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Taubenkogel
The Taubenkogel is a high peak in the Dachstein Mountains of Upper Austria Upper Austria (german: Oberösterreich ; bar, Obaöstareich) is one of the nine states or of Austria. Its capital is Linz. Upper Austria borders Germany and the Czech Republic, as well as the other Austrian states of Lower Austria, Styria, a ..., northeast of the Hallstätter Glacier. It can be reached from the summit station of the Dachstein Cable Car on the Gjaidalm or from the Simony Hut. In good weather there is a fine view from the summit of the Hoher Dachstein, the Gjaidstein and the Hallstätter Glacier. Dachstein Mountains Mountains of the Alps Mountains of Upper Austria Two-thousanders of Austria {{UpperAustria-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Simony Hut
The Simony Hut (german: Simonyhütte) is an Alpine club hut belonging to the Austrian Alpine Club (OeAV) located at a height of 2,205 metres, just below the Hallstätter Glacier at the foot of the Hoher Dachstein in Austria. The hut, which is named after Friedrich Simony the first person to ascend Hoher Dachstein, is high above Hallstatt in Upper Austria in the northern part of the Dachstein Mountains. It is open year-round and, in winter, offers numerous options for ski tours and snowshoe walking. The Simony Hut is an important base for climbing, climbers because they are able to set out from here on long tours over the Dachsteins. There is also a mountaineering school where training courses are run for glacier or ice climbing. The Dachstein Chapel is nearby. History In 1843 a stone rest and emergency shelter, known as "Hotel Simony", was opened just below the site of the present hut. In 1876, Friedrich Simony selected the present location himself for construction of the firs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dachstein Mountains
The Dachstein Mountains (german: Dachsteingebirge) are a mountain range in the Northern Limestone Alps. The term is used by the Austrian Alpine Club in its classification of the Eastern Alps as one of the 24 sub-ranges of the Northern Limestone Alps (AVE No. 14). The ''Dachstein'' range includes: * The Dachstein Massif proper with its highest peak, the Hoher Dachstein () * Grimming () in the east to the upper Styrian Enns valley * Sarstein () in the north at the other bank of the River Traun Extent The Dachstein Mountains are bordered as follows: * to the northeast by the ''Totes Gebirge'', which is separated by the line from Sankt Agatha on the Hallstättersee – Pötschenhöhe – Bad Aussee – Kainischtraun – Bad Mitterndorf – Klachau – Grimmingbach to the River Enns * to the south by the '' Rottenmanner und Wölzer Tauern'' and the ''Niedere Tauern'', which are separated by the River Enns, roughly from Untergrimming to its con ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upper Austria
Upper Austria (german: Oberösterreich ; bar, Obaöstareich) is one of the nine states or of Austria. Its capital is Linz. Upper Austria borders Germany and the Czech Republic, as well as the other Austrian states of Lower Austria, Styria, and Salzburg. With an area of and 1.49 million inhabitants, Upper Austria is the fourth-largest Austrian state by land area and the third-largest by population. History Origins For a long period of the Middle Ages, much of what would become Upper Austria constituted Traungau, a region of the Duchy of Bavaria. In the mid-13th century, it became known as the Principality above the Enns River ('), this name being first recorded in 1264. (At the time, the term "Upper Austria" also included Tyrol and various scattered Habsburg possessions in South Germany.) Early modern era In 1490, the area was given a measure of independence within the Holy Roman Empire, with the status of a principality. By 1550, there was a Protestant majority. In 1564, ... [...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] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hallstätter Glacier
The Hallstätter Glacier (german: Hallstätter Gletscher) (formerly also called the ''Karleisfeld'' or Karl Icefield) is the largest glacier in the Dachstein Mountains. It lies immediately beneath the northern foot of the Dachstein itself and runs down to the Eissee lake below the Simony Hut The Simony Hut (german: Simonyhütte) is an Alpine club hut belonging to the Austrian Alpine Club (OeAV) located at a height of 2,205 metres, just below the Hallstätter Glacier at the foot of the Hoher Dachstein in Austria. The hut, which is name ... at a height of 2,205 m. To the east the Hallstätter Glacier is bounded by the High Gjaidstein. Firmly sealed off at its western snout by the Schöberl, 2,426 m, it is bordered in the west by the eastern flank of the Hohes Kreuz ridge, running from south to north, which reaches a height of 2,837 metres. In its upper third the glacier flows around a prominent landmark, the ''Eisstein''. At its head in the south it is also bordered by the Hu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dachstein Cable Car
Hoher Dachstein () is a strongly karstic mountain in central Austria and the second-highest mountain in the Northern Limestone Alps. It is situated at the border of Upper Austria and Styria, and is the highest point in each of those states. Parts of the massif also lie in the state of Salzburg, leading to the mountain being referred to as the ''Drei-Länder-Berg'' ("three-state mountain"). The Dachstein massif covers an area of around with dozens of peaks above 2,500 m, the highest of which are in the southern and southwestern areas. The main summit of the Hoher Dachstein is at an elevation of . Seen from the north, the Dachstein massif is dominated by glaciers with rocky summits rising beyond them. By contrast, to the south, the mountain drops almost vertically to the valley floor. Geology The geology of the Dachstein massif is dominated by the ''Dachstein-Kalk'' Formation ("Dachstein limestone"), dating from Triassic times. In common with other karstic areas, the Dach ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hoher Dachstein
Hoher Dachstein () is a strongly karstic mountain in central Austria and the second-highest mountain in the Northern Limestone Alps. It is situated at the border of Upper Austria and Styria, and is the highest point in each of those states. Parts of the massif also lie in the state of Salzburg, leading to the mountain being referred to as the ''Drei-Länder-Berg'' ("three-state mountain"). The Dachstein massif covers an area of around with dozens of peaks above 2,500 m, the highest of which are in the southern and southwestern areas. The main summit of the Hoher Dachstein is at an elevation of . Seen from the north, the Dachstein massif is dominated by glaciers with rocky summits rising beyond them. By contrast, to the south, the mountain drops almost vertically to the valley floor. Geology The geology of the Dachstein massif is dominated by the ''Dachstein-Kalk'' Formation ("Dachstein limestone"), dating from Triassic times. In common with other karstic areas, the Dachs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gjaidstein
The Hoher Gjaidstein is a 2,794 m high mountain peak in the Dachstein Mountains in Upper Austria east and above the Hallstätter Glacier. It may be reached from the summit station of the Dachstein South Face Cable Car or from the Simony Hut each of which is an easy grade I climb. As well as the ''Hoher Gjaidstein'' (="Higher Gjaidstein") there is also the ''Niederen Gjaidstein'' ("Lower Gjaidstein", 2,482 m) and the ''Kleinen Gjaidstein'' ("Little Gjaidstein", 2,734 m). The mountain was climbed as early as 1823 by de Halley from the north from the Gjaid cirque (''Gjaidkar''). Whether the actual summit had been conquered earlier is not known. Sources * Willi End: ''Alpenvereinsführer Dachsteingebirge Ost''. Bergverlag Rudolf 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 cooperatio ... [...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 Upper Austria
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 and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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