavarian State Office for the Environment, www.lfu.bayern.de, Geotoprecherche (accessed on September 16, 2017)
Web links
Commons : Geotopes in the Bad Kissingen district - collection of images, videos and audio files