Reintal (Wetterstein)
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Reintal (Wetterstein)
The Reintal ("Rein Valley") is the name given to the upper and lower valleys of the River Partnach between the ''Zugspitzplatt'' plateau and the Partnachklamm gorge. A hiking route to Germany's highest mountain, the Zugspitze runs through the valley. The valley was formed during the Würm Ice Age by the Reintal Glacier and then deepened by the Partnach in the post-ice age period after the retreat of the glacier to the periphery of the Schneefernerkopf mountain. The upper Reintal, which was shaped by the glacier and today forms a U-shaped glacial valley, ends between the ''Hohe Gaifkopf'' in the west and the Schachen in the east. The lower Reintal lies in the area of the former glacial lake of the Loisach Glacier, into which the Reintal Glacier flowed from the southwest. It is a V-shaped valley and has been predominantly shaped by the Partnach river. Together with the Höllental valley to the north, the Reintal divides the Wetterstein Mountains into several ridges. The north ...
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Hochwanner
__NOTOC__ At , the Hochwanner (formerly: ''Kothbachspitze'') is the second highest mountain in Germany
at en.tixik.com. Accessed on 10 Feb 2010. after the (if the somewhat higher is only considered as a sub-peak of the Zugspitze). In addition the Hochwanner is the highest peak on the main ridge of the (''Wettersteinhauptkamm'') running from ''Gatterl'' to the Upper Wettersteinspitze (''Oberen Wettersteinspitze'') above

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Valleys Of Bavaria
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ...
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Nature Reserve
A nature reserve (also known as a wildlife refuge, wildlife sanctuary, biosphere reserve or bioreserve, natural or nature preserve, or nature conservation area) is a protected area of importance for flora, fauna, or features of geological or other special interest, which is reserved and managed for purposes of conservation and to provide special opportunities for study or research. They may be designated by government institutions in some countries, or by private landowners, such as charities and research institutions. Nature reserves fall into different IUCN categories depending on the level of protection afforded by local laws. Normally it is more strictly protected than a nature park. Various jurisdictions may use other terminology, such as ecological protection area or private protected area in legislation and in official titles of the reserves. History Cultural practices that roughly equate to the establishment and maintenance of reserved areas for animals date bac ...
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Bavarian Alps
The Bavarian Alps (german: Bayerische Alpen) is a collective name for several mountain ranges of the Northern Limestone Alps within the German state of Bavaria. Geography The term in its wider sense refers to that part of the Eastern Alps that lies on Bavarian state territory. However, it is traditionally understood that the Bavarian Alps are only those ranges between the rivers Lech and Saalach ('' Altbayern''). In this narrower sense, the Allgäu Alps in Swabia, which have only been part of Bavaria in more recent times, and the Berchtesgaden Alps in the east are not considered part of the Bavarian Alps. The term is frequently used, but does not correspond to the common classification of the Eastern Alps (AVE) developed by the German, Austrian and South Tyrol Alpine Clubs. It should not be confused with the term Bavarian Prealps either. The latter only covers the Bavarian section of the Prealps between the River Loisach in the west and the River Inn in the east. According t ...
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Berchtesgadener Land
Berchtesgadener Land (Central Bavarian: ''Berchtsgoana Land'') is a ''Landkreis'' (district) in Bavaria, Germany. It is bounded by the district of Traunstein and by the state of Austria. History Middle ages and early modern era The southern alpine regions were part of the stem duchy of Bavaria from the early Middle Ages. The 11th and 12th centuries saw the founding of numerous mountain villages. One of these settlements was Berchtesgaden, which later assumed a more dominant role in the administrative district that now bears its name. The northern portion of the Salzach river valley was traditionally part of the Prince-Archbishopric of Salzburg (an imperial principality ruled by the archbishop of Salzburg), while Berchtesgaden itself was the seat of the Berchtesgaden Provostry (a principality ruled by a Prince-Provost) comprising roughly the modern municipalities of Berchtesgaden, Bischofswiesen, Marktschellenberg, Ramsau and Schönau am Königssee. These states existed fr ...
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Reintalanger Hut
The Reintalanger Hut (1,366 m) is an Alpine Club hut in the Wetterstein Mountains at the head of the Reintal valley. The River Partnach has its source in the vicinity. West of the hut the valley floor climbs steeply up to the plateau of the ''Zugspitzplatt'' below Germany's highest mountain. The hut belongs to the Munich section of the German Alpine Club and the administrative district of Garmisch-Partenkirchen. It was built in 1912''Reintalangerhütte 1369 m''
at www.alpenverein-muenchen-oberland.de. Retrieved 30 Mar 2018.
and is a Category 1 hut. The house has 132 bedspaces and is managed from the end of May to mid-October.


History

The use of the pasture of the Reintalangeralm is discernible as early as 1485. It was often used by Tyrolese subjects ...
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Via Alpina
The Via Alpina is a network of five long-distance hiking trails across the alpine regions of Slovenia, Austria, Germany, Liechtenstein, Switzerland, Italy, France, and Monaco. The longest of trails is the red trail, whose termini are in Trieste and Monaco. The Via Alpina was created by a group of public and private organisations from the 8 Alpine countries in 2000, receiving EU funding from 2001 until 2008. It was initiated by the Association Grande Traversée des Alpes in Grenoble, which hosted the Via Alpina international secretariat until January 2014, when it was transferred to the International Commission for the Protection of the Alps CIPRA (Liechtenstein). There are national secretariats (hosted by public administrations or hiking associations) in each country. Its aim is to support sustainable development in remote mountain areas and promote the Alpine cultures and cultural exchanges. Purple trail * A1: From Tržaška koča na Doliču to Aljažev dom v Vratih. * A2: ...
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Knorr Hut
The Knorr Hut is a mountain hut belonging to the German Alpine Club and located in the Wetterstein Mountains at a height of 2,052 m. Its lies right on the edge of the ''Zugspitzplatt'' where it drops into the Reintalanger in a location with scenic views and is an important base for hikers who can climb up to it on the normal route from the town of Garmisch-Partenkirchen through the Reintal valley to Germany's highest mountain, the Zugspitze. The Knorr Hut is rated as category I, and belongs to the Munich Section of the German Alpine Club (DAV). History The Knorr Hut was built by 1855 as a small, rude refuge hut, the merchant, Angelo Knorr, contributing ''"a significant sum of money"'' towards it. By 1860 the hut had become run down, because ''"the maintenance of the same had been paid little attention"''. Finally the Munich Section of the newly founded German Alpine Club took over the hut. As well as the section itself, ''"the Royal District Office of Werdenfels, as well a ...
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Rockslide
A rockslide is a type of landslide caused by rock failure in which part of the bedding plane of failure passes through compacted rock and material collapses ''en masse'' and not in individual blocks. Note that a rockslide is similar to an avalanche because they are both slides of debris that can bury a piece of land. While a landslide occurs when loose dirt or sediment falls down a slope, a rockslide occurs only when solid rocks are transported down slope. The rocks tumble downhill, loosening other rocks on their way and smashing everything in their path. Fast-flowing rock slides or debris slides behave similarly to snow avalanches, and are often referred to as rock avalanches or debris avalanches. Definition The term landslide refers to a variety of mass wasting events (geologic slope failures) that include slumps, slides, falls, and flows. The two major types of slides are rotational slides and translational slides. Rockslides are a type of translational event since the rock ...
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