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Schoberköpfe
The Schoberköpfe are several ridge-shaped peaks, arranged along the eastern edge of the Hochkönig plateau in the Berchtesgaden Alps, and which lie in a semi-circular arc that opens towards the east facing the Salzach valley: * Southwestern Schoberkopf (''Südwestlicher Schoberkopf'', http://www.austrianmap.at/ BEV 1:50,000 series.) * Eastern Schoberkopf (''Östlicher Schoberkopf'', 2,666 m) * ''Teufelskirche'', also called the ''Teufelskirchl'' (2,520 mAlbert Precht: '' Alpenvereinsführer Hochkönig''), a rock tower in front of the Eastern Schoberkopf. The relatively steep, 200-300-metre-high south faces drop into the scree-covered ''Eiskar'' and climb up again opposite into the striking, isolated pillar of the Torsäule 2,588 m. Somewhat west of the arête, near the ''Schoberschartl'' gap (2,579 m), ends the plateau glacier of the Übergossene Alm, which covers part of the Hochkönig summit region. Ascents The first known tourist ascent of the Schober ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Torsäule
The Torsäule () is a very steep, about 500-metre-high limestone formation on the eastern flank of the Hochkönig massif in the Berchtesgaden Alps. The imposing column (''Torsäule'' means "gateway column"), which bears a summit cross, lies immediately north of the ascent route to the Hochkönig from the Arthurhaus, a thousand metres below, and measures about 500 × 200 metres at its base. In an east-west direction it looks like a giant column, but on reaching the high plateau of the Übergossene Alm it slowly disappears below the local horizon. Its south face which tapers towards the top is almost vertical, whilst the other faces have average gradients of about 60 to 80°. Structurally, the Torsäule rises in front of the mountain ridge which the high plateau of the Hochkönig massif and its plateau glacier bound on the eastern side and which opens like a rock arena in a semi-circle facing the column and looking towards the Salzach valley. The Torsäule rises, as the crow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hochkönig
The Hochkönig is a mountain group containing the highest mountain (Mount Hochkönig) in the Berchtesgaden Alps, Salzburgerland, Austria. The Berchtesgaden Alps form part of the Northern Limestone Alps. Location It lies to the west of the town of Bischofshofen in the Austrian state of Salzburg, 42 km due south of the city of Salzburg. Hochkönig is separated from the rest of the Berchtesgaden Alps, and more specifically from the Steinernes Meer (''stone ocean'') by the mountain pass '' Torscharte'' at 2246 m. The summit itself is at the southern edge of a large limestone plateau, which is covered by the glacier known as the "Übergossene Alm", however this glacier is currently shrinking at a rate of 6.2% per year, and is likely to vanish in the relatively near future. The edge of the summit plateau is surrounded by an almost circular chain of mountains: * Hochseiler, * Lammkopf, * Hochkönig, * Großer Bratschenkopf, * Kleiner Bratschenkopf, * Torsäule, * Schoberkö ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ãœbergossene Alm
The Übergossene Alm is the name of the summit region of the Hochkönig (2,941 m) in the Berchtesgaden Alps. It contains the remains of a glacier that used to cover almost the entire summit plateau; in 1888 around 5.5 km² of the plateau was covered by an ice sheet. Since then the glacial surface has melted until it now covers just 1.5 km² and the glacier has split into three, small crevasse-free areas. The name of the glacier goes back to a local legend. High plateau and its perimeter mountains The ''Hochkönig'' is the southernmost and highest mountain block in the Berchtesgaden Alps. Unlike the Watzmann massif about 20 kilometres to the north, it has a plateau that tilts gently towards the north and covers about 15 km². Only in the south does it fall steeply away in rock faces up to 1,000 metres high (the ''Mandlwände''). The edge of the plateau is formed by several high two-thousanders in the shape of a giant oval. Apart from the main summit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Großer Bratschenkopf
Grosser or Großer is the masculine nominative singular form of the German adjective "gross", meaning "big", "great", "large", "tall", and the like. It is part of many placenames, especially of mountains. It is also a surname. People with that surname include: * Alfred Grosser (born 1925), German-French writer, sociologist, and political scientist * Arthur Grosser (active from 1987), Canadian physical chemist and actor * Peter Grosser (1938–2021), German football player and coach * Philip Grosser (1890–1933), Ukrainian-American anarchist and anti-militarist * Thomas Grosser (1965–2008), German footballer * Pamela Grosser (born 1977), German actress See also * Gross (other) Gross may refer to: Finance *Gross Cash Registers, a defunct UK company with a high profile in the 1970s *Gross (economics), is the total income before deducting expenses Science and measurement *Gross (unit), a counting unit equal to 144 i ... * * {{surname Surnames of German origin< ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Two-thousanders Of Austria
Two-thousanders are mountains that have a height of at least 2,000 metres above sea level, but less than 3,000 metres. The term is used in Alpine circles, especially in Europe (e.g. German: ''Zweitausender''). The two photographs show two typical two-thousanders in the Alps that illustrate different types of mountain. The Säuling (top) is a prominent, individual peak, whereas the Schneeberg (bottom) is an elongated limestone massif. In ranges like the Allgäu Alps, the Gesäuse or the Styrian-Lower Austrian Limestone Alps the mountain tour descriptions for mountaineers or hikers commonly include the two-thousanders, especially in areas where only a few summits exceed this level. Examples from these regions of the Eastern Alps are: * the striking Nebelhorn (2,224 m) near Oberstdorf or the Säuling (2,047 m) near Neuschwanstein, * the Admonter Reichenstein (2,251 m), Eisenerzer Reichenstein (2,165 m), Großer Pyhrgas (2,244 m) or Hochtor (2,369&nbs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Climbing Grade
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] |
Ludwig Purtscheller
Ludwig Purtscheller (6 October 1849 – 3 March 1900) was an Austrian mountaineer and teacher. Purtscheller pioneered climbing without a mountain guide, who in the 19th century did all the route finding and lead climbing. By the end of his life he had recorded climbing over 1,700 mountains. A celebrated climb was the traverse of the Meije together with the Zsigmondy brothers in 1885, which to this date is considered a classic alpine route. He is best known as the first European to ascend Kilimanjaro in 1889, together with the German mountaineer Hans Meyer. After a descent of the Aiguille du Dru with G. Löwenbach and Jakob Oberhollenzer on 25 August 1899, an ice axe broke and the rope team fell into a bergschrund. Purtscheller was injured and he was transferred to a hospital in Geneva and later Bern german: Berner(in)french: Bernois(e) it, bernese , neighboring_municipalities = Bremgarten bei Bern, Frauenkappelen, Ittigen, Kirchlindach, Köniz, Mühleberg, Muri bei Bern, N ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateau Glacier
In glaciology, an ice cap is a mass of ice that covers less than of land area (usually covering a highland area). Larger ice masses covering more than are termed ice sheets. Description Ice caps are not constrained by topographical features (i.e., they will lie over the top of mountains). By contrast, ice masses of similar size that ''are'' constrained by topographical features are known as ice fields. The ''dome'' of an ice cap is usually centred on the highest point of a massif. Ice flows away from this high point (the ice divide) towards the ice cap's periphery. Ice caps have significant effects on the geomorphology of the area that they occupy. Plastic moulding, gouging and other glacial erosional features become present upon the glacier's retreat. Many lakes, such as the Great Lakes in North America, as well as numerous valleys have been formed by glacial action over hundreds of thousands of years. On Earth, there are about of total ice mass. The average temperature ... [...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 Mass wasting, also known as mass movement, is a general term for the movement of rock or soil down slopes under the force of gravity. It differs from other processes of erosion in that the debris transported by mass wasting is not entrained in ... 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 language, German equivalent term ''Grat''. Where three or more cirques meet, a pyramidal peak is created. Cleaver A ''cleaver' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bundesamt Für Eich- Und Vermessungswesen
The Federal Office of Metrology and Surveying of Austria (german: Bundesamt für Eich- und Vermessungswesen, BEV) is the body responsible for official surveying, geo-information and weights and measures (metrology) in Austria. It belongs to the ' (Federal Ministry of the Economy Location and Digitization). Its headquarters is in Vienna en, Viennese , iso_code = AT-9 , registration_plate = W , postal_code_type = Postal code , postal_code = , timezone = CET , utc_offset = +1 , timezone_DST ... and it has 67 branches spread across all the Austrian federal states. at www.bev.gv.at. Accessed on 30 Dec 10. List of Surveying offices [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salzach
The Salzach (Austrian: ˆsaltsax ) is a river in Austria and Germany. It is in length and is a right tributary of the Inn, which eventually joins the Danube. Its drainage basin of comprises large parts of the Northern Limestone and Central Eastern Alps. 83% of its drainage basin () lies in Austria, the remainder in Germany (Bavaria). Its largest tributaries are Lammer, Berchtesgadener Ache, Saalach, Sur and Götzinger Achen. Etymology The river's name is derived from the German word ''Salz'' "salt" and '' Aach''. Until the 19th century, shipping of salt down the ''Salzach'' was an important part of the local economy. The shipping ended when the parallel Salzburg-Tyrol Railway line replaced the old transport system. Course The Salzach is the main river in the Austrian state of Salzburg. The source is located on the edge of the Kitzbühel Alps near Krimml in the western Pinzgau region. Its headstreams drain several alpine pastures at around (metres above the Adriatic), be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhaetian
The Rhaetian is the latest age of the Triassic Period (in geochronology) or the uppermost stage of the Triassic System (in chronostratigraphy). It was preceded by the Norian and succeeded by the Hettangian (the lowermost stage or earliest age of the Jurassic). The base of the Rhaetian lacks a formal GSSP, though candidate sections include Steinbergkogel in Austria (since 2007) and Pignola-Abriola in Italy (since 2016). The end of the Rhaetian (and the base of the overlying Hettangian Stage) is more well-defined. According to the current ICS (International Commission on Stratigraphy) system, the Rhaetian ended ± 0.2 Ma (million years ago). In 2010, the base of the Rhaetian (i.e. the Norian-Rhaetian boundary) was voted to be defined based on the first appearance of '' Misikella posthernsteini'', a marine conodont. However, there is still much debate over the age of this boundary, as well as the evolution of ''M. posthernsteini''. The most comprehensive source of precise age ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
