List of geotopes in the district of Ebersberg

This list contains the geotopes of the Upper Bavarian district of Ebersberg 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
Nagelfluhwand Tegernau		175A001	Frauenneuharting ( 48 ° 1 ′ 21 ″ N, 12 ° 2 ′ 28 ″ E )	Inn-Chiemsee-Jungmoränenregion	In the former Nagelfluh quarry, you can find undivided slab gravel exposed.	1200 400 × 3	Type: Rock Type: Conglomerate	Quarry	significant	no protected area
Tufa quarry WSW from Pullenhofen	more pictures	175A003	Bruck ( 48 ° 1 ′ 44 ″ N, 11 ° 54 ′ 19 ″ E )	Inn-Chiemsee-Jungmoränenregion	In the Moosachtal w von Pullenhofen there is an abandoned quarry, in which tufa limestone was mined until 1972. The tuff was a popular building material until the 20th century. Numerous farmsteads in the area as well as the churches in Taglaching and Alxing were built from it. The Ludwigsbrücke in Munich was also clad with Pullenhofen tuff. The fact that the material was used earlier is confirmed by early medieval tuff plate graves that were discovered just north of Pullenhofen. On the opposite slope of the valley, remains of modern lime kilns indicate that the lime was also burned for the production of building materials and fertilizers. The mining area is already overgrown, the existing limestone tuff can only be found in a few places. In the immediate vicinity of the newer quarry, heavily rolled former mining sites with no outcrops prove the once larger scope of the extraction work. The springs that are responsible for the formation of the tuff are used today for drinking water.	4500 150 × 30	Type: Rock Type: Tufa, gravel	other information	precious	Landscape protection area, FFH area
Eisendorf drainage tunnel N	more pictures	175G001	Grafing near Munich ( 48 ° 1 ′ 10 ″ N, 11 ° 58 ′ 4 ″ E )	Inn-Chiemsee-Jungmoränenregion	The tunnel was built in 1829 to drain a lake and use the dry land for agriculture. It still fulfills its function as a water solution tunnel. The two first recordings from the 19th century show the lake before and the tunnel after. The tunnel entrance is in swampy pastureland, the exit on a steep slope with Nagelfluh banks.	100 100 × 1	Type: Gallery Type: Limestone, Gravel	no information	significant	Landscape protection area
Source outlets NW of Glonn		175Q001	Glonn ( 47 ° 59 ′ 34 ″ N, 11 ° 51 ′ 26 ″ E )	Inn-Chiemsee-Jungmoränenregion	In a steep valley to the west of Glonn, near Urspring, there are a number of strong springs. The stratified springs emerge at the boundary between the gravel and the Upper Freshwater Molasse. The outlet of water is influenced by the Flinzsockel above the bottom of the meltwater valley. The springs are difficult to access, some are in a fenced fish farm.	2000 50x40	Type: Layer source Type: crushed stone, marl	no information	significant	FFH area
Source outlets in Altenburg NW of Moosach		175Q002	Moosach ( 48 ° 2 ′ 9 ″ N, 11 ° 51 ′ 57 ″ E )	Inn-Chiemsee-Jungmoränenregion	The source horizon lies in the border area between the ceiling gravel and the upper freshwater molasse. There are several source outlets that have been caught. The spring ponds are used as fish ponds.	6000 300 × 20	Type: Constriction source Type: crushed stone, marl	no information	significant	Landscape protection area
Erratic block in Ebersberg		175R002	Ebersberg ( 48 ° 4 ′ 49 ″ N, 11 ° 57 ′ 47 ″ E )	Inn-Chiemsee-Jungmoränenregion	The Nagelfluhblock was moved from its original location in front of the secondary school in Ebersberg.	12 4 × 3	Type: Boulder Type: Conglomerate	block	inferior	Natural monument
Erratic block in Grafing		175R004	Grafing near Munich ( 48 ° 2 ′ 51 ″ N, 11 ° 58 ′ 10 ″ E )	Inn-Chiemsee-Jungmoränenregion	Block north of the wall of the parish cemetery. The original location of the block is unknown.	6 3 × 2	Type: Boulder Type: Blocks	block	significant	Natural monument
Erratic block in the Egmatinger Forst NE of Aying		175R005	Egmating ( 47 ° 59 ′ 3 ″ N, 11 ° 48 ′ 19 ″ E )	Inn-Chiemsee-Jungmoränenregion	The gneiss boulder in the Egmatinger Forest is partly embedded in Würm gravel.	12 5 × 2	Type: Boulder Type: Gneiss	block	significant	Natural monument, landscape protection area
Egglburger Os W from Ebersberg	more pictures	175R006	Ebersberg ( 48 ° 4 ′ 47 ″ N, 11 ° 56 ′ 18 ″ E )	Inn-Chiemsee-Jungmoränenregion	The Egglburger Os can be recognized as a striking range of hills over approx. 1 km. In the south, an inclined layer of clay, sand and gravel alternating as well as scratched debris is exposed.	240000 800 × 300	Type: Os Type: gravel, moraine	no information	precious	Nature reserve, landscape protection area
Ice crumbling landscape Dobel S von Grafing		175R007	Grafing near Munich ( 48 ° 1 ′ 59 ″ N, 11 ° 58 ′ 4 ″ E )	Inn-Chiemsee-Jungmoränenregion	The wooded area of the dead ice landscape is approximately one square kilometer. There are typical dry valleys, dead ice holes and kames.	1000000 1000 × 1000	Type: Kames, ice crumbling landscape Type: Moraine	no information	precious	Landscape protection area
Hupfauer Höhe in Ebersberg		175R008	Ebersberg ( 48 ° 4 ′ 24 ″ N, 11 ° 57 ′ 43 ″ E )	Inn-Chiemsee-Jungmoränenregion	It is a terminal moraine from the Ebersberg stadium.	40000 200 × 200	Type: End (wall) moraine Type: Moraine	no information	significant	Natural monument
Umlaufberg Roßkopf E from Ebersberg		175R009	Ebersberg ( 48 ° 4 ′ 44 ″ N, 11 ° 58 ′ 48 ″ E )	Inn-Chiemsee-Jungmoränenregion	The Umlaufberg was created by meltwater erosion from the terminal moraine wall of the Ebersberger Stadium.	18000 300 × 60	Type: circulation / breakdown Mountain Type: Moraine	no information	precious	no protected area
Erratic block SW of Moosach		175R010	Moosach ( 48 ° 1 ′ 41 ″ N, 11 ° 52 ′ 17 ″ E )	Inn-Chiemsee-Jungmoränenregion	The sandstone block was exposed during road construction. It shows clear polish and scratches.	12 4 × 3	Type: Boulder Type: Sandstone	block	significant	Landscape protection area
Dead ice hole 1 SW of book		175R011	Kirchseeon ( 48 ° 3 ′ 21 ″ N, 11 ° 50 ′ 46 ″ E )	Inn-Chiemsee-Jungmoränenregion	The dead ice hole is overgrown with silting societies and large sedge. It is endangered by agriculture.	12000 120 × 100	Type: Dead Ice Hole Type: Gravel	no information	significant	no protected area
Terrace between Gutterstätt and Baumhau		175R014	Moosach ( 48 ° 2 ′ 1 ″ N, 11 ° 53 ′ 46 ″ E )	Inn-Chiemsee-Jungmoränenregion	There is a striking terrace between Gutterstätt and Baumhau. It is laid out in the gravel of the Inn glacier from the Würm period. The eastern area is used for grazing purposes and is therefore largely kept free of disturbing vegetation. Therefore, this section is particularly easy to see from the Gutterstätt - Taglaching road. In contrast, the western part of the terrace is less easy to see because of the trees (Fig. 3). At the foot of the terrace there are occasional springs where spring tufa forms (Fig. 4).	75000 750 × 100	Type: Terrace Type: Gravel, Tufa limestone	no information	precious	no protected area

Individual evidence

↑ Data source: Bavarian State Office for the Environment, www.lfu.bayern.de, Geotoprecherche (accessed on September 16, 2017)

Map with all coordinates: OSM | WikiMap

[1] Data source: Bavarian State Office for the Environment, www.lfu.bayern.de, Geotoprecherche (accessed on September 16, 2017)

List of geotopes in the district of Ebersberg

See also

Individual evidence