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Hinterreintalschrofen
The Hinterreintalschrofen is a 2,669 m high peak on the main, east–west oriented crest (the ''Teufelsgrat'' or "Devil's Ridge") of the Wetterstein Mountains in the Eastern Alps. It is a massive and dominant mountain with a high rock face that plunges into the Reintal valley to the north and stamps the appearance of the Wetterstein when seen from the north. In spite of that, the mountain is rarely climbed. Its neighbouring peaks are the ''Hochwanner'' (2,746 m) to the west and the ''Hundstallköpfe'' (2,533 m) to the east. The ''Teufelsgrat'' runs along the national border between the Austrian state of Tyrol, ( Gaistal) in the south and the German state of Bavaria, ( Reintal) in the north. First ascent The mountain was first climbed either on 1 September 1871 by Freiherr Hermann von Barth or, according to ''Stefan Beulke'',Alpenvereinsführer Wetterstein not until 1897 by A. Heinrich and F. Henning. Bases in the Gaistal valley *''Gaistalalm'' at 1356 m *''R ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hohe Munde
The Hohe Munde is a mountain at the eastern end of the Mieming Chain in the Austrian state of Tyrol. It has two peaks: the west top (2,662 m) and the east top or ''Mundekopf'' (2,592 m). Location The Hohe Munde rises north of the village of Telfs in the Inn valley. To the east is the Seefeld Plateau and the Leutasch village of ''Moos''. To the north it is separated from the Wetterstein Mountains by the valley of Gaistal. To the west, the Mieming Chain stretches away into the distance. Beyond the saddle of ''Niedere Munde'' (2,059 m) is the next peak in the chain, the 2,469 metre high Karkopf, followed by the 2,719 metre high Hochwand. Ascent The mountain may be climbed on an easy but strenuous tour from Moos via the Rauth Hut (1,605 m). The cable car from Moos to the Rauth Hut (the ''Mundelift'') is no longer working. On the eastern slopes of the Mundekopf extensive avalanche defences have been built to protect the village of Sagl. These were f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Tyrol (state)
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] |
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] |
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] |
Alpenvereinskarte
Alpine Club maps (german: Alpenvereinskarten, often abbreviated to ''AV-Karten'' i.e. AV maps) are specially detailed maps for summer and winter mountain climbers (mountaineers, hikers and ski tourers). They are predominantly published at a scale of 1:25.000, although some individual sheets have scales of 1:50.000 and 1:100.000. The cartographic library of the German (DAV) and Austrian Alpine Clubs (OeAV) currently has about 70 different high mountain maps. Also, individual map sheets of the Alpine region or other interesting mountain areas in the world are continually being published. The publication of its maps has been a function of the Alpine Club since 1865. The reason the two clubs still issue their maps is to complement the range of more or less good official maps of the high mountains with special large-scale maps. This is especially true for the Austrian Alpine region, which is the classical field for Alpine Club branches (sections). Here, there are no official maps at a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpenvereinsführer
The ''Alpine Club Guides'' (german: Alpenvereinsführer, commonly shortened to ''AV Führer'' or ''AVF'') are the standard series of Alpine guides that cover all the important mountain groups in the Eastern Alps. They are produced jointly by the German (DAV), Austrian (ÖAV) and South Tyrol Alpine Clubs (AVS). They have been published since 1950 by the firm of Bergverlag Rother in Munich, Germany. The AV guides contain all the routes – hiking trails, mountain hut approaches and summit climbs as well as ice and high mountain routes and ''klettersteigs'' in each mountain range. The descriptions are factual and dry, with few illustrations - rather unlike mountain books by e.g. Walter Pause – and despite introductory sections require general Alpine knowledge and experience. Examples are the ''AVF Allgäuer Alpen'' and the ''AVF Verwallgruppe''.The AV guides are often used as the basis for other publications and complement the Alpine Club maps or other map series. Available guid ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Climbing Grade
In rock climbing, mountaineering, and other climbing disciplines, climbers give a grade to a climbing route or boulder problem, intended to describe concisely the difficulty and danger of climbing it. Different types of climbing (such as sport climbing, bouldering or ice climbing) each have their own grading systems, and many nationalities developed their own, distinctive grading systems. There are a number of factors that contribute to the difficulty of a climb, including the technical difficulty of the moves, the strength, stamina and level of commitment required, and the difficulty of protecting the climber. Different grading systems consider these factors in different ways, so no two grading systems have an exact one-to-one correspondence. Climbing grades are inherently subjective.Reynolds Sagar, Heather, 2007, ''Climbing your best: training to maximize your performance'', Stackpole Books, UK, 9. They may be the opinion of one or a few climbers, often the first ascensi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dominance (geography)
The topographic isolation of a summit is the minimum distance to a point of equal elevation, representing a radius of dominance in which the peak is the highest point. It can be calculated for small hills and islands as well as for major mountain peaks and can even be calculated for submarine summits. Isolation table The following sortable table lists Earth's 40 most topographically isolated summits. Examples *The nearest peak to Germany's highest mountain, the 2,962-metre-high Zugspitze, that has a 2962-metre-contour is the Zwölferkogel (2,988 m) in Austria's Stubai Alps. The distance between the Zugspitze and this contour is 25.8 km; the Zugspitze is thus the highest peak for a radius of 25.8 km around. Its isolation is thus 25.8 km. *Because there are no higher mountains than Mount Everest, it has no definitive isolation. Many sources list its isolation as the circumference of the earth over the poles or – questionably, because there is no agreed de ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 |
Eastern Alps
Eastern Alps is the name given to the eastern half of the Alps, usually defined as the area east of a line from Lake Constance and the Alpine Rhine valley up to the Splügen Pass at the Alpine divide and down the Liro River to Lake Como in the south. The peaks and mountain passes are lower than the Western Alps, while the range itself is broader and less arched. Geography Overview The Eastern Alps include the eastern parts of Switzerland (mainly Graubünden), all of Liechtenstein, and most of Austria from Vorarlberg to the east, as well as parts of extreme Southern Germany (Upper Bavaria), northwestern Italy (Lombardy), northeastern Italy (Trentino-Alto Adige/Südtirol, Veneto and Friuli-Venezia Giulia) and a good portion of northern Slovenia (Upper Carniola and Lower Styria). In the south the range is bound by the Italian Padan Plain; in the north the valley of the Danube River separates it from the Bohemian Massif. The easternmost spur is formed by the Vienna Woods range, wi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
