List of geotopes in the Miesbach district

This list contains the geotopes of the Upper Bavarian district of Miesbach 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
Molasse outcrops in the Leitzach Valley		182A002	Fischbachau position	Paar-Isar region	A profile through the south wing of the Haushamer Mulde with the seam group, building block layers and clay marl layers is exposed.	3000 500 × 6	Type: Layer sequence, Animal fossils, Vegetable fossils Type: Sandstone, Marlstone, Brown coal	embankment	precious	FFH area
Molasse outcrops in the Sulzgraben		182A003	Miesbach position	Paar-Isar region	A profile through the N wing of the Haushamer Mulde is unlocked. The outcrop has partially collapsed.	18000 1200 × 15	Type: Layer sequence, Animal fossils, Vegetable fossils Type: Sandstone, Marlstone, Brown coal	Impact slope / river bed / stream profile	especially valuable	Landscape protection area, FFH area
Helvetikum outcrops in the Breitenbach Gorge		182A004	Schliersee position	Mangfall Mountains	The profile shows Schrattenkalk, Gault sandstone and Seewer limestone. Drusberg layers can be found in the saddle structure on the west side of the Breitenbach.	2000 200 × 10	Type: Layer sequence, Animal fossils Type: Limestone, Sandstone	Impact slope / river bed / stream profile	precious	Landscape protection area
Former Kalkgraben quarry		182A005	Schliersee position	Paar-Isar region	The type locality of the Kalkgraben formation in the flysch is here. This corresponds to the rock sequence previously known as the cement marl series. The former quarry is private property and is built on.	800 40 × 20	Type: Type locality, sedimentary structures Type: Limestone	Quarry	precious	no protected area
Molasse outcrop in the Schmerold Graben		182A007	Gmund am Tegernsee position	Paar-Isar region	In the poorly open-minded profile, v. a. Lower freshwater molasses can be seen (Tieferes Chatt and Rupel of the Haushammer Mulde).	6500 650 × 10	Type: Layer sequence Type: sandstone, marlstone, lignite	Impact slope / river bed / stream profile	precious	FFH area
Abandoned quarry sharpening		182A009	Kreuth position	Mangfall Mountains	In the former quarry, there is a steep succession of limestones from the alpine shell limestone to part nachschichten and marl. In the Alpine Muschelkalk, clear sediment structures (Wurstelbanks) can be seen, which are unique in terms of shape and extent in the Bavarian Alpine region. Thin layers of Pietra Verde are equally open. The part nights are delimited by a disturbance. The site is used as a storage area for building materials and machines.	7200 180 × 40	Type: Sedimentary structures, layer sequence Type: Limestone, claystone	Quarry	especially valuable	Natural monument
Pitch coal exposure on the Gschwendtner Bach		182A011	Hausham position	Paar-Isar region	An approx. 0.5 m thick coal seam is exposed on the rebound slope and in the bed of the Gschwendtner Bach.	50 10 × 5	Type: Layer sequence, Plant fossils, Animal fossils Type: Brown coal, sandstone	Impact slope / river bed / stream profile	precious	Landscape protection area
Former Tufa limestone quarries Maxlmühle NW of Weyarn		182A012	Valley position	Paar-Isar region	The limestone stores in the Mangfall valley near the Maxlmühle were already mentioned by Flurl (1792).	200 20 × 10	Type: Animal Fossils, Vegetable Fossils, Rock Type: Tufa	Quarry	significant	FFH area
Flysch outcrop N of Bad Wiessee		182A013	Bad Wiessee position	Isar-Loisach young moraine region	The Reiselsberg sandstone is particularly easily accessible at the road outcrop at the northern exit of Bad Wiessee. There is a parking lot across the street. Caution: busy road, the outcrop is in a curve. The outcrop is separated from the sidewalk by a concrete barrier and a chain link fence.	200 40 × 5	Type: Rock Type: Sandstone	embankment	precious	Landscape protection area
Abandoned quarry Schönet		182A014	Kreuth position	Mangfall Mountains	In the Schönet quarry, Tegernsee marble was mined earlier (until 1954). The break is still well preserved, but has overgrown.	5000 100 × 50	Type: Rock Type: Limestone	Quarry	significant	Landscape protection area
Triassic / Jura border in the Ankerstube SE quarry in Rottach-Egern		182A015	Rottach-Egern position	Mangfall Mountains	Trias-Lias border (Upper Rhätkalk - Adneter Kalk) and lowest banks of the Red Limes. The profile was considered by the Jura Sub-Commission as a standard profile for drawing the boundary between the Triassic and the Jura.	7800 130 × 60	Type: Standard / Reference Profile, Animal Fossils Type: Limestone	Quarry	especially valuable	Landscape protection area, FFH area, bird sanctuary
Rotwand with Rotwand Kalkken		182A016	Bayrischzell position	Mangfall Mountains	Exemplary open and clearly visible sequence of layers on the Rotwand south slope. Type locality of the Rotwand layers, Chiemgau formation with steeply set up silica limestone of the Rotwandköpfe.	350000 1000 × 350	Type: Type locality Type: Limestone	Rock slope / cliff	precious	Landscape protection area, FFH area, bird sanctuary
Preworm period Nagelfluh on Söllbach SW of Bad Wiessee		182A017	Bad Wiessee position	Mangfall Mountains	Sediments from older ice ages are rare within the distribution area of the Würmzeit glaciation, as they were mostly taken and processed by the younger glaciers. In the Söllbachtal below the Scheibenaualm, the slopes on both sides are built up by mighty spikes. The sediments are particularly impressive towards the waterworks.		Type: sequence of layers, type of rock, type: conglomerate	Impact slope / river bed / stream profile	precious	Landscape protection area
Rock tower and fossils of the Blankenstein SSE from Rottach-Egern		182A018	Rottach-Egern position	Mangfall Mountains	The striking (climbing) rocks of the Blankenstein are made of Upper Rhätkalk. The sequence of layers is set up vertically (saiger) here. In the lying part - towards the marbled and clayey-slippery weathered Kössen formation on the Blankenstein saddle - there are plenty of corals in the rock and in the reading stones. The Blankenstein is on the Sutten - Kreuth stage of the Via Alpina hiking trail. It can be reached with the slightest difference in altitude (on foot) from the Wallbergbahn mountain station on the Alpine nature trail.	80000 500 × 160	Type: Animal Fossils, Rock Tower / Needle Type: Limestone, Marlstone	Slope crack / rock wall	precious	FFH area, bird sanctuary
Show mine (in development) Deisenrieder Wetterstollen		182G002	Fischbachau position	Inn-Chiemsee-Jungmoränenregion	The Deisenried weather tunnel was started in 1953 to ventilate the Hausham coal mine. In 1956 the breakthrough from the Deisenried tunnel to the 3rd level of the Hausham pit took place and the fan was put into operation the following year. It discharged the air from the tunnel and thus sucked in fresh air through the mine building via the lift shaft at Hausham, 12 km away. With the cessation of the Haushamer coal mining and after dismantling work, the last shift ran over the tunnel in October 1966. It was partially backfilled and sealed until 1977. Since 2006 it has been re-opened to give the public access to a show mine in the future. Please send inquiries about the status of the development to the Fischbachau community, Tel. 08028 / 9066-0. The tunnel crosses 44 m Quaternary, then 21 m marine building block layers of the Oligocene made of sandstones and conglomerates. This is followed by limnic, brackish and marine deposits of sandstones and clay marls. At a tunnel length of 290 m, the 80 cm thick small coal seam is exposed.	2400 800 × 3	Type: Stollen Type: Lignite	Tunnel / gallery / shaft	precious	no protected area
Sulfur water source of the stinker ditch SW of Bad Wiessee		182Q001	Bad Wiessee position	Mangfall Mountains	The Stinkergraben got its name from the smell of hydrogen sulphide that stings on the nose again and again on the hiking trail through the valley. If you follow the stream upwards in search of the source, you will notice that hydrogen sulfide is evidently always released where the stream water bubbles over gradients and bright white biofilms cover stones or branches. The conspicuous biofilms are communities of different microorganisms. They sometimes form long threads (filaments, streamers) and - like elsewhere - are likely to consist mainly of hydrogen sulfide oxidizing bacteria. The spring water has high sulphate, hydrogen sulphide and strontium contents. The hydrogen sulfide content of the spring water comes from the anaerobic bacterial reduction of sulfate. The sulphate comes from the gypsum of the Raibl Formation, which Gümbel (1861) discovered near the source and had it excavated in an experimental building under massive debris. The sulphurous water source with a dilapidated wooden frame is found at 1,100 m below the hiking trail, where a stone-filled box lies in the path.	400 200 × 2	Type: Mineral Spring Type: Gypsum, Marlstone, Rauhwacke	other information	especially valuable	Landscape protection area
Meander of the Red Valepp	more pictures	182R001	Schliersee position	Mangfall Mountains	Beautifully formed meanders in the post-glacial gravel of the valley floor show the undisturbed course of the Rote Valepp.	100000 500 × 200	Type: Meander Type: Gravel	no information	significant	Landscape protection area, FFH area, bird sanctuary
Rotachfall		182R002	Rottach-Egern position	Mangfall Mountains	The Rottach falls towards Rottach-Egern east of the Wallberg over five closely spaced steep steps with waterfalls in the limestone range.	480 80 × 6	Type: Waterfall Type: Limestone	Impact slope / river bed / stream profile	significant	Landscape protection area
Aiplspitz with Karen	more pictures	182R003	Fischbachau position	Mangfall Mountains	In the east and north of the Aiplspitz there are several cirques with alpine pastures.	3000000 3000 × 1000	Type: Karling, Kar Type: Limestone	Slope crack / rock wall	precious	Landscape component, FFH area, bird sanctuary
Fuchsstein boulder		182R004	Fischbachau position	Mangfall Mountains	The 5 to 6 m high limestone boulder is stored on the highest lateral moraine of the Leitzach Glacier.	25 5 × 5	Type: Boulder Type: Limestone	block	significant	Natural monument
Felstor Breitensteiner window	more pictures	182R005	Fischbachau position	Mangfall Mountains	The single cliff in the Wetterstein Limestone has a summit cross.	225 15 × 15	Type: rock tower / needle, karst halfway / natural bridge Type: limestone	Slope crack / rock wall	significant	Natural monument
Glacier cut on the Hammer Felsriegel		182R007	Fischbachau position	Mangfall Mountains	The glacial cut was exposed by the gravel mining.	6 6 × 1	Type: glacial cut, rock type: limestone	Slope crack / rock wall	precious	no protected area
Schmelzwassertal Teufelsgraben SW of Holzkirchen	more pictures	182R010	Holzkirchen position	Paar-Isar region	The Teufelsgraben is an impressive glacial meltwater channel of the Tölzer Glacier Globe. A variety of outcrops can be found on the slopes, e.g. B. from Mindel-Ice Age Schotternagelfluh.	1200000 4000 × 300	Type: Schmelzwassertal Type: gravel, conglomerate	no information	precious	no protected area
Röthensteinkar with Karsee		182R011	Rottach-Egern position	Mangfall Mountains	A small cirque with a lake typical of the region, the construction of which was made easier by clearing out the softer Kössen layers.	200000 1000 × 200	Type: Kar Type: Marlstone	Slope crack / rock wall	significant	FFH area, bird sanctuary
Humpback meadows in the Kloo-Ascher Valley		182R012	Bayrischzell position	Mangfall Mountains	Buckelwiesen represent a geomorphological peculiarity of the alpine region: the surface of water-permeable limestone soils with thin, nutrient-poor humus layer was formed wavy (bumpy) by frost pressure and solution weathering. The meadows are partially meliorated today. The entire area is covered by the Bayer. Contract nature conservation program funded.	24000 300 × 80	Type: Buckelwiese Type: Gravel	no information	precious	Landscape protection area, FFH area, bird sanctuary
The Schneid W landslide from Bayrischzell		182R013	Bayrischzell position	Mangfall Mountains	To the north of the Schneid there is a very pronounced and deeply incised erosion gap. The falling cone below extends into the Leitzach valley.	300000 1000 × 300	Type: Landslide Type: Dolomite stone	Slope crack / rock wall	precious	Landscape reserve, bird sanctuary
Thunder holes on the Stümpfling		182R014	Schliersee position	Mangfall Mountains	A large slab of Rätkalk has broken here due to creeping movements in the underlying Kössen layers. In some cases, blocks the size of a house were created. A large number of sloping and fallen trees indicate that the movements are continuing.	125000 500 × 250	Type: Landslide Type: Limestone	block	precious	Landscape protection area
Landslide deposits in the fairytale forest near Aurach		182R015	Fischbachau position	Mangfall Mountains	The so-called fairy tale forest is the deposit area of a postglacial, but probably prehistoric landslide from Auracher Köpferl. A large part of the fall mass is surrounded by a wall. Inside the wall you will find a charming block landscape with up to 15 m high tumuli and boggy depressions. The hills consist mainly of Raibler limestone.	500000 1000 × 500	Type: Rockslide Type: Dolomite stone	block	precious	no protected area
Taubenstein		182R016	Schliersee position	Mangfall Mountains	Carbonate reef in the Kössen strata. Reef builder in life position. Massive facies with transition to banked facies.	25000 250 × 100	Type: Ridge, Type of rock, Animal fossils, Sedimentary structures Type: Limestone	Rock slope / cliff	precious	Bird sanctuary
Ruchenköpf	more pictures	182R017	Bayrischzell position	Mangfall Mountains	Massive Oberrhätkalk with red Lias base limestone (Adneter Kalk). Shingling / displacement and extreme folding to form a hollow can be seen as an example.	400000 800 × 500	Type: rock wall / slope, sequence of layers, fold / hollow / saddle, fault type: limestone	Rock slope / cliff	precious	Landscape protection area, FFH area, bird sanctuary
Moraine in the Schinderkar		182R018	Rottach-Egern position	Mangfall Mountains	Kar of the late glacial Schinder glacier with excellent lateral and terminal moraines of a retreat stage.	400000 1000 × 400	Type: End (wall) moraine Type: Gravel	no information	significant	FFH area, bird sanctuary
Hochmiesing with mountain tears		182R019	Bayrischzell position	Mangfall Mountains	Sliding mass on the southern slope of Hochmiesing. Clear neck valleys in the ridge area. On the mountain flank bulging and kinking of the moving benches parallel to the layers.	120000 400 × 300	Type: Landslide Type: Limestone	Slope crack / rock wall	precious	Landscape protection area, FFH area, bird sanctuary
Nice pools of the Pfanngraben		182R020	Schliersee position	Mangfall Mountains	Large pools were carved into the partially deeply cut gorge of the Pfanngraben by the flowing water.	25000 500 × 50	Type: Kolk, gorge, stream / river course Type: Dolomite stone	Impact slope / river bed / stream profile	significant	Landscape protection area, FFH area, bird sanctuary
Mure at the Grundalm		182R021	Bayrischzell position	Mangfall Mountains	Mur Canal, Murkegel with four different sub-subjects (historical - recent) in exemplary training.	12000 200 × 60	Type: Alluvial fans, landslide Type: Gravel	other information	precious	Landscape protection area, FFH area, bird sanctuary
Mangfallknie NW of Westerham		182R022	Valley position	Paar-Isar region	The Mangfallknie with the Untere Teufelsgraben in the west and the beginning of the Grub-Harthausen Dry Valley in the north impressively reveal the late glacial history of the river on the edge of the Inn glacier. First of all, the drainage to the north took place through the now dry Grub-Harthausen Schmelzwassertal (Ur-Mangfall). After the glaciers melted back, the Mangfall was diverted to the southeast in the direction of the steeper gradient. As a result, it cut like a gorge. The Teufelsgraben flows into this gorge at Mangfallknie. It represents the former drainage channel of the Tölzer Lobus of the Isar glacier. The best view of the situation of the Mangfallknee is from the level crossing below Grub. Other striking objects are the pipe bridge of the old Munich water supply and an outcrop on the bank of the Mangfall east of the bridge at Grubmühle, which shows that the Mangfall has cut down to the molasses sediments below the Quaternary gravel.	4860000 2700 × 1800	Type: Schmelzwassertal, stream / river course, terrace, end (wall) moraine Type: moraine, gravel, gravel	Impact slope / river bed / stream profile	precious	FFH area
Marienstollen and former quarry of the Marienstein cement works		182A001	Waakirchen position	Isar-Loisach young moraine region	In 1835, cement marls were found near today's Marienstein and in 1850 a cement factory was opened. Pitch coal was extracted from the Barbarastollen for the plant's own use. In 1885 the Marienstollen, from which cement stone was extracted, was approached. These were so-called stink stones, bituminous marl and limestone marl stones from molasses. Later, cement marl - marl stones of the Helveticum - were extracted from the tunnel, which was ultimately 2,000 m long. Most recently, the cement works obtained its raw material from a large quarry on the Bacheralm - 700 m south of the entrance to the Marienstollen. There, marl stones of the ultra-Helvetian marl series were mined. The closed and weathered entrance portal of the Marienstollen can still be found south of the old factory premises. The geological profile of the tunnel is enclosed with the explanations of the geological map. Up in the recultivated quarry, the marl stones of the marl series are only exposed at one point.	6000 2000 × 3	Type: Rock type, tunnel type: Marlstone	Tunnel / gallery / shaft	significant	Landscape protection area
Kössener Kalke north of the Kothalm ESE from Fischbachau		182A008	Fischbachau position	Mangfall Mountains	The hiking trail from the Kesselalm to the Kothalm runs on the western slope of the Schweinsberg in fossil-rich Kössen limestone. In a ditch - right where the path enters the forest - limestone and marl limestone with remains of mussels, oysters, corals and sea lilies can be found above and below the path. The light rock walls further above are made of Upper Rhätkalk, which, in the shape of a bowl, forms the top of the Schweinsberg.	30 15 × 2	Type: Animal fossils, layer sequence Type: Limestone, limestone marl	Impact slope / river bed / stream profile	precious	no protected area
Mindelzeitliche Nagelfluh E from Pelletsmühl		182A010	Holzkirchen position	Isar-Loisach young moraine region	Nagelfluh is on the road that leads down from the B13 to Pelletsmühl. It is classified as minimum time. In the Nagelfluh, half-caves have been created by weathering the scree component.	3600 120 × 30	Type: Rock Type: Conglomerate	Slope crack / rock wall	significant	no protected area
Clay marl layers on the Leitzach S von Drachenthal		182A019	Fischbachau position	Paar-Isar region	About 80 m east of the new bridge over the Leitzach, and visible from it, there are layers of clay marl on the slope of the Leitzach and in the river bed of the Lower Oligocene. They contain large and thick-skinned molluscs, but they disintegrate quickly when they dry out. Where the clay marl layers on the bank were washed away in summer 2018 (Fig. 2), a year later there was a wild landslide (Fig. 4) - probably not caused by fossil collectors, as was initially feared, but by the spring flood. Immediately to the south-east of this is the slope area, which is now completely overgrown in the lower part, from which Pflaumann & Stephan have recovered a rich fauna on the fresh landslide. The slide is already mentioned by Gümbel (1875). The trailing edge at the top of the slope shows Nagelfluh and gravel moraine over layers of clay marl.	3500 70 × 50	Type: Animal Fossils Species: Moraine, Conglomerate, Clay Marlstone	Impact slope / river bed / stream profile	precious	FFH area
Pitch coal seams on the Leitzachtal slope SSE of Drachenthal		182A020	Fischbachau position	Paar-Isar region	On a new forest path on the Leitzach valley slope, several pitch coal seams of the brackish water molasse are currently (2018) tipped over. The coal is temporarily stored in sand and marl stones with shell shells. Gümbel has the Flötz No. in his card from 1875. 2 drawn. Further up there are limestone tuffs and the Wurmzeitliche Nagelfluh and gravel moraine.	240 120 × 2	Type: Type of rock, type of layers : brown coal, sandstone, marlstone	Slope crack / rock wall	precious	FFH area
Outcrops in the Rohnbachtal WSW from Wörnsmühl		182A021	Fischbachau position	Paar-Isar region	In the Rohnbachtal, the coal-bearing formations of the Oligocene in the south wing of the Haushamer Mulde are easily accessible. The layers are stored tipped over. Up the Rohnbach, layers from the younger to the older are crossed. The outcrops in the Rohnbachtal are described in the explanations of the geological map (p. 253). From the confluence of the Rohnbach into the Leitzach upwards, sandstone and marl stone banks alternate between fossil-bearing brackish and limnic horizons with pitch coal seams. The seams are not noticeable, but bits of pitch coal can be found in the stream. About 500 m from the beginning of the valley, beautiful moss-covered tufa cascades are formed on the southern slope of the valley. Behind a building on the way is an old cement quarry. At the object point there is an approx. 20 cm thick coal seam directly on the stream. 90 m up the stream, there are reservoir sediments - finely layered silts - on the north side. Another 300 m upwards near the third ford on the map, the coal seam should be in the stream and in a side ditch. But even here there are only bits of pitch coal in the streambed.	40000 2000 × 20	Type: sequence of layers, type of rock Type: lignite, marl limestone, sandstone	Impact slope / river bed / stream profile	precious	no protected area
Nagelfluh via Molasse am Moosbach SE from Valley		182A022	Weyarn position	Inn-Chiemsee-Jungmoränenregion	To the east of the confluence of the Moosbach into the Mangfall, sandy marls of the Upper Freshwater Molasse under the at least-period Nagelfluh can only be reached without a path. The Nagelfluh forms impressively high walls from which the gravel weather and rubble slopes form at the foot of the wall. Only in the very east have the gravels not yet covered the underlying marls of the OSM, or rather the impact slope of the Moosbach keeps the outcrop free. The water-retaining and softly weathering marls are also the reason for blocks of the overlying Nagelfluh to slide along the entire wall towards the west. In such an exposed wall above large fall blocks in the Nagelfluh exposed weathering vents, similar to geological organs, can be seen. Be careful, stay away from the steep and overhanging walls - risk of falling rocks!	3000 150 × 20	Type: Layer sequence Type: conglomerate, clay marl	Slope crack / rock wall	significant	FFH area
Molasse of the Köcker trench W of Au b. Bad Aibling		182A023	Irschenberg position	Inn-Chiemsee-Jungmoränenregion	In the Köcker Graben a profile through the main Cyrenen layers of the lower brackish water molasse is exposed. The alternation of marlstones with sandstones contains coal seams.	10000 500 × 20	Type: Layer sequence Type: Marlstone, sandstone, brown coal	Impact slope / river bed / stream profile	significant	no protected area
Molasse of the Kaltenbachgraben ENE von Miesbach		182A024	Irschenberg position	Inn-Chiemsee-Jungmoränenregion	In 1875 Gümbel wrote about the extremely impassable Kaltenbach, which offers by far the best and most productive outcrop in these strata - what is meant is the Upper Sea Molasse. The Kaltenbachgraben is not that impassable (anymore) - rather its side ditches - but it has retained its importance as an important outcrop in the Upper Marine Molasse through further processing - above all by Hölzl in 1958. The upper sea molasse begins about 200 m downstream from the object point as an alternating sequence of marls and sands with a rich fauna. Fossils are also found not far up the ditch branching off to the SW from the object point (Fig. 1). However, these originate from the main Cyrene layers of the lower brackish water molasse beyond a thrust. And upstream from the object point there are gray marls of the lower sea molasses (Fig. 2), from which fossil-rich rubble (Fig. 3) in the stream could come. Lime-separating spring water has left beautiful leaf marks in the limestone tuff nearby (Fig. 4).	60000 2000 × 30	Type: Layer sequence, Animal fossils, Vegetable fossils Type: Tufa, marl, sand	Impact slope / river bed / stream profile	precious	no protected area
Schurfstollen at Klammstein SE from Spitzingsee		182G003	Schliersee position	Mangfall Mountains	In the northwest, under the rock wall of the Klammstein, there is a mining tunnel only a few meters deep in dark red lump limestone of the Adnet formation. There are sawing marks on the tunnel walls. What the reason for the supposed mining attempt was today is unknown. Perhaps the red color of the rock suggested iron ore.	10 5 × 2	Type: Stollen Type: Limestone	Tunnel / gallery / shaft	precious	Landscape protection area, FFH area, bird sanctuary
Source of the Quirinus oil in Bad Wiessee		182G004	Bad Wiessee position	Mangfall Mountains	In 1441 a strip of floating oil was discovered on the Tegernsee. He was followed to a spring above the Rohbogen courtyard. There a crude oil leaked out, which was subsequently bottled by the Tegernsee monastery for centuries and sold as healing Quirinus oil. The Quirins Chapel was built at the point of the source outlet. The oil was siphoned off by locals from other wells and used as heating oil and lubricating oil. Today no more oil escapes here, because from 1838-1840 the Bavarian state tried to extract oil in shafts and tunnels and from 1882 onwards, drilling for oil was started here in Bavaria for the first time. The numerous wells that were sunk in the first oil boom in Bavaria caused the spring to dry up. In the ditch below the chapel there are shiny films on spring water, but of iron and not of oil. Only on the Tegernsee below are there occasionally small oil films that come from leaking crude oil. According to the drilling results, the oil comes from the Flysch / Helvetikum thrust area, but the bedrock could also be in the thrust molasses.	25 5 × 5	Type: shaft type: not specified	no information	significant	Landscape protection area
Headframe of the Klenzeschacht of the Hausham coal mine		182G005	Hausham position	Paar-Isar region	Coal mining in the Hausham district began around 1860 and ended when it was shut down in 1966. The winding tower built in 1934/35 and listed above the former Klenzeschacht is a relic of 105 years of mining history.	900 30 × 30	Type: Shaft Type: Lignite	Tunnel / gallery / shaft	precious	Monument protection, landscape protection area
Spring pots on the Leitzach S of Osterhofen		182Q002	Bayrischzell position	Mangfall Mountains	At the foot of the Seeberg, groundwater emerges from the debris cone. The geological map shows a boggy area with Late Worm to Holocene basin silts and clays. The source situation can perhaps best be explained in such a way that groundwater from the Seeberg cannot pass directly from the rubble into the valley gravel as elsewhere, but is dammed on the basin silts and forced to escape. Some of the groundwater emerges in springs, beautiful but also ascending in spring pools. The area is a valuable biotope with rare plant species.	43750 250 × 175	Type: Debris source Type: peat, clay, silt	no information	significant	Landscape protection area
Tufa springs in Mangfalltal SSE von Valley		182Q003	Valley position	Paar-Isar region	To the south-southeast of Valley, numerous springs emerge on the western slope of the Mangfall valley. Lime-rich water from Pleistocene gravel emerges on damming marls of the Upper Freshwater Molasse. The spring situation has led to extensive landslides. Precipitated lime in the spring water has built up tuff terraces and dammed up a spring pool. The old Munich aqueduct runs through the headwaters. Please do not step on the sensitive tuff terraces!	500 50 × 10	Type: Layer source Type: Tufa	Rock slope / cliff	significant	FFH area
Dolines and ponors on the Breitenstein E of Fischbachau		182R023	Fischbachau position	Mangfall Mountains	In the alpine area up on the Breitenstein there are several sinkholes, one of which is circular and filled with water. The alpine farmer tells of how years ago he heard an unusual noise while working and then discovered that the sinkhole had emptied. In the opening at the bottom of the sinkhole, water is said to have rushed like a river and no impact was heard from stones thrown into it. The hole was closed with a stone and sealed so that a pond could again be dammed up for drinking cattle. The geological map shows a partly scaled strip of Raibl formation with sandstones, limestone and Rauhwacken in the steep Wetterstein limestone. It extends as a depression from W to E to behind the Hubertushütte. There are other small sinkholes and swallow holes (ponors). It cannot be decided whether the gypsum solution in the Raibl Formation was involved in the formation of the hollow form or whether it is purely due to karstification of limestone (in the Raibl Formation and Wetterstein limestone). WE disturbances will have prepared the waterway.	5600 280 × 20	Type: Dolinenfeld Type: Sandstone, Limestone	Sinkhole / sinkhole	significant	no protected area
Jenbach waterfalls in the Flysch S of Bad Feilnbach		182R024	Fischbachau position	Mangfall Mountains	From the hiking car park Oberes Jenbachtal, the Wasserfallsteig can be walked downwards (return upwards on the asphalt road). The inspection requires surefootedness. Caution - the path is dangerous for falling rocks! The path along the Jenbach crosses an alternation of limestone marl stones and limestones of the Kalkgraben formation. The Jenbach waterfall falls on a hard bench.	16000 400 × 40	Type: waterfall, layer sequence type: limestone marl stone, limestone	Impact slope / river bed / stream profile	precious	no protected area
Großdoline on the Lahnenkopf SW of Schliersee		182R025	Schliersee position	Mangfall Mountains	The deepest sinkholes in the Bavarian Alpine region are located on the Lahnenkopf and further west on the Baumgartenschneid. The sinkhole on the Lahnenkopf can be reached without a path up the slope via the alpine meadows of the Obere Krainsberger Alm. It has a diameter of 90 m and is 20 m on the valley side and 80 m deep on the slope side. The descent to the deepest of the dolines down the steep inner slope requires surefootedness. In the sinkhole there are steep main dolomite and plate limestone. After the explanations of the geological map, the base of the Kössen formation with black marls is also exposed in the sinkhole. The formation of sinkholes to this extent can only be traced back to the gypsum solution in the Raibl formation. The tectonic hollow situation on the Lahnenkopf makes it plausible that the Raibl Formation, which extends further to the north, is here in the deeper subsurface.	9000 100 × 90	Type: sinkhole Type: marl stone, limestone, dolomite stone	Sinkhole / sinkhole	precious	no protected area
Waterfall in Raibler Kalken on Lohbach SW of Rottach-Egern		182R026	Kreuth position	Mangfall Mountains	After we ... had won the country road again, we soon reached the place marked with a special sign, where a separate walking path, off the country road on the right, leads to the waterfall on the Lohbache, which we reached after a quarter of an hour. Although more arid than the other cataracts in the area, the waterfall on the Lohbache is nevertheless one of the most interesting and picturesque, and any stranger susceptible to noble natural beauty would do an injustice to leave it unvisited. This is what it says in a script from 1832. In the first half of the 19th century, it was still a tourist destination and marked with an access path in the first Bavarian image, but today the waterfall has been forgotten and the path overgrown. The waterfall can still be reached on the north side along the Lohbach stream. The little water in the Lohbach rushes down from the core of a vertically positioned fold of Raibler Kalk.	300 20 × 15	Type: waterfall, type of rock, type of storage : limestone	Slope crack / rock wall	precious	Landscape protection area
Cliff of Nagelfluh SE from Valley		182R027	Weyarn position	Paar-Isar region	A hole in the digital terrain model drew attention to this Nagelfluh block. It is lined with trees and the roots of the tree are still attached to the main rock. But he has already moved away from the main rock within a meter. This incision is the hole in the DTM. Sintering on the parting surface shows that the crevice had opened a long time ago. A moss-free edge area at the bottom of the crevice, on the other hand, seems to be an indication of recent opening movements, just like the tense roots above. Sooner or later the block will peel off completely and fall into the valley. Be careful at the edge of the terrain - risk of falling!	25 5 × 5	Type: Boulder Type: Conglomerate	Rock slope / cliff	significant	FFH area
Retreat moraine NW of Irschenberg		182R028	Irschenberg position	Inn-Chiemsee-Jungmoränenregion	To the northwest of Irschenberg are moraine rings of the retreat stages on the western edge of the Inn glacier. The landscape shows forms of ice decay. On the Schmalzberg, a temporary meltwater valley in front of the moraine wall can be seen in the digital terrain model (Fig. 4).	3000000 2000 × 1500	Type: End (wall) moraine, Schmelzwassertal Type: moraine	no information	significant	no protected area
Ice crumbling landscape at the Allgau Chapel E von Piesenkam		182R029	Waakirchen position	Isar-Loisach young moraine region	The Allgau Chapel stands on a retreat moraine of the Isar glacier from the Würmzeit period. Its Tölzer Lobus extended with its maximum extent another 3 km further east to the Taubenberg. Here, east of Piesenkam, the digital terrain model shows several successive moraine rings. For larger differences in relief, such as east of the chapel, they are covered with forest. To the west of the chapel they are a bit more dissolved as a ground moraine landscape with forms of ice decay and can then be used for agriculture.	700000 1000 × 700	Type: Ice crumbling landscape Type: Moraine	no information	significant	Landscape protection area
Terminal moraine wall of the Isar-Loisach glacier near Großhartpenning		182R030	Holzkirchen position	Paar-Isar region	At Großhartpenning, the outermost terminal moraine wall of the Isar-Loisach glacier (Tölzer Lobus) extends from WSW to ENE. Seen from the gravel plain in front of it, it rises almost 40 m.	3150000 4500 × 700	Type: End (wall) moraine Type: Moraine	no information	precious	no protected area