List of geotopes in the Mühldorf am Inn district

This list contains the geotopes of the Upper Bavarian district of Mühldorf am Inn 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
Aubenham tertiary world		183A003	Oberbergkirchen position	Isar-Inn hill country	The abandoned marl pit opened up sediments from the Upper Freshwater Molasse as a raw material for the brick industry. Basal fine and coarse sands alternate with marls, limestone marls and clayey silts towards the hanging wall. Because of the rich plant fossil content, the pit is the type locality of Phytozone OSM-5. In addition to the first description of the genus Fagus (beech) in the Upper Freshwater Molasse, there was evidence of animal fossils of fish, mollusks, insects and deer-like mammals. There is an active pit in the same layers 200 meters to the northwest. The abandoned pit has been recultivated, there are residual outcrops of marl in the northeastern slope, otherwise a tertiary forest has been created here. A nature trail leads through the area. Fossils from the pit are on display in the neighboring school center. The Aubenham tertiary world is one of Bavaria's most beautiful geotopes and is explained on site with a corresponding information board.	90000 300 × 300	Type: standard / reference profile, plant fossils, animal fossils Type: marl, sand, silt	Clay pit / clay pit / marl pit	precious	no protected area	Bavaria's most beautiful geotopes No. 66
Dead ice kettle NW of Grub		183R003	Right-more position	Inn-Chiemsee-Jungmoränenregion	The property lies on the terminal moraine wall of the Kirchseeon retreat stage.	120 15 × 8	Type: Dead Ice Hole Type: Moraine	no information	significant	Natural monument
Death ice kettle NE from Höller		183R004	Right-more position	Inn-Chiemsee-Jungmoränenregion	The dead ice kettle lies on the wall moraine of the Kirchseeon retreat stage.	375 25 × 15	Type: Dead Ice Hole Type: Moraine	no information	inferior	Natural monument, part of the landscape
Dead ice kettle NW of Maxau		183R006	Gars at the Inn position	Inn-Chiemsee-Jungmoränenregion	The nearly circular dead ice hole lies in the forest and is heavily swamped. In the southwest there is a small open water area. The basin, which was temporarily overgrown, was cleared in 2011/2012. It is located on Toteiskesselweg Haager Land and is marked by a numbered (4) boulder.	900 30 × 30	Type: Dead Ice Hole Type: Moraine	no information	inferior	Natural monument, part of the landscape
Ice crumbling landscape N of Gänsgerbl		183R008	Gars at the Inn position	Inn-Chiemsee-Jungmoränenregion	The ice crumbling landscape near Gänsgerbl lies on the terminal moraine of the Kirchseeon retreat stage and presents typical relics of the late Ice Age: At that time, the living (moving) glaciers disappeared, ice masses and blocks separated from them and only later melted as dead ice under the protection of rubble and debris poured over them. What remained were steep-walled or cup-shaped hollow forms. At Gänsgerbl, these so-called dead ice holes are sometimes designed like textbooks.	108000 360 × 300	Type: Ice collapse landscape, dead ice hole Type: Moraine	no information	precious	Natural monument
Kettle N by Bergmann		183R009	Under riding position	Inn-Chiemsee-Jungmoränenregion	The elongated dead ice kettle lies in front of the wall moraine on worm and terminal moraine material.	7200 120 × 60	Type: Dead Ice Hole Type: Moraine	no information	significant	no protected area
Impact slope of the Inn NE from Heisting	more pictures	183R010	Polling position	Inn region	The Inn-Prallhang near Heisting is unobstructed. therefore it is still active and is constantly shifting. This means that fresh outcrops are permanently available. The boundary between molasse sediments and overlying glacial gravel is clearly visible on the impact slope. Near the, in the rocks of the Upper Freshwater Molasse at river kilometer 112, primeval elephants (gomphotheria) and in the low terrace gravel at river kilometer 110 a mammoth tooth were found. Such fossil finds can in principle also be expected in the area of the Heistinger Prallhang. The geotope is used as a local recreation area because of its beauty, its special vegetation (dry grass with pine vegetation) and favorable afternoon and evening tanning.	48000 800 × 60	Type: Impact slope, sequence of layers, animal fossils Type: sand, marl sand, gravel	Impact slope / river bed / stream profile	especially valuable	FFH area
Dead ice kettle W from Löfflmoos		183R011	Maitenbeth position	Inn-Chiemsee-Jungmoränenregion	The Toteisloch lies in the Würm terminal moraine wall of the Kirchseeon retreat stage. Its steep-edged basin is bordered almost all around by high flanks (up to 40 m). Only to the south does the basin open up with an embankment that is only 10 m high.	2100 70 × 30	Type: Dead Ice Hole Type: Moraine	no information	significant	Natural monument
Dead ice kettle N by Bachenöd		183R013	Gars at the Inn position	Inn-Chiemsee-Jungmoränenregion	The large, swampy dead ice hole with the partly steep edges and heavy vegetation is also interesting as a biotope. It lies in the restless relief of the terminal moraine wall of the Kirchseeon retreat stage.	5000 100 × 50	Type: Dead Ice Hole Type: Moraine	no information	significant	Natural monument
Kettle E by Löfflmoos		183R014	Maitenbeth position	Inn-Chiemsee-Jungmoränenregion	Water-filled kettle in the area of the distinctive moraine belt.	400 20 × 20	Type: Dead Ice Hole Type: Moraine	no information	significant	no protected area
Dead ice landscape SE from Weidholz		183R015	Right-more position	Inn-Chiemsee-Jungmoränenregion	Several shallow holes in the dead ice lie in the boggy bottom of a peripheral meltwater valley. The property is increasingly silting up and is being managed / researched.	100000 500 × 200	Type: ice crumbling landscape, meltwater valley , dead ice hole Type: gravel, moraine	no information	precious	no protected area
Terrace landscape between Gars and Au am Inn		183R016	Gars at the Inn position	Inn region	The terraced landscape between Gars and Au am Inn is built up from post-glacial terrace gravel as well as debris from the worm and crack ice age. The defense tower of the Stampfl Castle stands above the river terraces on old moraine material (lower old moraine with wall shape from the Rift Ice Age).	4500000 3000 × 1500	Type: terrace, hardwood Type: gravel, moraine	no information	significant	no protected area
Kettle SW by Maitenbeth		183R017	Maitenbeth position	Inn-Chiemsee-Jungmoränenregion	An elongated dead ice hole about 30 × 50 meters in size is surrounded by several smaller dead ice holes and a hilly relief. This ice crumbling landscape lies in the moraine ridges of the Würmglacials.	27000 180 × 150	Type: Dead ice hole, ice collapse landscape Type: Moraine	no information	significant	FFH area
Moraine landscape near Joppenpoint		183R018	Haag in Upper Bavaria position	Inn-Chiemsee-Jungmoränenregion	On the outskirts of Joppenpoint there is an area with a strongly hilly relief that does not consist of forest and is therefore particularly easy to recognize. The area is used for agriculture and is partially fenced. However, you have good views from Mühlstraße and from the beginning of Robert-Scherzer-Weg at the upper north-western end of the area.	30000 200 × 150	Type: End (wall) moraine Type: Moraine	no information	significant	no protected area
Tower from Nagelfluh above the barrage Teufelsbruck W von Wang		183R019	Under riding position	Inn-Chiemsee-Jungmoränenregion	A rock pillar from Nagelfluh stands directly on a hiking trail high above the Inn, east of the Teufelsbruck barrage. The conglomerate of calcareous cemented gravel shows abundant crystalline components. Würmzeit gravel is seldom cemented to Nagelfluh and in fact no further Nagelfluh can be observed in the gravel along the hiking trail. Perhaps the silty moraine cover over the gravel showed a hole here and seeping lime-rich water formed this column?	4 2 × 2	Type: Rock Tower / Needle Type: Conglomerate	block	precious	FFH area