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Großer Geiger
The Großer Geiger, formerly also called the ''Obersulzbacher Venediger'' and ''Heiliggeistkogel'', is a mountain, , in the Venediger Group in the main chain of the Central Tauern (''Mittlerer Tauernhauptkamm''). This chain lies in the High Tauern, part of the Austrian Central Alps on the border between the Austrian states of Tyrol in the south and Salzburg in the north. The mountain was given its present name in 1855 by the Austrian chemist and cartographer, Franz Keil. Because of its isolated situation the Großer Geiger has a significant dominance. With its distinctive, symmetric, pyramidal shape and its mighty northwest face which rises 350 metres above the Obersulzbachkees glacier at a gradient of 50°, it is the most prominent landmark in the entire Upper Sulzbach valley. Arêtes radiate from the summit in all four directions of the compass. The mountain is easy to reach and is thus a popular touring and climbing destination. It was first climbed on 20 August 1871 by the A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Keeskogel (Venediger Group)
The Keeskogel, a mountain with a height of , lies in the Venediger Group of the High Tauern in Austria. The summit is located about 4 km as the crow flies northwest of the Großvenediger (). The waymarked, glacier-free normal route A normal route or normal way (french: voie normale; german: Normalweg) is the most frequently used route for ascending and descending a mountain peak. It is usually the simplest route. Overview In the Alps, routes are classed in the following way ... from the Kürsinger Hut (), is a relatively straightforward climb in dry and snow-free condition and takes about 1½ to 2 hours to reach the summit ( sure-footedness required). Especially impressive in good weather is the view from the summit of the north side of the Großvenediger and the main chain of the Tauern and the glaciated landscape of the ''Obersulzbachkees'' and ''Untersulzbachkees''. Literature and maps *Willi End/Hubert Peterka: Alpine Club Guide: ''Venedigergruppe''; Bergverlag Ru ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Climbing Route
A climbing route is a path by which a climber reaches the top of a mountain, rock, or ice wall. Routes can vary dramatically in difficulty and grade; once committed to that ascent, it can sometimes be difficult to stop or return. Choice of route can be critically important. Guidebooks, if available, are helpful in providing detailed diagrams and photographs of routes. In the earliest days of hillwalking and mountaineering, climbers got to the top by whatever means got them there. Little information about how they did it is available. During the 19th century, as explorers of the Alps tried ever harder summits, it became clear that choosing an eastern face over a southwestern ridge could spell the difference between success or failure. One example was the first ascent of the Matterhorn, which had been repeatedly and unsuccessfully attempted via the southern side. The strata there tended to slope down and away while the rocks of the northeastern ridge (the one closest to Ze ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Summit Cross
A summit cross (german: Gipfelkreuz) is a cross on the summit of a mountain or hill that marks the top. Often there will be a summit register (''Gipfelbuch'') at the cross, either in a container or at least a weatherproof case. Various other forms of marking or symbol such as cairns, prayer flags or ovoos may be found around the world on passes and hills, in particular on sacred mountains. In the Italian Alps a Madonna is sometimes placed at the summit instead of a cross. Summit crosses are normally about two to four metres high and are usually made of wood or metal. In April 2010, the world's first glass summit cross was erected on the ''Schartwand'' (2,339 m) in Salzburg's Tennengebirge mountains. Summit crosses are mainly found in Catholic regions of the Alps, especially in Austria, Switzerland and Bavaria, mountainous regions of Poland, but also in America. They usually stand on mountains whose summits are above the tree line, but they are also found in the German Central ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Normal Route
A normal route or normal way (french: voie normale; german: Normalweg) is the most frequently used route for ascending and descending a mountain peak. It is usually the simplest route. Overview In the Alps, routes are classed in the following ways, based on their waymarking, construction and upkeep: * Footpaths (''Fußwege'') *Hiking trails (''Wanderwege'') * Mountain trails (''Bergwege'') * Alpine routes (''Alpine Routen'') *Climbing routes (''Kletterrouten'') and High Alpine routes (''Hochalpine Routen'') in combined rock and ice terrain, (UIAA) graded by difficulty Sometimes the normal route is not the easiest ascent to the summit, but just the one that is most used. There may be technically easier variations. This is especially the case on the Watzmannfrau, the Hochkalter and also Mount Everest. There may be many reasons these easier options are less well-used: * the simplest route is less well known than the normal route (Watzmannfrau). * the technically easiest route is mor ... [...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] |
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] |
Crevasse
A crevasse is a deep crack, that forms in a glacier or ice sheet that can be a few inches across to over 40 feet. Crevasses form as a result of the movement and resulting stress associated with the shear stress generated when two semi-rigid pieces above a plastic substrate have different rates of movement. The resulting intensity of the shear stress causes a breakage along the faces. Description Crevasses often have vertical or near-vertical walls, which can then melt and create seracs, arches, and other ice formations. These walls sometimes expose layers that represent the glacier's stratigraphy. Crevasse size often depends upon the amount of liquid water present in the glacier. A crevasse may be as deep as 45 metres and as wide as 20 metres. by |
High Mountain Tour
A high mountain tour (german: Hochtour) is a mountaineering, mountain tour that takes place in the Altitudinal zonation, zone that is covered by ice all year round, the nival zone. High mountain tours require special preparation and equipment. Alpine ''Hochtour'' In the Alps a high mountain tour is known in the German-speaking areas as a ''Hochtour'' where, above a height of about 3,000 metres (High Alps), many mountains are at least partly glaciated. Important historic milestones in the development of high mountain touring in the Alps were the first ascents of the Ankogel (3,262 m) in 1762, Mont Blanc (4,810 m) in 1786, the Großglockner (3,798 m) in 1800 and the Ortler (3,905 m) in 1804 as well as the conquest of many high Western Alps, western Alpine summits during the golden age of Alpinism around the middle of the 19th century. In other parts of the world the term may be misleading. For example, in many non-Alpine areas, such as the polar regions, much l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Großer Geiger
The Großer Geiger, formerly also called the ''Obersulzbacher Venediger'' and ''Heiliggeistkogel'', is a mountain, , in the Venediger Group in the main chain of the Central Tauern (''Mittlerer Tauernhauptkamm''). This chain lies in the High Tauern, part of the Austrian Central Alps on the border between the Austrian states of Tyrol in the south and Salzburg in the north. The mountain was given its present name in 1855 by the Austrian chemist and cartographer, Franz Keil. Because of its isolated situation the Großer Geiger has a significant dominance. With its distinctive, symmetric, pyramidal shape and its mighty northwest face which rises 350 metres above the Obersulzbachkees glacier at a gradient of 50°, it is the most prominent landmark in the entire Upper Sulzbach valley. Arêtes radiate from the summit in all four directions of the compass. The mountain is easy to reach and is thus a popular touring and climbing destination. It was first climbed on 20 August 1871 by the A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
