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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] |
Großvenediger
Großvenediger () is the main peak of the Venediger Group within the Hohe Tauern mountain range, on the border of the Austrian state of Tyrol (East Tyrol) with Salzburg. It is generally considered to be Austria's fourth highest mountain (although it can be up to sixteenth if every subsidiary summit is counted). The summit, covered by glaciers, is part of the Hohe Tauern National Park. Name Originally known as ''Stützerkopf'', the name ''Großvenediger'' ( en, Great Venetian) is first recorded from a 1797 border survey. The origin of this name is unclear, probably deriving from Venetian merchants on their way over the mountain passes. An alternative theory is that the view from the summit may reach as far as Venice, some away, however, this is not in accordance with the facts. The author and mountaineer Ignaz von Kürsinger (1795–1861), one of the first climbers of the Großvenediger in 1840, coined the epithet ''weltalte Majestät'' (World-old Majesty). Climbing history Seve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
High Tauern
The High Tauern ( pl.; german: Hohe Tauern, it, Alti Tauri) are a mountain range on the main chain of the Central Eastern Alps, comprising the highest peaks east of the Brenner Pass. The crest forms the southern border of the Austrian states of Salzburg, Carinthia and East Tyrol, with a small part in the southwest belongs to the Italian province of South Tyrol. The range includes Austria's highest mountain, the Grossglockner at above the Adriatic. In the east, the range is adjoined by the Lower Tauern. For the etymology of the name, see Tauern. Geography According to the Alpine Club classification of the Eastern Alps, the range is bounded by the Salzach valley to the north (separating it from the Kitzbühel Alps), the Mur valley and the Murtörl Pass to the east (separating it from the Lower Tauern), the Drava valley to the south (separating it from the Southern Limestone Alps), and the Birnlücke Pass to the west (separating it from the Zillertal Alps). Its most important s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Venediger Group
The Venediger Group (german: Venedigergruppe) is a mountain range of the Central Eastern Alps. Together with the Granatspitze Group, the Glockner Group, the Goldberg Group, and the Ankogel Group, it forms the main ridge of the High Tauern. The highest peak is the Großvenediger at , which gives its name to the group. Considerable parts of the Venediger Group belong to the core zone of the High Tauern National parks of Austria, National Park. Geography The Venediger Group is located in Austria in the federal states of Salzburg (Bundesland), Salzburg and Tyrol (Bundesland), Tyrol, and also in Italy in the autonomous province of South Tyrol. The greater part of the range lies in East Tyrol. The Venediger Group includes the western part of the main chain of the High Tauern range. The Felber Tauern pass road runs across the Main chain of the Alps, Alpine crest between Salzburg and East Tyrol on the eastern side of the range. The Venediger Group is the most Glacier, glaciated mounta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salzburg (state)
Salzburg (, ; bar, Soizbuag, label=Bavarian language, Austro-Bavarian) (also known as ''Salzburgerland'') is a States of Austria, state (''Land'') of the modern Republic of Austria. It is officially named ''Land Salzburg'' to distinguish it from its eponymous capital — the city of Salzburg. For centuries, it was an independent Prince-Archbishopric of Salzburg, Prince-Bishopric of the Holy Roman Empire. Geography Location The state of Salzburg covers area of . It stretches along its main river — the Salzach – which rises in the Central Eastern Alps in the south to the Alpine foothills in the north. It is located in the north-west of Austria, close to the border with the Germany, German state of Bavaria; to the northeast lies the state of Upper Austria; to the east the state of Styria; to the south the states of Carinthia (state), Carinthia and Tyrol (state), Tyrol. With 529,085 inhabitants, it is one of the country's smaller states in terms of population. Running through th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Austria
Austria, , bar, Östareich officially the Republic of Austria, is a country in the southern part of Central Europe, lying in the Eastern Alps. It is a federation of nine states, one of which is the capital, Vienna, the most populous city and state. A landlocked country, Austria is bordered by Germany to the northwest, the Czech Republic to the north, Slovakia to the northeast, Hungary to the east, Slovenia and Italy to the south, and Switzerland and Liechtenstein to the west. The country occupies an area of and has a population of 9 million. Austria emerged from the remnants of the Eastern and Hungarian March at the end of the first millennium. Originally a margraviate of Bavaria, it developed into a duchy of the Holy Roman Empire in 1156 and was later made an archduchy in 1453. In the 16th century, Vienna began serving as the empire's administrative capital and Austria thus became the heartland of the Habsburg monarchy. After the dissolution of the H ... [...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] |
Sure-footedness
Sure-footedness is the ability, especially when hiking or mountain climbing, to negotiate difficult or rough terrain safely. Such situations place demands on a person's coordination and reserves of strength as well as requiring sufficient appreciation of the terrain. A person who is sure-footed is thus unlikely to slip or stumble, and will have a good head for heights when required. On many hiking trails and mountain tours, sure-footedness is assumed to be a prerequisite without ever being defined. The term is frequently used in the literature presumably to ensure that the reader is made sufficiently aware that, under certain circumstances, one false step may lead to serious consequences. Required attributes Although there is no standard definition of sure-footedness, [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...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] |
Mountains Of Salzburg (federal 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 a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
