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Hintertux Glacier
The Hintertux Glacier (german: Hintertuxer Gletscher) is the tourist name for the glaciers of the Gefrorene-Wand-Kees, also called the Tuxer Ferner, and the nearby Riepenkees at the top of the Tuxertal, a side valley of the Zillertal in the Austrian state of Tyrol. Both glaciers are accessed by gondola and chair lifts and is one of only two ski resorts in the world offering skiing 365 days a year (the other being Zermatt in Switzerland). At its highest point the ski region reaches a height of in the saddle between the peaks of the Gefrorene-Wand-Spitzen. Hintertux glacier is one of the most popular glaciers in Austria. It is open all year round with skiing in the winter, and hiking activities in the summer. Ice The ice of the Hintertux Glacier is up to thick at its deepest point. It has a length of about , but this varies annually by up to . As a result, the lifts have to be moved several times a year so that the masts remain vertical. The glacier contains up to about 190 mi ...
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Austrian Central Alps
The Central Eastern Alps (german: Zentralalpen or Zentrale Ostalpen), also referred to as Austrian Central Alps (german: Österreichische Zentralalpen) or just Central Alps, comprise the main chain of the Eastern Alps in Austria and the adjacent regions of Switzerland, Liechtenstein, Italy and Slovenia. South them is the Southern Limestone Alps. The term "Central Alps" is very common in the Geography of Austria as one of the seven major landscape regions of the country. "Central Eastern Alps" is usually used in connection with the Alpine Club classification of the Eastern Alps (''Alpenvereinseinteilung'', AVE). The Central Alps form the eastern part of the Alpine divide, its central chain of mountains, as well as those ranges that extend or accompany it to the north and south. The highest mountain in the Austrian Central Alps is Grossglockner at . Location The Central Alps have the highest peaks of the Eastern Alps, and are located between the Northern Limestone Alps and th ...
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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 ...
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Schwaz District
The Bezirk Schwaz is an administrative district (''Bezirk'') in Tyrol, Austria. It borders Bavaria (Germany) in the north, the districts of Kufstein, Kitzbühel and Pinzgau (Salzburg) in the east, South Tyrol (Italy) in the south, and the Innsbruck-Land district in the west. Area of the district is 1,887.49 km², with a population of 79,511 (January 1, 2012), and population density of 42 persons per km². Administrative center of the district is Schwaz. Geography The district comprises a part of the lower Inn valley, the complete Zillertal valley with its tributary valleys (like the Tuxertal), and the Achental valley with the Achensee. Mountain ranges within the district include the Tux Alps, Zillertal Alps, Kitzbühel Alps, the Karwendel and the Rofan. Administrative divisions The district is divided into 39 municipalities: * Achenkirch (2,156) * Aschau im Zillertal (1,732) * Brandberg (348) * Bruck am Ziller (993) * Buch bei Jenbach (2,549) * Eben am Achensee (2,84 ...
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Ski Areas In Austria
A ski is a narrow strip of semi-rigid material worn underfoot to glide over snow. Substantially longer than wide and characteristically employed in pairs, skis are attached to ski boots with ski bindings, with either a free, lockable, or partially secured heel. For climbing slopes, ski skins (originally made of seal fur, but now made of synthetic materials) can be attached at the base of the ski. Originally intended as an aid to travel over snow, they are now mainly used recreationally in the sport of skiing. Etymology and usage The word ''ski'' comes from the Old Norse word which means "cleft wood", "stick of wood" or "ski". In Old Norse common phrases describing skiing were ''fara á skíðum'' (to travel, move fast on skis), ''renna'' (to move swiftly) and ''skríða á skíðum'' (to stride on skis). In modern Norwegian the word ''ski'' has largely retained the Old Norse meaning in words for split firewood, wood building materials (such as bargeboards) and roundpole fence ...
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Inn Basin
Inns are generally establishments or buildings where travelers can seek lodging, and usually, food and drink. Inns are typically located in the country or along a highway; before the advent of motorized transportation they also provided accommodation for horses. History Inns in Europe were possibly first established when the Romans built their system of Roman roads two millennia ago. Many inns in Europe are several centuries old. In addition to providing for the needs of travelers, inns traditionally acted as community gathering places. Historically, inns provided not only food and lodging, but stabling and fodder for the travelers' horses, as well. Famous London examples of inns include The George Inn, Southwark, The George and The Tabard. However, there is no longer a formal distinction between an inn and several other kinds of establishments: many pubs use the name "inn", either because they are long established and may have been formerly coaching inns, or to summon up ...
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Glaciers Of The Alps
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur only in ...
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Glaciers Of Austria
A glacier ( ) or () is a persistent body of dense ice that is constantly moving under its own weight; it forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many years, often centuries. Glaciers slowly deform and flow due to stresses induced by their weight, creating crevasses, seracs, and other distinguishing features. Because glacial mass is affected by long-term climate changes, e.g., precipitation, mean temperature, and cloud cover, glacial mass changes are considered among the most sensitive indicators of climate change. There are about 198,000 to 200,000 glaciers in the world. Glaciers by continent Africa Africa, specifically East Africa, has contained glacial regions, possibly as far back as the last glacier maximum 10 to 15 thousand years ago. Seasonal snow does exist on the highest peaks of East Africa as well as in the Drakensberg Range of South Africa, the Stormberg Mountains, and the Atlas Mountains in Morocco. Current ...
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Gefrorene-Wand-Spitze
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 ...
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Funitel
A funitel is a type of cableway, generally used to transport skiers, although at least one is used to transport finished cars between different areas of a factory. It differs from a standard gondola lift through the use of two arms attached to two parallel overhead cables, providing more stability in high winds. The name ''funitel'' is a portmanteau of the French words ''funiculaire'' and ''telepherique''. When used to transport skiers, funitels are a fast way to get to a higher altitude. Skis or snowboard have to be taken off and held during the trip. Depending on the configuration, cabins may or may not contain seats. Without seats, funitels can sometimes be uncomfortable for long trips, in the same way other large cable cars can be. Funitels combine a short time between successive cabins with a capacity of around 20 to 30 people per cabin. Overview A funitel consists of one or two loops of cable strung between two terminals over intermediate towers. In order to maximize th ...
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Gondola Lift
A gondola lift is a means of cable transport and type of aerial lift which is supported and propelled by cables from above. It consists of a loop of steel wire rope that is strung between two stations, sometimes over intermediate supporting towers. The cable is driven by a bullwheel in a terminal, which is typically connected to an engine or electric motor. It is often considered a ''continuous system'' since it features a haul rope which continuously moves and circulates around two terminal stations. In contrast, an aerial tramway operates solely with fixed grips and simply shuttles back and forth between two end terminals. The capacity, cost, and functionality of a gondola lift will differ dramatically depending on the combination of cables used for support and haulage and the type of grip (detachable or fixed). Because of the proliferation of such systems in the Alps, the it, Cabinovia and french: Télécabine are also used in English-language texts. The systems m ...
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