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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 cooperat ... [...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 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 first fre ... [...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 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 Hohes Kreuz () is a municipality in the Eichsfeld in Thuringia Thuringia (; german: Thüringen ), officially the Free State of Thuringia ( ), is a state of central Germany, covering , the sixth smallest of the sixteen German states. It has a ... 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 Hun ... [...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] |
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 Dac ... [...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 th ... [...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 lime ... [...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 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 equivalent term ''Grat''. Where three or more cirques meet, a pyramidal peak is created. Cleaver A ''cleaver'' is a type of arête that separates a unified flow of glacial ice from its uphill side into two glaciers flanking, and flowing parallel to, the ridge. ''Cleaver'' gets its name from the way it resembles a meat cleaver slicing meat into two parts. A cleaver may be t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grade (climbing)
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] |
Dachstein South Face 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] |
Cirque
A (; from the Latin word ') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic , meaning a pot or cauldron) and (; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (small lake) behind a dam, which marks the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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