|
Double Peak (other)
A double summit, double peak, twin summit, or twin peak refers to a mountain or hill that has two summits, separated by a col or saddle. One well-known double summit is Austria’s highest mountain, the Großglockner, where the main summit of the Großglockner is separated from that of the Kleinglockner by the Glocknerscharte col in the area of a geological fault. Other double summits have resulted from geological folding. For example, on Mont Withrow in British Columbia, resistant sandstones form the limbs of the double summit, whilst the softer rock in the core of the fold was eroded.{{cite web , url=http://gsc.nrcan.gc.ca/natmap/cf/intro_e.php , title=Mt. Withrow syncline , archive-url=https://web.archive.org/web/20060404185911/http://gsc.nrcan.gc.ca/natmap/cf/intro_e.php , archive-date=2006-04-04 , access-date=2009-05-12 Triple peaks occur more rarely; one example is the Rosengartenspitze in the Dolomites. The Illimani in Bolivia is an example of a rare quadruple summit. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schneeberg (Lower Austria)
The Schneeberg, with its high summit ''Klosterwappen'', is the highest mountain of Lower Austria, and the easternmost and northernmost mountain in the Alps to exceed 2000 m. It is a distinctive limestone massif with steep slopes on three sides. The Schneeberg is one of the Northern Calcareous Alps in the borderland between Lower Austria and Styria, in the eastern part of Austria. It and the Rax (), some to the south-west, are collectively considered the Viennese Hausberge (Vienna's "local mountains"). The rich Karst plateaux have provided drinking water for Vienna, via a long pipeline, since 1873, and is claimed to be the best drinking water in the world. On clear days, Schneeberg can be readily seen from parts of Vienna, some away (as the crow flies), from Bratislava in Slovakia and even from Babí Lom above Brno 180 km away. The Schneeberg is a summit with a height of over 1500 m, which just misses the limit for an ultra-prominent peak (1500). A rack-and-pinion rai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karlspitzen
The Karlspitzen is a twin-peaked mountain in the middle of the Kaisergebirge range of the Northern Limestone Alps in Austria. The two peaks are the northern ''Hintere Karlspitze'' (2,281 m) and the southern ''Vordere Karlspitze'' (2,263 m) with its summit cross; they are linked by a sharp, exposed, rocky arête. Seen from the south the Vordere Karlspitze is a huge and very prominent block of rock, whereas the Hintere Karlspitze is hidden behind other (lower) neighbouring mountains. Location The Karlspitzen peaks tower over the Ellmauer Tor saddle and Steinerne Rinne couloir to their east and so lie in the heart of the Wilder Kaiser mountains. To the east rise the rather lower summits of the Goinger Halt and Predigtstuhl, immediately to the north are the Fleischbank and Totenkirchl and, further west, separated by the Kopftörl arête, is the higher Ellmauer Halt. Thanks to its location the Karlspitzen have extensive views over both the Wilder Kaiser and also the neighbouring ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salzburg State
Salzburg (, ; bar, Soizbuag, label=Austro-Bavarian) (also known as ''Salzburgerland'') is a 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-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 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 and Tyrol. With 529,085 inhabitants, it is one of the country's smaller states in terms of population. Running through the south are the main ranges of the Alpine divide (incl. the Hohe Tauern mountains) with numerous three-thousander ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tennen Mountains
The Tennen Mountains (german: Tennengebirge) is a small, but rugged, mountain range in the Northern Limestone Alps, which lies in front of the Eastern Alps for its entire length. It is a very heavily karstified high plateau, about 60 km² in area, with many caves. The range is located in Austria in the district of Salzburg near Bischofshofen. Some 37 square kilometres of the Tennen plateau are above the 2,000 metre line and that part of the range within the state of Salzburg was turned into a nature reserve in 1982. Extent and neighbouring ranges The outline of the Tennen range is formed: * in the west by the ''Hagen Mountains'', a part of the ''Berchtesgaden Alps'', separated by the Salzach river. Here, at the northern end of the Lueg Pass, is the narrowest point of the Salzachöfen Gorge through the Limestone Alps. * in the north and northeast by the River Lammer as far as the Rußbach stream, which descends from the Gschütt Pass. Beyond the Lammer is the ''Osterhorn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eiskogel (Tennengebirge)
Eiskogel ("ice peak") may refer to the following mountains: * Eiskogel (Tennen Mountains), 2321 m, near Werfenweng in the Pongau, Salzburg state, Austria * Eiskogel (Upper Austrian Prealps), 1,087 m, between Almtal und Kremstal, Upper Austria * Großer Eiskogel, 3547 m, in the Ortler Alps, South Tyrol, Italy * Kleiner Eiskogel, 3105 m, in the Ortler Alps, South Tyrol, Italy {{dab ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gosaukamm
The Gosaukamm is an Austrian mountain chain within the Dachstein range of the Northern Limestone Alps. Although relatively short in length, the chain forms an imposing backdrop to the valley and town of Gosau. Its highest point reaches an elevation of . Geography The main ridge of the Gosaukamm forms the border between the Austrian states of Salzburg and Upper Austria. Part of the ''Dachstein Massif;'' it is located northwest of the Hoher Dachstein summit and forms part of the UNESCO World Heritage Site Hallstatt-Dachstein/Salzkammergut Cultural Landscape"Hallstatt-Dachstein/Salzkammergut Cultural Landscape - Maps" Unesco.org. Map download retrieved 12/06/2020 The Vorderer Gosausee lies a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Große Bischofsmütze
The Große Bischofsmütze (German: "great bishop's mitre") is the highest peak in the Gosaukamm range of the Dachstein Mountains, Austria. Together with the Kleine Bischofsmütze (), the Große Bischofsmütze () forms a distinctive twin-peak, with the two summits separated by the ''Mützenschlucht'' ravine''.'' The mountain is in the state of Salzburg, near the border with Upper Austria, and forms part of the larger Northern Limestone Alps. History The name of the mountain can be attributed to its characteristic shape, that resembles a bishop's mitre ("Bischofsmütze"). The mountain has also been referred to historically as ''Gosauer Stein'' ("Stone of Gosau") due to its location overlooking the town of Gosau. The Große Bischofsmütze was first ascended on June 28, 1879 by Johann Anhäusler and Johann Steiner. Two major rockfalls occurred in 1993 that displaced 100,000 tonnes of rock into the valley below, altering the mountain's visual profile. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
