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Hochwannig
The Wannig (also Hochwannig or Wanneck) is a 2,493-metre-high mountain in the Mieming Chain in the Austrian state of Tyrol. Location The Wannig forms the western end of the Mieming Range. To the southwest lies the village of Nassereith in the Gurgltal valley, to the south is the Holzleiten Saddle that links the Gurgltal with the Mieming Plateau. To the north lies the Fern Pass, a crossing from the Gurgltal to Biberwier in the Ehrwald Basin. To the east the Mieming Chain continues with the ''Handschuhspitzen'' and the Marienbergjoch (1,789 m). The upper 400m of the Wannig are characterised by crags and boulder fields, below which is a wide belt of mountain pine. In the lower regions of its western and southern slopes are the remains of old mine workings. Here in the Feigenstein Field (''Revier Feigenstein''), lead and zinc ore (Smithsonite) was mined. Ascents The Wannig is usually climbed from the ''Nassereither Alm'' (1,718 m, also called the ''Muthenaualm'') to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mieming Chain
The Mieming(er) Range, Mieminger Chain (german: Mieminger Kette) or Mieminger Mountains (''Mieminger Gebirge''), is a mountain range of the Northern Limestone Alps in the Eastern Alps. It is located entirely in Austria within the state of Tyrol. This sub-group is somewhat in the shadows of its more famous neighbour, the Wetterstein to the north. Whilst the region around the Coburger Hut and the lakes of Seebensee and Drachensee in the west ( Ehrwalder Sonnenspitze and Vorderer Tajakopf with its new ''klettersteig'' over the Tajakante) and the Hohe Munde in the extreme east receive large numbers of visitors, the less developed central area remains very quiet. The Hohe Munde is also a popular and challenging ski touring destination. Public transport links: The Außerfern Railway stops at Ehrwald on the western side of the range. Busses run from Leutasch on the southern side of the mountains to Mittenwald and Seefeld in Tirol. Geology The Mieminger Mountains lie in a partic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zinc
Zinc is a chemical element with the symbol Zn and atomic number 30. Zinc is a slightly brittle metal at room temperature and has a shiny-greyish appearance when oxidation is removed. It is the first element in group 12 (IIB) of the periodic table. In some respects, zinc is chemically similar to magnesium: both elements exhibit only one normal oxidation state (+2), and the Zn2+ and Mg2+ ions are of similar size.The elements are from different metal groups. See periodic table. Zinc is the 24th most abundant element in Earth's crust and has five stable isotopes. The most common zinc ore is sphalerite (zinc blende), a zinc sulfide mineral. The largest workable lodes are in Australia, Asia, and the United States. Zinc is refined by froth flotation of the ore, roasting, and final extraction using electricity ( electrowinning). Zinc is an essential trace element for humans, animals, plants and for microorganisms and is necessary for prenatal and postnatal development. It ... [...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] |
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] |
Alpenverein Südtirol
The South Tyrol Alpine Club (german: Alpenverein Südtirol), abbreviated AVS, is an association of German and Ladin-speaking mountain climbers in South Tyrol, northern Italy. Founded in 1946, it is sub-divided into 32 sections and 58 local divisions. The AVS is based in Bolzano and has more than 60,000 members. History Originally, the South Tyrolean alpine club sections were members of the German and Austrian Alpine Club (''Deutscher und Österreichischer Alpenverein''). In 1869 the first sections were founded in Bozen and Niederdorf, Puster Valley. By 1910, 15 more sections had been established in South Tyrol. They initiated the construction of 19 mountain huts, an extensive network of paths through the mountains and training for mountain guides. After the end of the First World War, the annexation of South Tyrol by Italy and the coming into power of the fascists, the South Tyrolean sections were disappropriated and banned in 1923 (see Italianization of South Tyrol). After th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deutscher Alpenverein
The German Alpine Club (german: links=no, Deutscher Alpenverein, DAV for short) is the world's largest climbing association and the eighth-largest sporting association in Germany. It is a member of the German Olympic Sports Confederation and the competent body for sport and competition climbing, hiking, mountaineering, hill walking, ice climbing, mountain expeditions, as well as ski mountaineering. It is an association made up of local branches known as 'sections'. History The German Alpine Club was founded as on 9 May 1869 in Munich by 36 former members of the Austrian Alpine Club around the Ötztal curate Franz Senn. It was founded in order to promote the development of tourism in the Eastern Alps through the building of mountain huts, and establishment of hiking trails, and via ferratas. The association had a large membership from the beginning, attracting 1,070 members in the first ten months. The German and the Austrian societies merged in 1873 to form the German and Aus ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Österreichischer Alpenverein
The Austrian Alpine Club (german: Österreichischer Alpenverein) has about 573,000 members in 196 sections and is the largest mountaineering organisation in Austria. It is responsible for the upkeep of over 234 alpine huts in Austria and neighbouring countries. It also maintains over 26,000 kilometres of footpaths, and produces detailed maps of key mountain areas within Austria. Much of this work is done by the association's 22,000 volunteers. The association has a museum in Innsbruck dedicated to the history of alpinism. It also has sections in Belgium and the United Kingdom, and a group in Poland. See also * South Tyrol Alpine Club (Alpenverein Südtirol, AVS) * German Alpine Club The German Alpine Club (german: links=no, Deutscher Alpenverein, DAV for short) is the world's largest climbing association and the eighth-largest sporting association in Germany. It is a member of the German Olympic Sports Confederation and the ... (Deutscher Alpenverein, DAV) References E ... [...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] |
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] |
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] |
Smithsonite
Smithsonite, also known as zinc spar, is the mineral form of zinc carbonate ( Zn CO3). Historically, smithsonite was identified with hemimorphite before it was realized that they were two different minerals. The two minerals are very similar in appearance and the term calamine has been used for both, leading to some confusion. The distinct mineral smithsonite was named in 1832 by François Sulpice Beudant in honor of English chemist and mineralogist James Smithson (c.1765–1829), who first identified the mineral in 1802. Smithsonite is a variably colored trigonal mineral which only rarely is found in well formed crystals. The typical habit is as earthy botryoidal masses. It has a Mohs hardness of 4.5 and a specific gravity of 4.4 to 4.5. Smithsonite occurs as a secondary mineral in the weathering or oxidation zone of zinc-bearing ore deposits. It sometimes occurs as replacement bodies in carbonate rocks and as such may constitute zinc ore. It commonly occurs in association with he ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
