List of geotopes in the Rhön-Grabfeld district
This list contains the geotopes of the Lower Franconian district of Rhön-Grabfeld 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 Altenfeld NW of Urspringen | 673A001 |
Ostheim before the Rhön position |
Rhön | In the former, extensive mining area, the exposure conditions are very poor due to the strong overgrowning. However, the quarry serves as an example of natural succession of uncultivated quarries. | 120000 400 × 300 |
Type: Rock Type: Basalt |
Quarry | significant | Landscape protection area, FFH area, bird sanctuary | ||
Former Basaltsee quarry northwest of Oberelsbach |
|
673A003 |
Oberelsbach position |
Rhön | This exposure shows typical, columnar basalt of the Rhön. Due to the already existing protection status (NSG Rhön), dry and wet biotopes formed in the Bruch. The source outlets in the outcrop feed the basalt lake. Formerly up to 12 m high pillars were opened here, which were dismantled in the 1930s and sent to Holland for dam construction. Only the top ends of the basalt columns are visible. Developed with parking lot, kiosk, barbecue area. | 450 30 × 15 |
Type: basalt columns, rock type, layer source type: basalt |
Quarry | significant | Natural monument, nature reserve, landscape protection area | |
Basaltsee (Silbersee) S of Roth |
|
673A004 |
Hausen position |
Rhön | In the central part of the former basalt quarry, fan-shaped or pile-shaped columnar basalt was mined. The massive olivine basalts show columnar formation on the SW wall. At the deepest point of the bottom a lake formed, which is partly surrounded by a picturesque tree population (picnic area and hiking trails open up the place). Beautiful, palisade-like basalt columns along the south and south-west bank. | 14000 100 × 140 |
Type: basalt columns, rock wall / slope, rock type: basalt |
Quarry | precious | Landscape protection area, FFH area, bird sanctuary | |
Former Basalt quarry NNE from Sennhütte | 673A005 |
Fladungen position |
Rhön | In the former basalt quarrying, columnar basalt is partially exposed on the steep walls. | 21600 120 × 180 |
Type: Rock type, Basalt columns Type: Basalt |
Quarry | significant | Landscape protection area, FFH area, bird sanctuary | ||
Former Basalt quarry E from Sennhütte | 673A006 |
Fladungen position |
Rhön | The entire quarry complex (approx. 3 larger extraction areas) opens up tuff, basanite and columnar basalt. Basalt flows store e.g. T. on pyroclastites. In this break there is interesting geology paired with valuable wet and dry biotopes. The entire complex is overgrown and difficult to walk, the two lakes are fishing waters. | 120000 300 × 400 |
Type: Basalt columns, sequence of layers, type of rock Type: Basalt, tuff / tuffite |
Quarry | significant | Bird sanctuary, nature park | ||
Former Basalt quarry WSW from Roth | 673A007 |
Hausen position |
Rhön | The former quarry is right on the edge of the NSG Lange Rhön. He develops olivine basalts in massive training. | 20000 100 × 200 |
Type: Rock Type: Basalt |
Quarry | significant | Landscape protection area, FFH area, bird sanctuary | ||
Former Basalt quarry N of Bischofsheim (am Holzberg) | 673A008 |
Bischofsheim in the Rhön position |
Rhön | The extensive basalt quarry complex has two main excavation levels. Above the upper level there are basalt columns showing effusive lava ceilings (similar to those in the neighboring Bauersberg quarry). T. bulky waste, partly in the groundwater area, deposited. | 120000 300 × 400 |
Type: Rock type, Basalt columns Type: Basalt |
Quarry | significant | Landscape protection area, nature park | ||
Former Shell limestone quarry northwest of Hollstadt | 673A009 |
Hollstadt position |
Northern Franconian Plates | The former quarry opens up a section of the Lower Muschelkalk with the Beta 2 oolite bank under the upper edge. The main wall, which is formed by a single large fissure area, shows a karst chute and primary sedimentary structures (sedimentary landslides, inclined stratification, bioturbation) that have been excellently prepared by weathering. Buildings have been heavily overbuilt since the initial survey. | 1000 50 × 20 |
Type: sedimentary structures, rock type, karst chimney, karst crevice Type: limestone |
Quarry | precious | no protected area | ||
Clay pit ENE from Kleinbardorf | 673A010 |
Bad Königshofen in the Grabfeld position |
Hassberge region | The uppermost section of the myophoria layers is exposed, consisting of alternating blue-green and red-brown clay silt stones with hard dolomitic marl banks (stone marls) inserted into them. The open fracture tectonics is a typical (Germanotype or Saxon) alternative tectonics. The outcrop is the type locality of the Grabfeld formation. | 1600 80 × 20 |
Type: Type locality, disturbance, sequence of layers Type: Clay marl |
Clay pit / clay pit / marl pit | especially valuable | Landscape protection area, nature park | ||
Outcrop at the Judenhügel NE of Sulzfeld | 673A011 |
Sulzfeld position |
Hassberge region | In a ravine on the hill, clay-marly layers of the Middle to Upper Burgsandstein (basin facies) are well exposed in a slightly (20 °) inclined position. They are marked by stone marl banks with gray-greenish and red-brown clay silt stones in between. The gray-greenish (chemically-reduced?) Clay siltstone inclusions directly below the stone marl banks are typical. | 800 80 × 10 |
Type: Layer sequence, type of rock Type: Clay marl |
embankment | precious | Landscape protection area, nature park | ||
Basalt prism wall on the Gangolfsberg WNW of Urspringen |
|
673A016 |
Oberelsbach position |
Rhön | Basalt columns (approx. 30–40 cm in diameter) lying on top of each other like a stack of wood. Spectacularly open-minded and visible. Information board on the wall base. Medium-sized sea of blocks to the right of the prism wall. Very rare type of digestion. Approx. 50 m west to the right of the path there is a small outcrop with contact between basalt / tuff and slag. Possibly. Remnant of a cinder cone? | 150 30 × 5 |
Type: basalt columns, contact, rock type: basalt, tuff / tuffite |
Slope crack / rock wall | precious | Nature reserve, landscape protection area, FFH area | |
Brend gate NW of Schönau | 673A017 |
Schönau at the Brend Position |
Rhön | The 10 m high outcrop on the steep bank of the Brend shows part of the Volpriehausen alternation. It represents the only major outcrop in this sequence in the entire region. | 0 not specified |
Type: sequence of layers, sediment structures Type: sandstone, claystone, siltstone |
Impact slope / river bed / stream profile | precious | Landscape protection area, FFH area, nature park | ||
Gypsum marl outcrop at Altenburg SE von Trappstadt | 673A019 |
Trappstadt position |
Hassberge region | Below the Altenburg plateau, which is formed from layers of Coburg sandstone, the Heldburg marl is exposed. A plaster lens used to be removed here. Today only a small outcrop is left overgrown with rare plants typical of the site. | 120 30 × 4 |
Type: Type of rock, sedimentary structures Type: gypsum, marlstone |
Open pit | significant | Nature reserve, landscape protection area, FFH area | ||
Aufgel. Rhätsandsteinbruch SE by Johanneshof | 673A020 |
Sulzfeld position |
Hassberge region | The abandoned quarry at the holiday complex is located in the lower part of the Rhät. What is particularly striking in the quarry is a dense array of crevices and faults that literally break the sandstone layers into dominoes. Some of the sandstone banks are tilted and placed at an angle. The brackish water mussel Haßbergia haßbergensis can be found in the uppermost parts of the sandstone. Information board No. 15 of the Haßberge route. | 250 25 × 10 |
Type: Fault, Animal Fossils, Rock Type: Sandstone |
Quarry | precious | Landscape reserve, bird sanctuary, nature park | ||
Abandoned clay pit S from Großbardorf | 673A021 |
Großbardorf position |
Hassberge region | The layers of the grave field formation with their alternating blue-green and red-brown clay silt stones are exposed. Hard dolomitic stone marl benches are inserted in it. The prominent bench in the uppermost area is the so-called beta bench. | 1200 120 × 10 |
Type: sequence of layers, sediment structures Type: clay, marlstone |
Clay pit / clay pit / marl pit | precious | no protected area | ||
Abandoned reed sand quarry NNW of Eyershausen | 673A022 |
Bad Königshofen in the Grabfeld position |
Hassberge region | The dismantling walls document a mighty and homogeneous sandstone, which is traversed by sloping fissures. The parting line that divides the sandstone is only slightly formed. The quarry is located in the center of a former river channel. At the lower entrance to the break, the transition to the Middle Estherian layers is open. The upper part was cleared out by the river system. | 8100 90 × 90 |
Type: Rock Type: Sandstone |
Quarry | precious | Landscape protection area, FFH area, bird sanctuary | ||
Gypsum hill SE from Alsleben | 673A023 |
Trappstadt position |
Hassberge region | In the nature reserve southeast of Alsleben, a pronounced subrosion landscape has been preserved over an area of around 200 200 meters. Numerous unevenness are the remains of the leaching of gypsum (gypsum karst) from the gypsum keuper. In the wider area, due to intensive agriculture, no evidence of subrosion can be seen. Occasionally, however, smaller pieces of plaster of paris can be found on the arable land. | 40000 200 × 200 |
Type: subrosion landscape, sinkhole, sinkhole, layer level Type: plaster |
Slope crack / rock wall | precious | Nature reserve, landscape protection area, nature park | ||
Former Basalt quarry on the northern slope of the Kreuzberg | 673A024 |
Bischofsheim in the Rhön position |
Rhön | The small basalt quarry located on the slope shows extremely regular basalt columns, as if drawn with a ruler. The quarry is growing rapidly. | 400 20 × 20 |
Type: Rock type, Basalt columns Type: Basalt |
Quarry | significant | Landscape protection area, FFH area, bird sanctuary | ||
Former basalt quarry Steinernes Haus 2 | 673A025 |
Oberelsbach position |
Rhön | Former dismantling of basalt columns, which stand in the partially overgrown up to 8 meter high exposed walls in horizontal to vertical position. In the late summer of 2010, parts of the outcrop were deforested. Unusual is the occurrence of the swamp heart leaf (Parnassia palustris), an indicator for damp locations, which prefers chalky-marly locations. This may indicate backfilling with foreign material. | 17500 175 × 100 |
Type: Rock type, Basalt columns Type: Basalt |
Quarry | significant | Nature reserve, landscape protection area, FFH area | ||
Sand pit S by Wollbach | 673A026 |
Wollbach position |
Rhön | The sand pit is owned by the municipality and opens up an approx. 4 m thick sand deposit. After consulting the municipal administration, private individuals may remove sand for non-commercial purposes. The cross-layered sand contains irregular, thin layers of light gray plastic clay. On the northern excavation face there are brood tubes from hymenoptera (presumably solitary bees). In the eastern area there is a seldom drying out accumulation of surface water. Approx. 500 m northwest There is another sand pit. This is operated sporadically. It is fenced in and entry is prohibited. In the clay lenses there, relics of leaves, fruits and seeds were found, which allow a stratigraphic assignment to the Pliocene. The organic matter was dissolved by circulating water, so that only prints remained. It is assumed that these are deposits of a primeval Saale with a river-side forest. Thus one of the oldest known river systems in Northern Bavaria is documented here. | 2700 90 × 30 |
Type: Vegetable Fossils, Open Pit Type: Sand, Clay |
Gravel pit / sand pit | especially valuable | no protected area | ||
Frickenhäuser See ESE from Frickenhausen |
|
673R001 |
Mellrichstadt position |
Northern Franconian Plates | The almost circular, inflow and outflow-free Frickenhäuser Lake, the only naturally formed lake in northern Lower Franconia, lies on a fault that separates a slab of Lower Muschelkalk in the NE from the Upper Buntsandstein in the SW, about 20 degrees to the SW. Since half of the lake lies in the area of the lower shell limestone, which was previously there, it must have been dissolved. It remains to be seen whether the fundamental cause is leaching of Zechstein salt. | 22500 150 × 150 |
Type: sinkhole, rock type: limestone |
Slope crack / rock wall | especially valuable | Natural monument, landscape protection area | Bavaria's most beautiful geotopes No. 12 |
Basalt block sea Johannisfeuer on Kreuzberg |
|
673R002 |
Bischofsheim in the Rhön position |
Rhön | Immediately to the east of the transmitter mast lies a wide sea of boulders made of massive basalt. The Kreuzberg is the most popular excursion mountain in the Bavarian Rhön (monastery). As a result, the block sea is also better known than the block sea on neighboring mountains. The block flow on the eastern slope feeds on the basalt on the edge of the plateau / valley slope. | 8000 200 × 40 |
Type: Block Sea, Rock Type: Basalt |
other information | precious | Landscape protection area, FFH area, bird sanctuary | |
Teufelskeller on Gangolfsberg NW of Oberelsbach |
|
673R003 |
Oberelsbach position |
Rhön | Rock wall with cut of two basalt ceilings over a discordance: in the hanging wall a more or less horizontally layered ceiling, underneath a ceiling consisting of steep basalt columns that are bent over directly under the discordance. The Teufelskeller is a 5 3 1.5 m large natural cave under a huge fall block at the foot of the steep wall, where numerous small blocks lie around. The earlier interpretation of the formation as a gas bubble in the magma cannot be confirmed. | 4000 100 × 40 |
Type: volcanic vent, basalt columns, boulder, contact, rock type: basalt |
Slope crack / rock wall | precious | Nature reserve, landscape protection area, FFH area | |
Basalt block rubble at the Eisgraben WSW von Hausen | 673R004 |
Hausen position |
Rhön | The deposit is located on the slope of the Eisgraben behind a house (Eisgraben hut) and turns into a slide down the valley. | 6000 60 × 100 |
Type: Blockmeer Type: Basalt |
Slope crack / rock wall | precious | Nature reserve, natural monument, landscape protection area | ||
Shell limestone strata NW of Ostheim | 673R005 |
Ostheim before the Rhön position |
Northern Franconian Plates | The Weyershauk nature reserve is located on a slab of Lower Muschelkalk (wave limestone) that dips to the east at about 20 °. The path leading to the top rises especially in its upper half (up to the summit cross) with the streaking on the edge of the terrain and z. Partly well exposed limestone layers (especially with a conglomerate bank). | 240000 300 × 800 |
Type: Layer Type: Limestone |
Slope crack / rock wall | precious | Nature reserve, landscape protection area, FFH area | ||
Sinkhole NNW of Großbardorf | 673R006 |
Großbardorf position |
Northern Franconian Plates | The circular, approx. 10 m deep and funnel-shaped widened hole was created in 1989 by leaching in the Upper Muschelkalk, approx. 350 m west of the Untertanningsmühle in the forest. | 4 2 × 2 |
Type: sinkhole, karst shaft cave Type: clay marl stone, gypsum |
other information | precious | no protected area | ||
Teufelsmühle SSE by Holzberg |
|
673R007 |
Bischofsheim in the Rhön position |
Rhön | Surrounded by canyon forest lies a legendary 3 m deep fall. | 60 20 × 3 |
Type: Waterfall Type: Basalt |
Impact slope / river bed / stream profile | significant | Natural monument, landscape protection area, FFH area | |
Schwarzes Moor WNW von Hausen |
|
673R008 |
Hausen position |
Rhön | The Black Moor is one of the largest and best preserved moorlands in the Rhön. The visitors are led through the raised bog on wooden planks. Signs show the origin and ecology of the moor. An observation tower provides an overview. | 1200000 1500 × 800 |
Type: raised bog, low bog Type: peat, basalt |
no information | precious | Nature reserve, landscape protection area, FFH area | Bavaria's most beautiful geotopes No. 47 |
Basalt block heaps on Gangolfsberg NW of Oberelsbach | 673R009 |
Oberelsbach position |
Rhön | The block heap made of early Tertiary basalt covers large areas of the west side of the Gangolfsberg. | 20000 200 × 100 |
Type: Blockmeer Type: Basalt |
block | precious | Nature reserve, landscape protection area, FFH area | ||
Arnsberg NE volcanic residue from Wildflecken | 673R010 |
Bischofsheim in the Rhön position |
Rhön | The summit area of the Arnsberg consists of a morphologically striking basalt dome, which towers over the surrounding Lower Muschelkalk by about 50 m. The hiking trail leading to the summit shows the Lower Muschelkalk pending, while the partially wooded hilltop offers opportunities to find basalt (partly pending, partly as reading stones). | 250000 500 × 500 |
Type: volcanic vent, cliff Type: basalt, limestone |
Rock slope / cliff | precious | Landscape protection area |
See also
- List of nature reserves in the Rhön-Grabfeld district
- List of landscape protection areas in the Rhön-Grabfeld district
- List of FFH areas in the Rhön-Grabfeld 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 Rhön-Grabfeld district - collection of images, videos and audio files