Plattspitzen
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Plattspitzen
The Plattspitzen is a mountain in the Wetterstein Mountains on the border between Germany and Austria. It is a very striking mountain and the southern companion of Germany's highest peak, the Zugspitze, located at the opposite end of the ledge known as the ''Plattumrahmung''. The mountain has three summits: the eastern summit, known as the ''Gatterlspitz'' (2,680 m), the middle summit (''Mittelgipfel'', 2,674 m) and the western summit (''Westgipfel'', 2,676 m). It was first climbed in 1871 by Hermann von Barth, who conquered all three peaks alone departing from the '' Zugspitzplatt'' ledge. At that time the mountain was also known as the ''Wetterschrofen''. Location The mountain is made of Wetterstein limestone and lies just under 3 kilometres south of the Zugspitze, forming the southern cornerstone of the Zugspitze massif. One kilometre to the west it meets the higher, but much less prominent Wetterspitzen (2,746 m). To the south, towards the valley of ...
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Zugspitze
The Zugspitze (), at above Normalhöhennull, sea level, is the highest peak of the Wetterstein Mountains as well as the highest mountain in Germany. It lies south of the town of Garmisch-Partenkirchen, and the Austria–Germany border runs over its western summit. South of the mountain is the ''Zugspitzplatt'', a high karst plateau with numerous caves. On the flanks of the Zugspitze are three glaciers, including the two largest in Germany: the Schneeferner#Northern Schneeferner, Northern Schneeferner with an area of 30.7 hectares and the Höllentalferner with an area of 24.7 hectares. The third is the Schneeferner#Southern Schneeferner, Southern Schneeferner which covers 8.4 hectares. The Zugspitze was first climbed on 27 August 1820 by Josef Naus, his survey assistant, Maier, and mountain guide, Johann Georg Tauschl. Today there are three normal routes to the summit: one from the Höllental (Wetterstein), Höllental valley to the northeast; another out of the Reintal (Wetterste ...
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Zugspitzplatt
The Zugspitze (), at above sea level, is the highest peak of the Wetterstein Mountains as well as the highest mountain in Germany. It lies south of the town of Garmisch-Partenkirchen, and the Austria–Germany border runs over its western summit. South of the mountain is the ''Zugspitzplatt'', a high karst plateau with numerous caves. On the flanks of the Zugspitze are three glaciers, including the two largest in Germany: the Northern Schneeferner with an area of 30.7 hectares and the Höllentalferner with an area of 24.7 hectares. The third is the Southern Schneeferner which covers 8.4 hectares. The Zugspitze was first climbed on 27 August 1820 by Josef Naus, his survey assistant, Maier, and mountain guide, Johann Georg Tauschl. Today there are three normal routes to the summit: one from the Höllental valley to the northeast; another out of the Reintal valley to the southeast; and the third from the west over the Austrian Cirque (''Österreichische Schneekar''). One of the ...
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Jubiläumsgrat
The Jubiläumsgrat ("Jubilee Arête") or Jubiläumsweg ("Jubilee Way"), also nicknamed ''Jubi'' in climbing circles, is the name given to the climbing route along the arête between the Zugspitze (2,962 m) and the Hochblassen (2,706 m) (hence it is also called the ''Blassenkamm'' which means "Blassen Crest"). In front of its northwestern end, at the wind gap known as ''Falsche Grießkarscharte'', climbers normally cross over to the Alpspitze (2,628 m) or down to the Matheisen cirque. Along the arête the three peaks of the Höllentalspitzen (2,740 m), the Vollkarspitze (2,630 m) and several rises have to be assailed or circumnavigated. The route is a serious, high Alpine tour and not, as often described, a ''Klettersteig''. History Its name goes back to the founding members of the Munich branch of the German Alpine Club who, in 1894 in return for being honoured at the 25th anniversary of the branch, initially donated 900 marks, so that a "Jubilee Way" could be financed. By ...
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Gais
, neighboring_municipalities= Altstätten (SG), Appenzell (AI), Bühler (AR), Eichberg (SG), Rüte (AI), Schlatt-Haslen (AI), Trogen (AR) , twintowns= } Gais () is a village and a municipality in the canton of Appenzell Ausserrhoden in Switzerland. The area of Gais is . In 1977, the village Gais received the Wakker Prize for the development and preservation of its architectural heritage. The village square, the Protestant church of 1782, the former spa hotel ''Neuer Ochsen'' of 1796 and the ''Krone'' inn of 1781 are listed as heritage sites of national significance. Swiss inventory of cultural property of national and regional significance (1995), p. 53 History The village of ''de Geis'' is first mentioned in a list of offerings given to the Abbey of St Gall in 1272. While under the Abbey, Gais was a semi-independent village with its own '' Ammann'' (bailiff) and judge. By the 14th century Gais was already acting as an independent community. Under the Ammann Konrad ...
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International Mountains Of Europe
International is an adjective (also used as a noun) meaning "between nations". International may also refer to: Music Albums * ''International'' (Kevin Michael album), 2011 * ''International'' (New Order album), 2002 * ''International'' (The Three Degrees album), 1975 *''International'', 2018 album by L'Algérino Songs * The Internationale, the left-wing anthem * "International" (Chase & Status song), 2014 * "International", by Adventures in Stereo from ''Monomania'', 2000 * "International", by Brass Construction from ''Renegades'', 1984 * "International", by Thomas Leer from ''The Scale of Ten'', 1985 * "International", by Kevin Michael from ''International'' (Kevin Michael album), 2011 * "International", by McGuinness Flint from ''McGuinness Flint'', 1970 * "International", by Orchestral Manoeuvres in the Dark from '' Dazzle Ships'', 1983 * "International (Serious)", by Estelle from '' All of Me'', 2012 Politics * Political international, any transnational organization of ...
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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 ...
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Mountains Of Tyrol (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 and ...
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Mountains Of Bavaria
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 ...
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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 ...
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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 ascensioni ...
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Knorr Hut
The Knorr Hut is a mountain hut belonging to the German Alpine Club and located in the Wetterstein Mountains at a height of 2,052 m. Its lies right on the edge of the ''Zugspitzplatt'' where it drops into the Reintalanger in a location with scenic views and is an important base for hikers who can climb up to it on the normal route from the town of Garmisch-Partenkirchen through the Reintal valley to Germany's highest mountain, the Zugspitze. The Knorr Hut is rated as category I, and belongs to the Munich Section of the German Alpine Club (DAV). History The Knorr Hut was built by 1855 as a small, rude refuge hut, the merchant, Angelo Knorr, contributing ''"a significant sum of money"'' towards it. By 1860 the hut had become run down, because ''"the maintenance of the same had been paid little attention"''. Finally the Munich Section of the newly founded German Alpine Club took over the hut. As well as the section itself, ''"the Royal District Office of Werdenfels, as well a ...
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Wetterstein Limestone
The Wetterstein Formation is a regional geologic formation of the Northern Limestone Alps and Western Carpathians extending from southern Bavaria, Germany in the west, through northern Austria to northern Hungary and western Slovakia in the east. The formation dates back to the Ladinian to Carnian stages of the Late Triassic. The formation is named after the Wetterstein Mountains in southern Germany and northwestern Austria. The center of its distribution, however, is in the Karwendel Mountains. It occurs in the Northern and Southern Limestone Alps and in the Western Carpathians. The formation is composed of mostly reefal limestones and dolomites, the latter the result of widespread diagenesis. In many areas there is a frequent alternation of limestone and dolomite facies. Local variants to indicate the Wetterstein Formation include german: Wettersteinkalk (Wetterstein Limestone), Wettersteindolomit ("Wetterstein Dolomite") and combinations thereof. The Wetterstein Formation rea ...
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