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Große Schlenkerspitze
The Große Schlenkerspitze is a mountain in the Lechtal Alps in the Austrian state of Tyrol. At or, according to other sources, 2,831 m, it is the highest peak in the eastern part of the Lechtal Alps. Summit block The massif of the Schlenkerspitze is a rock wall of main dolomite over two kilometres long. Its north arête drops down to the saddle of Galtseitejoch, its southwest arête links the Große Schlenkerspitze to the ''Kleine Schlenkerspitze'' () and then drops into the Hintere Dremelscharte col. The east arête joins it to the Brunnkarspitze. The entire Schlenker massif is brittle and ruptured, the arêtes bristle with innumerable pinnacles because the rock strata are vertical here. First ascent The Große Schlenkerspitze was first ascended in 1882 from the Galtseitenjoch saddle by Spiehler and Friedel; the Kleine Schlenkerspitze via the southeast arête in 1896 by Ampferer and W. Hammer. Tours * From Galtseitejoch, 2,423 m, via the north arête, grade II+ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arête
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 arête steepened through mass wasting Mass wasting, also known as mass movement, is a general term for the movement of rock or soil down slopes under the force of gravity. It differs from other processes of erosion in that the debris transported by mass wasting is not entrained in ... events and the erosion of exposed, unstable rock. The word ''arête'' () is actually French for "edge" or "ridge"; similar features in the Alps are often described with the German language, German equivalent term ''Grat''. Where three or more cirques meet, a pyramidal peak is created. Cleaver A ''cleaver' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Two-thousanders Of Austria
Two-thousanders are mountains that have a height of at least 2,000 metres above sea level, but less than 3,000 metres. The term is used in Alpine circles, especially in Europe (e.g. German: ''Zweitausender''). The two photographs show two typical two-thousanders in the Alps that illustrate different types of mountain. The Säuling (top) is a prominent, individual peak, whereas the Schneeberg (bottom) is an elongated limestone massif. In ranges like the Allgäu Alps, the Gesäuse or the Styrian-Lower Austrian Limestone Alps the mountain tour descriptions for mountaineers or hikers commonly include the two-thousanders, especially in areas where only a few summits exceed this level. Examples from these regions of the Eastern Alps are: * the striking Nebelhorn (2,224 m) near Oberstdorf or the Säuling (2,047 m) near Neuschwanstein, * the Admonter Reichenstein (2,251 m), Eisenerzer Reichenstein (2,165 m), Großer Pyhrgas (2,244 m) or Hochtor (2,369&nbs ... [...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] |
Bergverlag Rother
Bergverlag Rother is a German publisher with its headquarters in Oberhaching, Upper Bavaria. Since 1950 the company, that formerly went under the name of ''Bergverlag Rudolf Rother'', has published the Alpine Club Guides in cooperation with the German Alpine Club (DAV), the Austrian Alpine Club (ÖAV) and the South Tyrol Alpine Club. Rother publish a "famous series of English language guides" covering most of the popular walking destinations in the Alps and Europe. History The company was founded on 16 November 1920 in Munich Munich ( ; german: München ; bar, Minga ) is the capital and most populous city of the States of Germany, German state of Bavaria. With a population of 1,558,395 inhabitants as of 31 July 2020, it is the List of cities in Germany by popu ... by Rudolf Rother sen., a bookseller and mountaineer, and is one of the oldest and most important specialist Alpine publishers. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpine Club Guide
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] |
Otto Ampferer
Otto Ampferer (* 1 December 1875 in Hötting near Innsbruck; † 9 July 1947) was an Austrian alpinist and geologist. To explain the complex processes of Orogeny, he developed his "theory of undercurrent" with the idea of a partially plastic earth's crust. He became - even before Alfred Wegener - the pioneer of the modern view of mobilism. Life and scientific work Ampferer attended grammar school and then studied physics, mathematics and geology at the University of Innsbruck from 1895, where he obtained his doctorate in 1899. In 1901 he entered the service of the Vienna Geologische Bundesanstalt, which at that time was still ''Geologische Reichsanstalt''. In 1902 he married Olga Sander, the sister of the well-known Innsbruck geologist Bruno Sander. She was his companion on all the walks and she assisted him in many ways. In 1919 he was appointed chief geologist and vice-director of the Federal Institute in 1925. From 1935 to 1937 he was director of this research institute, bu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
First Ascended
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 referring t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Main Dolomite
Main Dolomite (german: Hauptdolomit, hu, Fődolomit, it, Dolomia Principale) is a lithostratigraphic unit in the Alps of Europe. Formation was defined by K.W. Gümbel in 1857. Middle to Late Triassic sedimentary record in the Alpine realm is characterized by presence of various masses of dolomitic rock formations. In the Northern Calcareous Alps the dolomitic mass of Ladinian - Norian age is divided by the Carnian sandstones and shales of Lunz Formation to the Ladinian - Carnian Wetterstein Dolomite and Norian Main Dolomite.Tollmann, A., 1976: Analyse des klassischen nordalpinen Mesozoikums, Wien, Franz Deuticke, 580 pp. The Main Dolomite reaches higher thickness than underlying dolomites in Alps, therefore it is considered as more important "Main". Extent The formation is found in: * the Northern Limestone Alps and Southern Limestone Alps of the Limestone Alps, a mountain system of the western and Central Eastern Alps. * the Apennines in Italy * the Western Carpathians (Ta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edward Theodore Compton
Edward Theodore Compton, usually referred to as E. T. Compton, (29 July 1849 – 22 March 1921) was an English-born, German artist, illustrator and mountain climber. He is well known for his paintings and drawings of alpine scenery, and as a mountaineer made 300 major ascents including no fewer than 27 first ascents. Life Compton was born in Stoke Newington in London, the son of Theodore Compton, an art-loving insurance agent, and grew up in a deeply religious Quaker household. He attended Sidcot School from 1861 to 1864 and various art schools, including, for a time, the Royal Academy in London, but otherwise he was mainly self-taught in art. In 1867, wanting the best education for their artistically-talented son, and due to the high cost of schooling in England, the family decided to emigrate to Germany settling in Darmstadt. The city at that time was the seat of the Grand Duchy of Hesse under Grand Duke Ludwig III, and a community of artists had sprung up there. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anton Spiehler (alpinist) , the championship trophy of the Swedish junior hockey ...
Anton may refer to: People *Anton (given name), including a list of people with the given name *Anton (surname) Places *Anton Municipality, Bulgaria **Anton, Sofia Province, a village *Antón District, Panama **Antón, a town and capital of the district *Anton, Colorado, an unincorporated town *Anton, Texas, a city *Anton, Wisconsin, an unincorporated community *River Anton, Hampshire, United Kingdom Other uses *Case Anton, codename for the German and Italian occupation of Vichy France in 1942 *Anton (computer), a highly parallel supercomputer for molecular dynamics simulations * ''Anton'' (1973 film), a Norwegian film * ''Anton'' (2008 film), an Irish film *Anton Cup The Anton Cup is the championship trophy of the Swedish junior hockey league, J20 SuperElit. The trophy was donated by Anton Johansson, chairman of the Swedish Ice Hockey Association between 1924 and 1948, in 1952, as an award for Sweden's top-rank ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Main Dolomite
Main Dolomite (german: Hauptdolomit, hu, Fődolomit, it, Dolomia Principale) is a lithostratigraphic unit in the Alps of Europe. Formation was defined by K.W. Gümbel in 1857. Middle to Late Triassic sedimentary record in the Alpine realm is characterized by presence of various masses of dolomitic rock formations. In the Northern Calcareous Alps the dolomitic mass of Ladinian - Norian age is divided by the Carnian sandstones and shales of Lunz Formation to the Ladinian - Carnian Wetterstein Dolomite and Norian Main Dolomite.Tollmann, A., 1976: Analyse des klassischen nordalpinen Mesozoikums, Wien, Franz Deuticke, 580 pp. The Main Dolomite reaches higher thickness than underlying dolomites in Alps, therefore it is considered as more important "Main". Extent The formation is found in: * the Northern Limestone Alps and Southern Limestone Alps of the Limestone Alps, a mountain system of the western and Central Eastern Alps. * the Apennines in Italy * the Western Carpathians (Ta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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