Stümpfling
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Stümpfling
The Stümpfling is a mountain, 1,506 metres high, in 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 .... The mountain is an easy mountain walk from the Spitzingsee lake or from the Wildbach Hut. The ''Suttenbahn'' and ''Stümpflingbahn'' lifts run up the mountain to just below the summit. External links Entry about the mountain tour {{DEFAULTSORT:Stumpfling One-thousanders of Germany Mountains of the Alps Mountains of Bavaria Bavarian Prealps ...
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Mangfall Mountains
The Mangfall Mountains (,), or sometimes Mangfall Alps, are the easternmost part of the Bavarian Prealps that, in turn, belong to the Northern Limestone Alps. The name comes from the river Mangfall, 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. Geography Location The mountain region is bounded by the Isar valley in the west, the Inn valley in the east, the Brandenberg Alps (the Rofan) and the Austrian state border in the south. North of the Mangfalls lies the Alpine Foreland. 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 (from the Isar to the line Tegernsee− Rottach−Weiße Valepp), Schliersee Mountains (to the Leitzach valley) and the Wendelstein Group (between the Leitzach glacial valley and the Inn valley). Peaks The highest pea ...
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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 land area of Germany, and with over 13.08 million inhabitants, it is the list of German states by population, second most populous German state, behind only North Rhine-Westphalia; however, due to its large land area, its population density is list of German states by population density, below the German average. Major cities include Munich (its capital and List of cities in Bavaria by population, largest city, which is also the list of cities in Germany by population, third largest city in Germany), Nuremberg, and Augsburg. The history of Bavaria includes its earliest settlement by Iron Age Celts, Celtic tribes, followed by the conquests of the Roman Empire in the 1st century BC, when the territory was incorporated into the provinces of Ra ...
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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 about long and wide. The term is not defined politically, but alpine-geographically because, although the range is mostly located in Bavaria, southeast Germany, small areas of the Bavarian Prealps lie in the states of Austria, state of Tyrol (state), Tyrol (e.g. the Hinteres Sonnwendjoch south of the Rotwand (Bavaria), Rotwand), Austria. The term is not to be confused with the Bavarian Alps or the Bavarian Alpine Foreland. These terms include the whole of the alpine region (together with parts of the Wetterstein, the Karwendel, etc.) and the whole Alpine Foreland on Bavarian state territory. Except in the Ester Mountains in the extreme west, the summits of the Bavarian Prealps are all below 2000 metres in height and only a few have pro ...
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Spitzingsee
Spitzingsee is a lake in Bavaria, 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 .... At an elevation of 1084 m, its surface area is . Geography The Spitzingsee is located about five kilometers south of the Schliersee and a few hundred meters south of the Spitzingsattels at an altitude of 1084 m in the Schliersee Mountains in the Bavarian Alps. With a surface area of , it is one of the largest mountain lakes in Bavaria. The lake's maximum depth is in the south basin, while the north basin's depth is up to . The Spitzingsee has a comparatively large water catchment area of . The lake is owned by the Free State of Bavaria; the Bavarian Administration of State-Owned Palaces, Gardens and Lakes is responsible for its administration.
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Mountains Of The Alps
This page tabulates only the most prominent mountains of the Alps, selected for having a topographic prominence of ''at least'' , all exceeding in height. Although the list contains 537 summits, some significant alpine mountains are necessarily excluded for failing to meet the stringent prominence criterion. The list of these most prominent mountains is continued down to 2500 m elevation at List of prominent mountains of the Alps (2500–2999 m) and down to 2000 m elevation on List of prominent mountains of the Alps (2000–2499 m). All such mountains are located in France, Italy, Switzerland, Liechtenstein, Austria, Germany or Slovenia, even in some lower regions. Together, these lists include all 44 ultra-prominent peaks of the Alps, with 19 ultras over 3000m on this page. For a definitive list of all 82 of the highest peaks of the Alps, as identified by the International Climbing and Mountaineering Federation (UIAA), and often referred to as the 'Alpine four-thousanders' ...
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Mountains Of Bavaria
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains ...
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