Kuchenspitze
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Kuchenspitze
The Kuchenspitze is a mountain, , in the Verwall between the valley of Stanzer Tal and Paznaun in the west of North Tyrol. Location and landscape The mountain rises south of St. Anton am Arlberg in the Stanzer valley. Northeast of the summit is the Darmstädter Hut.Peter Pindur, Roland Luzian, Andreas Weiskopf: 1770 ''Kuchenspitze 3148 m'' in ''Verwallgruppe'', Alpenvereinsführer, 1988, pp. 203 ff. The Kuchenspitze is the second highest peak in the Verwall Group after the Hoher Riffler. Its main summit is not the 3148 spot height, but the peak to the south; to the north are several other subpeaks.Alpenvereinsführer ''Verwallgruppe'' 1988, Skizze ''Übersicht Nord- und Nordostwand'', p. 207. The mountain is glaciated. In its north cirque (''Nordkar'') is the ''Großer Kuchenferner''; to the west, the ''Kleiner Kuchenferner''; and, to the south, between the main summit and the subpeak of the Küchlspitze (3,147 m), is the ''Großer Küchlferner''. The ridg ...
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Küchlspitze
The Küchlspitze (also: ''Küchelspitze'') is a three-thousander () in the Verwall between the valley of Stanzer Tal and Paznaun in the western North Tyrol in Austria. Location and landscape The mountain rises between St. Anton am Arlberg in the Stanzer valley and Ischgl in the Paznaun to the southeast. Northeast of the summit is the Darmstädter Hut.Peter Pindur, Roland Luzian, Andreas Weiskopf: 1790 ''Küchlspitze 3147 m'' in Alpine Club Guide ''Verwallgruppe'' 1988, pp. 216 ff. The Küchlspitze (which means "little Kuchenspitze") is the third highest peak in the range after the Hoher Riffler and 1 metre higher Kuchenspitze immediately to the north. It is a striking, three-sided pyramid. On the main ridge the eastern arête descends to the Rautejöchli () and ''Rautekopf'' (), the southwestern arête to the Schönpleisjöchli () and twin peaks of the Schönpleisköpfe (northern , southern ), and the northern arête runs in an S-shape to ...
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Scheibler (mountain)
Scheibler is a high mountain in the Verwall Alps in the Austrian state Tyrol. File:Blick_vom_Scheibler_zur_DA-Hütte.jpg, View from summit to the direction of Darmstädter Hütte File:Blick vom Scheibler 2.jpg, View from summit There are directs ascents from two alpine club hut Alpine club huts (german: Alpenvereinshütten) or simply club huts (''Clubhütten'') form the majority of the over 1,300 mountain huts in the Alps and are maintained by branches, or sections, of the various Alpine clubs. Although the usual English ...s: * From Darmstädter Hütte (2384 m, east of Scheibler) in two hours. * From Konstanzer Hütte (1688 m, north-west of Scheibler) in three hours. Both ascents meet at ''Kuchenjöchli'', the col between Scheibler and Kuchenspitze.AMAP: Austrian Map 1:50.000' References {{Reflist Mountains of the Alps Mountains of Tyrol (state) Two-thousanders of Austria Verwall Alps ...
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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 ...
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Verwall
The Verwall Alps or Verwall Group Reynolds, Kev (2005). ''Walking in the Alps'', 2nd ed., Cicerone, Singapore, pp. 321-326. . are a mountain range of the Central Eastern Alps at the border of the Austrian states of Tyrol and Vorarlberg. It includes the following peaks (sorted by height): * Hoher Riffler 3,168 metres (10,394 feet) * Kuchenspitze 3,148 metres (10,401 feet) * Küchlspitze 3,147 metres (10,315 feet) * Patteriol 3,059 metres (10,037 feet) * Saumspitze 3,039 metres (9,970 feet) * Scheibler 2,978 metres (9,770 feet) * Gaisspitze 2,779 metres (9,117 feet) For a list of passes, see Passes of the Silvretta and Rätikon Ranges The Verwall Alps border on the Silvretta Alps in the west and on the Samnaun Alps The Samnaun Alps are a mountain range of the Central Eastern Alps, named after the Swiss ...
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Verwall Alps
The Verwall Alps or Verwall Group Reynolds, Kev (2005). ''Walking in the Alps'', 2nd ed., Cicerone, Singapore, pp. 321-326. . are a mountain range of the Central Eastern Alps at the border of the Austrian states of Tyrol and Vorarlberg. It includes the following peaks (sorted by height): * Hoher Riffler 3,168 metres (10,394 feet) * Kuchenspitze 3,148 metres (10,401 feet) * Küchlspitze 3,147 metres (10,315 feet) * Patteriol 3,059 metres (10,037 feet) * Saumspitze 3,039 metres (9,970 feet) * Scheibler 2,978 metres (9,770 feet) * Gaisspitze 2,779 metres (9,117 feet) For a list of passes, see Passes of the Silvretta and Rätikon Ranges The Verwall Alps border on the Silvretta Alps The Silvretta Alps are a mountain range of the Central Eastern Alps shared by Tirol, Vorarlberg (both in Austria) and Gra ...
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Verwall Group
The Verwall Alps or Verwall Group Reynolds, Kev (2005). ''Walking in the Alps'', 2nd ed., Cicerone, Singapore, pp. 321-326. . are a mountain range of the Central Eastern Alps at the border of the Austrian states of Tyrol and Vorarlberg. It includes the following peaks (sorted by height): * Hoher Riffler 3,168 metres (10,394 feet) * Kuchenspitze 3,148 metres (10,401 feet) * Küchlspitze 3,147 metres (10,315 feet) * Patteriol 3,059 metres (10,037 feet) * Saumspitze 3,039 metres (9,970 feet) * Scheibler 2,978 metres (9,770 feet) * Gaisspitze 2,779 metres (9,117 feet) For a list of passes, see Passes of the Silvretta and Rätikon Ranges The Verwall Alps border on the Silvretta Alps in the west and on the Samnaun Alps The Samnaun Alps are a mountain range of the Central Eastern Alps, named after the Swiss ...
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Mountain
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 (topography), 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 Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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First Climbed
In mountaineering, a first ascent (abbreviated to FA in guide books) is the first successful, documented attainment of the top of a mountain or the first to follow a particular climbing route. First mountain ascents are notable because they entail genuine exploration, with greater risks, challenges and recognition than climbing a route pioneered by others. The person who performs the first ascent is called the first ascensionist. In free climbing, a first ascent (or first free ascent, abbreviated FFA) of a climbing route is the first successful, documented climb of a route without using equipment such as anchors or ropes for aiding progression or resting. History The details of the first ascents of even many prominent mountains are scanty or unknown; sometimes the only evidence of prior summiting is a cairn, artifacts, or inscriptions at the top. Today, first ascents are generally carefully recorded and usually mentioned in guidebooks. The term is also used when referrin ...
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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 ...
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Alpine Three-thousanders
Three-thousanders are mountains with a height of between , but less than above sea level. Similar terms are commonly used for mountains of other height brackets e. g. four-thousanders or eight-thousanders. In Britain, the term may refer to mountains above . Climatological significance In temperate latitudes three-thousanders play an important role, because even in summer they lie below the zero degree line for weeks. Thus the chains of three-thousanders always form important climatic divides and support glaciation - in the Alps the contour is roughly the general limit of the "nival step"; only a few glaciated mountains are under (the Dachstein, the easternmost glaciated mountain in the Alps, is, at , not a three-thousander). In the Mediterranean, however, the three-thousanders remain free of ice and, in the tropics, they are almost insignificant from a climatic perspective; here the snow line lies at around to , and in the dry continental areas (Trans-Himalayas, Ande ...
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UIAA 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 ascensioni ...
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