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Olperer
The Olperer is a mountain in the Zillertal Alps in the Austrian federal state of Tyrol. It is the main summit on the Tux Crest (''Tuxer Kamm'') and is often crossed in the summer as climbers transit from the Olperer Hut to the Geraer Hut. It was first climbed on 10 September 1867 along the southeast ridge (''Südostgrat'') by Paul Grohmann, Georg Samer and Gainer Jackl. On its north flank is the ski region known as Hintertux Glacier on the ''Gefrorene-Wand-Kees'' glacier (also called the ''Tuxer Ferner''). Location and area The Olperer, with its pyramidal summit block, presents a striking appearance. As a result of that and because of its geographical prominence over its nearby peaks, the summit is a popular viewing point. It lies about four kilometres as the crow flies northwest of the Schlegeisspeicher dam and seven kilometres south of Hintertux. Its neighbours are, to the north and separated by the ''Wildlahnerscharte'' (3,220 m), the Großer Kaserer at 3,266 metres, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Olperer 2007-11-27
The Olperer is a mountain in the Zillertal Alps in the Austrian federal state of Tyrol. It is the main summit on the Tux Crest (''Tuxer Kamm'') and is often crossed in the summer as climbers transit from the Olperer Hut to the Geraer Hut. It was first climbed on 10 September 1867 along the southeast ridge (''Südostgrat'') by Paul Grohmann, Georg Samer and Gainer Jackl. On its north flank is the ski region known as Hintertux Glacier on the ''Gefrorene-Wand-Kees'' glacier (also called the ''Tuxer Ferner''). Location and area The Olperer, with its pyramidal summit block, presents a striking appearance. As a result of that and because of its geographical prominence over its nearby peaks, the summit is a popular viewing point. It lies about four kilometres as the crow flies northwest of the Schlegeisspeicher dam and seven kilometres south of Hintertux. Its neighbours are, to the north and separated by the ''Wildlahnerscharte'' (3,220 m), the Großer Kaserer at 3,266 metres, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Olperer Hut
The Olperer is a mountain in the Zillertal Alps in the Austrian federal state of Tyrol. It is the main summit on the Tux Crest (''Tuxer Kamm'') and is often crossed in the summer as climbers transit from the Olperer Hut to the Geraer Hut. It was first climbed on 10 September 1867 along the southeast ridge (''Südostgrat'') by Paul Grohmann, Georg Samer and Gainer Jackl. On its north flank is the ski region known as Hintertux Glacier on the ''Gefrorene-Wand-Kees'' glacier (also called the ''Tuxer Ferner''). Location and area The Olperer, with its pyramidal summit block, presents a striking appearance. As a result of that and because of its geographical prominence over its nearby peaks, the summit is a popular viewing point. It lies about four kilometres as the crow flies northwest of the Schlegeisspeicher dam and seven kilometres south of Hintertux. Its neighbours are, to the north and separated by the ''Wildlahnerscharte'' (3,220 m), the Großer Kaserer at 3,266 metres, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains Of The Alps Above 3000 M
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] |
Paul Grohmann
Paul Grohmann (12 June 1838 – 29 July 1908) was an Austrian mountaineer and writer. Biography Grohmann was a pioneer in exploring technically challenging mountains and is thought to have made more first ascents of Eastern Alps summits than anyone else. Among these are the four highest summits in the Dolomites. In 1862, Grohman, Friedrich Simony and Edmund von Mojsvár founded the Austrian Alpine Club. This was the second mountaineering club in the world, following the founding of the British Alpine Club in 1857. In 1875, he published a detailed map of the Dolomites (''Karte der Dolomit-Alpen'') and, in 1877, the travel book ''Wanderungen in den Dolomiten'', which significantly stimulated mountain tourism in the area. In his honor, the as yet unclimbed ''Sasso di Levante'' in the Langkofel Dolomites was renamed Grohmannspitze in 1875. The west peak of the Kellerspitzen in the Carnic Alps, which he first-ascended in 1868, is also known as Grohmannspitze. Already in 1898, 10 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zillertal Alps
The Zillertal Alps ( it, Alpi Aurine; german: Zillertaler Alpen) are a mountain range of the Central Eastern Alps on the border of Austria and Italy. Name The range is named after the Zillertal (Ziller river valley) on its north. Geography The range is bounded by the ''Tuxerjoch'' mountain pass to the north (separating it from the Tux Alps); the ''Birnlücke'' - ''Forcella del Picco'' pass to the east (separating it from the Hohe Tauern); the Eisack and its tributary the Rienz to the south (separating it from the Southern Limestone Alps); and the Brenner Pass to the west (separating it from the Stubai Alps). Sub-groups The Zillertal Alps are divided into the following sub-groups: * Tux main ridge (''Tuxer Hauptkamm'') * Zillertal main ridge (''Zillertaler Hauptkamm'') and side ridgesThis is further sub-divided as follows: Hauptkamm, Hochstellerkamm, Greinerkamm, Mörchen and Igentkamm, Floitenkamm, Ahornkamm, Riblerkamm, Magnerkamm. * Reichenspitze Group and eastern Ziller ri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gefrorene-Wand-Spitzen
The Gefrorene-Wand-Spitzen are two summits on the Tux Crest (''Tuxer Kamm''), a mountain chain in the Zillertal Alps, one of the ranges of the central Eastern Alps in the Austrian state of Tyrol. The north summit (''Nordgipfel'') is recorded as 3,286 metres high in the literature, but is 3,288 metres high according to the Federal Office for Metrology and Survey. The south summit (''Südgipfel''), by contrast, is only 3,270 metres high. The two peaks are about 300 metres apart. They appear from the north as a stubby, cone-shaped, firn-covered dome, but from the east as a forbidding, dark rock face. Sharp, prominent ridges radiate from the peaks to the northeast and southwest, along the main crest of the mountain range. The twin peaks are the highest points in the summer skiing area of the Hintertux Glacier and, since the end of the 1990s, have been accessible from Hintertux on cable cars and ski lifts; which makes them a popular destination for day trippers. The north summit was fi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schwierigkeitsskala (Klettern)
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] |
Karl Diener
Karl may refer to: People * Karl (given name), including a list of people and characters with the name * Karl der Große, commonly known in English as Charlemagne * Karl Marx, German philosopher and political writer * Karl of Austria, last Austrian Emperor * Karl (footballer) (born 1993), Karl Cachoeira Della Vedova Júnior, Brazilian footballer In myth * Karl (mythology), in Norse mythology, a son of Rig and considered the progenitor of peasants (churl) * ''Karl'', giant in Icelandic myth, associated with Drangey island Vehicles * Opel Karl, a car * ST ''Karl'', Swedish tugboat requisitioned during the Second World War as ST ''Empire Henchman'' Other uses * Karl, Germany, municipality in Rhineland-Palatinate, Germany * ''Karl-Gerät'', AKA Mörser Karl, 600mm German mortar used in the Second World War * KARL project, an open source knowledge management system * Korean Amateur Radio League, a national non-profit organization for amateur radio enthusiasts in South Korea * KARL, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Firn
__NOTOC__ Firn (; from Swiss German "last year's", cognate with ''before'') is partially compacted névé, a type of snow that has been left over from past seasons and has been recrystallized into a substance denser than névé. It is ice that is at an intermediate stage between snow and glacial ice. Firn has the appearance of wet sugar, but has a hardness that makes it extremely resistant to shovelling. Its density generally ranges from 0.35 g/cm3 to 0.9 g/cm3, and it can often be found underneath the snow that accumulates at the head of a glacier. Snowflakes are compressed under the weight of the overlying snowpack. Individual crystals near the melting point are semiliquid and slick, allowing them to glide along other crystal planes and to fill in the spaces between them, increasing the ice's density. Where the crystals touch they bond together, squeezing the air between them to the surface or into bubbles. In the summer months, the crystal metamorphosis can occur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
