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The Mangfall Mountains (,), or sometimes Mangfall Alps, are the easternmost part 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 ...
that, in turn, belong to the
Northern Limestone Alps The Northern Limestone Alps (), also called the Northern Calcareous Alps, are the ranges of the Eastern Alps north of the Central Eastern Alps located in Austria and the adjacent Bavarian lands of southeastern Germany. The distinction from the ...
. The name comes from the river
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 ...
, whose tributaries, the Rottach, Weißach, Schlierach and Leitzach, drain large parts of the area and form an important drinking water reservoir for the city of
Munich Munich is the capital and most populous city of Bavaria, Germany. As of 30 November 2024, its population was 1,604,384, making it the third-largest city in Germany after Berlin and Hamburg. Munich is the largest city in Germany that is no ...
.


Geography


Location

The mountain region is bounded by the
Isar The Isar () is a river in Austria and in Bavaria, Germany. Its source is in the Karwendel mountain range of the Alps. The Isar river enters Germany near Mittenwald and flows through Krün, Wallgau, Bad Tölz, Munich, and Landshut before reaching ...
valley in the west, the
Inn valley The Inn (; ; ) is a river in Switzerland, Austria and Germany. The long river is a right tributary of the Danube, being the third largest tributary of the Danube by discharge. The highest point of its drainage basin is the summit of Piz Bernin ...
in the east, the
Brandenberg Alps The Brandenberg Alps () are a sub-group of the Northern Limestone Alps, that run in front of the Eastern Alps for their whole length. They lie entirely in Austria between Achensee in Tyrol (state), Tyrol, the Inn Valley and the Bavarian Prealps. ...
(the Rofan) and the Austrian state border in the south. North of the Mangfalls lies the
Alpine Foreland The Alpine Foreland, less commonly called the Bavarian Foreland,Dickinson, Robert E (1964). ''Germany: A regional and economic geography'' (2nd ed.). London: Methuen, pp. 585-586. . Bavarian Plateau or Bavarian Alpine Foreland (), refers to a tria ...
. The region has an area of 752.40 km2 or, by narrower definitions, only 333 km2. The Mangfall Mountains are divided into the
Tegernsee Mountains The Tegernsee Mountains () form a mountain region between the River Isar in the west and the lake of Tegernsee as well as the Rottach, Weißen Valepp and Grundache south of the Tegernsee, in the east, and so form a part of the Bavarian Prealps. T ...
(from the Isar to the line
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 ...
Rottach−Weiße Valepp), Schliersee Mountains (to the Leitzach valley) and the Wendelstein Group (between the Leitzach glacial valley and the
Inn Inns are generally establishments or buildings where travelers can seek lodging, and usually, food and drink. Inns are typically located in the country or along a highway. Before the advent of motorized transportation, they also provided accomm ...
valley).


Peaks

The highest peak in the Mangfalls is the Rotwand at , one of the most popular local mountains for Munich's citizens at all times of the year. The Wendelstein lies a few kilometres further northeast of the Rotwand, but is separated from it by a valley. Another popular destination is the Brünnstein. These and the other main peaks in the Mangfall Mountains are (sorted by height in metres (m) above ''
Normalnull ("standard zero") or (short N. N. or NN) is an outdated official vertical datum used in Germany. Elevations using this reference system were to be marked (“meters above standard zero”). has been replaced by (NHN). History In 187 ...
'' (NN): * Rotwand (1.884 m), Miesbach district * Großer Traithen (1.852 m), Rosenheim district * Wendelstein (1.838 m), Rosenheim district * Risserkogel (1.826 m), Miesbach district * Schinder (1.808 m), Miesbach district * Ruchenköpfe (1.805 m), Miesbach district * Plankenstein (1.768 m), Miesbach district * Kaserwand (1.690 m), Rosenheim district * Brecherspitz (1.683 m), Miesbach district * Hochsalwand (1.625 m), Rosenheim district * Brünnstein (1.619 m), Rosenheim district * Seebergkopf (1.538 m), Rosenheim district * Großer Riesenkopf (1.337 m) *
Madron Madron ( (village) or (parish)) is a civil parishes in England, civil parish and village in west Cornwall, England, United Kingdom. Madron is named after Saint Madern's Church. Its annual Trafalgar Service commemorating the death of Horatio ...
(942 m), Rosenheim district *
Petersberg Petersberg may refer to: * The Hotel Petersberg near Bonn, the site of the ** Petersberg Agreement, 1949, regarding the international status of West Germany. ** Petersberg tasks, 1992 and 1997, regarding European security cooperation. Also known as ...
(847 m), Rosenheim district


Lakes

Like the Alps as a whole, the Mangfall Mountains were heavily affected by the last ice age (
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 ...
). For example, lakes like 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 ...
, and the typical
U-shaped valley U-shaped valleys, also called trough valleys or glacial troughs, are formed by the process of Glacial period, glaciation. They are characteristic of mountain glaciation in particular. They have a characteristic U shape in cross-section, with s ...
s were formed by glaciers.


References


External links

{{Authority control Miesbach (district) Bavarian Prealps Mountain ranges of Bavaria