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 Partnach is an 18 km (11 mi) long mountain river in Bavaria, Germany.
The Zugspitze, at 2,962 m (9,718 ft) above sea level, is the highest peak of the Wetterstein Mountains as well as the highest mountain in Germany. It lies south of the town of Garmisch-Partenkirchen, and the Austria–Germany border runs over its western summit. South of the mountain is the Zugspitzplatt, a high karst plateau with numerous caves. On the flanks of the Zugspitze are three glaciers, including the two largest in Germany: the Northern Schneeferner with an area of 30.7 hectares and the Höllentalferner with an area of 24.7 hectares. The third is the Southern Schneeferner which covers 8.4 hectares.
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.
The Schneefernerkopf is a 2,875-metre-high (9,432 ft) peak in the Zugspitze massif in the Alps. It lies at the western end of the Wetterstein chain in the Alps on the border between the German state of Bavaria and the Austrian state of Tyrol. It is the dominant mountain in the Wetterstein, especially when viewed from Ehrwald.
Together with the Höllental valley to the north, the Reintal divides the Wetterstein Mountains into several ridges. The northern periphery is formed by the arêtes of the Höllentalspitzen (2,743 m) and the Hohe Gaifkopf (1,864 m). The highest points on the southern flank of the valley lie on the Hochwanner (2,744 m), the Hinterreintalschrofen (2,670 m) and the Dreitorspitze (2,682 m). The valley floor lies at elevations between 1400 m above NN at the source of the Partnach river, 1,002 m at the entrance to the gorge of the Hinteren Klamm and 797 m at the start of the Partnachklamm gorge, in the upper Reintal therefore about 1300 to 850 m above the surrounding mountain peaks. [?] In the upper Reintal the rubble from rockslides from the southern faces of the Hochwanner and Hinterreintalschrofen also play a rôle in the shaping of the valley. These have spilled into the old glacial valley, forced back the course of the Partnach to the north and, in places, impounding it.
The Höllental, English translation "Hell Valley" or "Valley of Hell" is one of the routes on the German side leading up the Zugspitze on the German-Austrian border in the northern Alps. It is located in the district of Garmisch-Partenkirchen.
An arête is a narrow ridge of rock which separates two valleys. It is typically formed when two glaciers erode parallel U-shaped valleys. Arêtes can also form when two glacial cirques erode headwards towards one another, although frequently this results in a saddle-shaped pass, called a col. The edge is then sharpened by freeze-thaw weathering, and the slope on either side of the arete steepened through mass wasting events and the erosion of exposed, unstable rock. The word ‘arête’ is actually French for edge or ridge; similar features in the Alps are described with the German equivalent term Grat.
The Höllentalspitzen are three peaks in the Wetterstein Mountains near Garmisch-Partenkirchen in southern Germany. They rise from the ridge of Blassenkamm which runs eastwards from Germany's highest peak, the Zugspitze, and separate the Hölle Valley to the north from the Reintal Valley to the south. The summit nearest to the Zugspitze is the Inner Höllentalspitze, 2,741 metres (8,993 ft) high; this is followed by the main summit Middle Höllentalspitze, 2,743 metres (8,999 ft) high; and the Outer Höllentalspitze at 2,720 metres (8,920 ft).
Around 1800 rockslides created two small lakes, the Vordere Blaue Gumpe and Hintere Blaue Gumpe . On 23 August 2005 the former was completely filled with sediment as a result of heavy rain (200mm in 24h) whereupon high pressure broke the natural dam. The resulting deluge of flood water caused considerable damage further down the valley. [1] [2]
A moderately steep climbing path to the Zugspitze runs through the Reintal, the section as far as the Knorr Hut forming part of the Red Trail of the Via Alpina. The mountain huts in the valley, the Bock Hut and Reintalanger Hut, are used by hikers and climbers as bases for numerous tours.
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 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 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.
Due to its great distance from any settlements and because no roads runs up the valley the Reintal is very unspoilt and still very natural, despite being easily accessible on foot. Together with the Wimbachtal in the Berchtesgadener Land it may be considered as one of the most impressive, large, near-natural valley landscapes in the Bavarian Alps. The upper Reintal is protected as a nature reserve.
Berchtesgadener Land is a Landkreis (district) in Bavaria, Germany. It is bounded by the district of Traunstein and by the state of Austria.
Bavarian Alps is a summarizing term of several mountain ranges of the Northern Limestone Alps in the German state of Bavaria.
A nature reserve is a protected area of importance for flora, fauna or features of geological or other special interest, which is reserved and managed for conservation and to provide special opportunities for study or research. Nature reserves may be designated by government institutions in some countries, or by private landowners, such as charities and research institutions, regardless of nationality. 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.
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Garmisch-Partenkirchen is a Landkreis (district) in Bavaria, Germany. It is bounded by the districts of Ostallgäu, Weilheim-Schongau and Bad Tölz-Wolfratshausen, and by the Austrian state of Tyrol.
The Tux Alps or Tux Prealps are a sub-group of the Austrian Central Alps, which in turn form part of the Eastern Alps within Central Europe. They are located entirely within the Austrian federal state of Tyrol. The Tux Alps are one of three mountain ranges that form an Alpine backdrop to the city of Innsbruck. Their highest peak is the Lizumer Reckner, 2,886 m (AA), which rises between the glen of Wattentaler Lizum and the valley of the Navisbach. Their name is derived from the village of Tux which is tucked away in a side valley of the Zillertal.
The Ester Mountains are a small mountain range in Bavaria. They are classified either as part of Bavarian Prealps or the larger chain of Northern Limestone Alps. The range stretches for about 15 kilometres. From the west it is bordered by the valley of the river Loisach and from the east by Walchensee lake and the valley of the river Isar. With its highest peak being Krottenkopf, the highest part of the range just exceeds 2,000 m. The range is of composed of limestone. The treeline is around 1,700 m.
U-shaped valleys, trough valleys or glacial troughs, are formed by the process of glaciation. They are characteristic of mountain glaciation in particular. They have a characteristic U shape, with steep, straight sides and a flat or rounded bottom. Glaciated valleys are formed when a glacier travels across and down a slope, carving the valley by the action of scouring. When the ice recedes or thaws, the valley remains, often littered with small boulders that were transported within the ice, called glacial till or glacial erratic.
Lake Sils is a lake in the Upper Engadine valley, Grisons, Switzerland. It takes its name from the village of Sils im Engadin. The lake lies at an altitude of 1,797 metres above sea level, between Maloja Pass and Lake Silvaplana. Several mountains over 3,000 metres overlook the lake, notably Piz Corvatsch, Piz Grevasalvas and Piz da la Margna. The lake's drainage basin culminates at Piz Fora and comprises the Vadrec da Fedoz glacier.
The Allgäu Alps are a mountain range in the Northern Limestone Alps, located in Bavaria in Germany and Tyrol and Vorarlberg in Austria. The range lies directly east of Lake Constance.
The Wetterstein mountains, colloquially called Wetterstein, is a mountain group in the Northern Limestone Alps within the Eastern Alps. It is a comparatively compact range located between Garmisch-Partenkirchen, Mittenwald, Seefeld in Tirol and Ehrwald along the border between Germany (Bavaria) and Austria (Tyrol). Zugspitze, the highest peak is at the same time the highest mountain in Germany.
At 2,744 metres (9,003 ft), the Hochwanner is the second highest mountain in Germany after the Zugspitze. In addition the Hochwanner is the highest peak on the main ridge of the Wetterstein (Wettersteinhauptkamm) running from Gatterl to the Upper Wettersteinspitze above Mittenwald in an east-west direction. From the Hochwanner massif there is an all-round view of the Rein valley (Reintal), the Leutasch valley in Austria, the Gais valley, the Zugspitze, the Mieming Chain, the Jubiläumsgrat, the Karwendel mountains and far into the central Alps.
At 2,606.9 metres (8,553 ft), the Hochkalter in the Berchtesgaden Alps is the highest peak in the massif of the same name and therefore one of the highest mountains in Germany. The Hochkalter Massif is also called the Hochkalter mountains.
The Ammergau Alps are a mountain range in the Northern Limestone Alps in the states of Bavaria (Germany) and Tyrol (Austria). They cover an area of about 30 x 30 km and begin at the outer edge of the Alps. The highest summit is the Daniel which has a height of 2,340 metres (7,680 ft).
The Mieming(er) Range, Mieminger Chain or Mieminger Mountains, is a mountain range of the Northern Limestone Alps in the Eastern Alps. It is located entirely in Austria within the state of Tyrol. This sub-group is somewhat in the shadows of its more famous neighbour, the Wetterstein to the north. Whilst the region around the Coburger Hut and the lakes of Seebensee and Drachensee in the west and the Hohe Munde in the extreme east receive large numbers of visitors, the less developed central area remains very quiet. The Hohe Munde is also a popular and challenging ski touring destination.
The Partnach Gorge is a deep gorge that has been incised by a mountain stream, the Partnach, in the Reintal valley near the south German town of Garmisch-Partenkirchen. The gorge is 702 metres (2,303 ft) long and, in places, over 80 metres (260 ft) deep. It was designated a natural monument in 1912.