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Stümpfling
The Stümpfling is a mountain, 1,506 metres high, in the Bavarian Prealps. The mountain is an easy mountain walk from the Spitzingsee Spitzingsee is a lake in Bavaria, Germany. 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 ... 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mangfall Mountains
The Mangfall Mountains (german: Mangfallgebirge), 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 (Tegernsee), Rottach, Weißach (Tegernsee), 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 (lake), Tegernsee−Rottach (Tegernsee), Rottach−Weiße Valepp), Schliersee Mountains (to the Leitzach valley) and the Wende ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bavaria
Bavaria ( ; ), officially the Free State of Bavaria (german: Freistaat Bayern, link=no ), is a state in the south-east of Germany. With an area of , Bavaria is the largest German state by land area, comprising roughly a fifth of the total land area of Germany. With over 13 million inhabitants, it is second in population only to North Rhine-Westphalia, but due to its large size its population density is below the German average. Bavaria's main cities are Munich (its capital and largest city and also the third largest city in Germany), Nuremberg, and Augsburg. The history of Bavaria includes its earliest settlement by Iron Age Celtic tribes, followed by the conquests of the Roman Empire in the 1st century BC, when the territory was incorporated into the provinces of Raetia and Noricum. It became the Duchy of Bavaria (a stem duchy) in the 6th century AD following the collapse of the Western Roman Empire. It was later incorporated into the Holy Roman Empire, became an ind ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bavarian Prealps
The Bavarian Prealps (german: Bayerische Voralpen) are a mountain range within the Northern Limestone Alps in south Germany. They include the Bavarian Prealp region between the river Loisach to the west and the river Inn to the east; the range is about long and wide. The term is not defined politically, but alpine-geographically because small areas of the Bavarian Prealps lie in Tyrol (e.g. the Hinteres Sonnwendjoch south of the Rotwand). 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 prominent limestone cliffs. Extent According to the 1984 classification of the Eastern Alps by the German Alpine Club the Bavarian Prealps a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spitzingsee
Spitzingsee is a lake in Bavaria, Germany. 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. auf der Website der Bay. Schlösserverwaltung . Footnotes See also * |
Mountains Of The Alps
This page tabulates only the most prominent mountains of the Alps, selected for having a topographic prominence of ''at least'' , and all of them 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 either France, Italy, Switzerland, Liechtenstein, Austria, Germany or Slovenia, even in some lower regions. Together, these three 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 the highest peaks of the Alps, as identified by the International Climbing and Mountaineering Federation (UIAA), and often referred to as the 'Alpi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 300 metres (1,000 feet) 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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