Taubenberg is a mountain with a height of 896 m

amsl Height above mean sea level is a measure of a location's vertical distance (height, elevation or altitude) in reference to a vertical datum based on a historic mean sea level. In geodesy, it is formalized as orthometric height. The zero level v ...

and area of 1847 haWalentowski, Fischer 2006, S. 24. in the Warngau municipality in the district of

Miesbach Miesbach () is a Town#Germany, town in Bavaria, Germany, and is the capital of the Miesbach (district), Miesbach district. The district is at an altitude of 697 metres above sea level. It covers an area of approximately 863.50 km2 of alpine ...

Bavaria Bavaria, officially the Free State of Bavaria, is a States of Germany, state in the southeast of Germany. With an area of , it is the list of German states by area, largest German state by land area, comprising approximately 1/5 of the total l ...

Germany Germany, officially the Federal Republic of Germany, is a country in Central Europe. It lies between the Baltic Sea and the North Sea to the north and the Alps to the south. Its sixteen States of Germany, constituent states have a total popu ...

. It is set apart from the

Tegernsee Tegernsee () is a Town#Germany, town in the Miesbach (district), Miesbach district of Bavaria, Germany. It is located on the banks of Tegernsee (lake), Lake Tegernsee, which is 747 m (2,451 ft) AMSL, above sea level. A spa town, it is su ...

mountains of the

Bavarian Prealps The Bavarian Prealps () are a mountain range within the Northern Limestone Alps along the Austria–Germany border. They include the Bavarian Prealp region between the river Loisach to the west and the river Inn River, Inn to the east; the range is ...

. It is a popular hiking destination and the most important water supply area of the Bavarian capital Munich. About two-thirds of the mountain is owned by the city of Munich, the rest is freehold of local farmers and foresters.

Geography

Geologically Taubenberg belongs to the

Molasse __NOTOC__ In geology, "molasse" () are sandstones, shales and conglomerates that form as terrestrial or shallow marine deposits in front of rising mountain chains. The molasse deposits accumulate in a foreland basin, especially on top of flys ...

foothillsWalentowski, Fischer 2006, Seite 10 ff. with its characteristic east–west orientation and marks (as ,for example, the Hoher Peißenberg ) the northern edge of the Subalpine Molasse(German) in the Bavarian Alpine foothills and thus the geological edge of the Alps. Taubenberg is the result of debris flows of the upper freshwater molasses, which came from the south about 10-15 million years ago - when the Alps were formed. These coarse debris cones now form characteristic mountains in front of the exits of the former tertiary Alpine rivers ( Tischberg, Hoher Peißenberg,

Irschenberg Irschenberg is a municipality in the district of Miesbach in the German state of Bavaria, about southeast of Munich. It consists of numerous hamlets situated on the ''Irschenberg'' hill range. The hill is a notorious ascent of the Bundesautobah ...

and others). Through the ice of later glaciations ,they were later left as

Butte In geomorphology, a butte ( ) is an isolated hill with steep, often vertical sides and a small, relatively flat top; buttes are smaller landforms than mesas, plateaus, and table (landform), tablelands. The word ''butte'' comes from the French l ...

s from their softer environment of fine sands and acted as icebreakers, separating the ice flows of individual glacier termini. The distribution of

Glacial erratic A glacial erratic is a glacially deposited rock (geology), rock differing from the type of country rock (geology), rock native to the area in which it rests. Erratics, which take their name from the Latin word ' ("to wander"), are carried by gla ...

s and the

soil horizon A soil horizon is a layer parallel to the soil surface whose physical, chemical and biological characteristics differ from the layers above and beneath. Horizons are defined in many cases by obvious physical features, mainly colour and texture. ...

s in the summit area of the Taubenberg suggest that it was not overshadowed by glaciers in the last, the

Würm glaciation The Würm glaciation or Würm stage ( or ''Würm-Glazial'', colloquially often also ''Würmeiszeit'' or ''Würmzeit''; cf. ice age), usually referred to in the literature as the Würm (often spelled "Wurm"), was the last glacial period in the ...

, but emerged from the ice as

Nunatak A nunatak (from Inuit language, Inuit ) is the summit or ridge of a mountain that protrudes from an ice field or glacier that otherwise covers most of the mountain or ridge. They often form natural pyramidal peaks. Isolated nunataks are also cal ...

. Taubenberg has a peculiar

geomorphology Geomorphology () is the scientific study of the origin and evolution of topographic and bathymetric features generated by physical, chemical or biological processes operating at or near Earth's surface. Geomorphologists seek to understand wh ...

. The highest point is in the west of the ridge. From there, the small Farnbach(German) flows in a valley in the center of the terrain structure to the east and the

Mangfall The Mangfall () is a river of Upper Bavaria, Germany. It is a left tributary of the Inn. The Mangfall is the outflow of the Tegernsee lake and discharges into the Inn in Rosenheim. The Mangfall is long. Towns and villages on the Mangfall * G ...

, in which it flows. The valley of the Farnbach divides Taubenberg into a northern and a southern ridge, which are connected to each other in the west. The northern ridge is higher, in its east is the second highest point of the mountain. The southern ridge drops almost equally from west to east. In front of it is the Steinbachtal(German), a broad sloping hollow with fen.

References

Mountains of Bavaria Mountains of the Alps {{Bavaria-geo-stub