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Gehrenspitze (Allgäu Alps)
At 2,163 metres, the Gehrenspitze is the third highest mountain in the Tannheim Mountains, Tannheim Group and is situated in the Austrian state of Tyrol (Bundesland), Tyrol. It should not be confused with the Gehrenspitze (Wetterstein), Gehrenspitze in the Wetterstein Mountains. Surrounding area The massif of the Gehrenspitze forms the northeastern corner of the Tannheim Valley. East of the Gehrenspitze the terrain descends into the Lech valley towards Reutte. West of the mountain is the Kellenspitze (2,238 m), north of the massif, the Große Schlicke and ''Musauer Berg'' (1,510 m), and, to the south is the ''Schneid'' (2,009 m). Geology Like the Tannheim Mountains, the Gehrenspitze is part of the Northern Limestone Alps, which started to form during the course of Alpine orogeny in the Cretaceous period, about 140 million years ago, a process that has still not quite finished today. The summit of the Gehrenspitze is made of Wetterstein limestone. To the south, somewhat below t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schneid (Tannheim Mountains)
This is an alphabetical list of selected unofficial and specialized terms, phrases, and other jargon used in baseball, along with their definitions, including illustrative examples for many entries. 0–9 0 :"Oh and ..." See #count, count. 1 The number 1 in baseball refers to the pitcher's position, a shorthand call for throwing to first, a single hit, and a fastball sign. 1-2-3 inning :An inning in which a pitcher faces only three batters and none safely reaches a base. "Three up, three down." 1-2-3 double play :A double play in which the pitcher (1) fields a batted ball and throws home to the catcher (2), who retires a runner advancing from third. The catcher then throws to the first baseman (3) to force play, force out the batter. These almost always happen with the bases loaded. 1-6-3 double play :The pitcher (1) fields a batted ball and throws to the shortstop (6) to force out a runner advancing to second. The shortstop then throws to the first baseman ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpine Orogeny
The Alpine orogeny, sometimes referred to as the Alpide orogeny, is an orogenic phase in the Late Mesozoic and the current Cenozoic which has formed the mountain ranges of the Alpide belt. Cause The Alpine orogeny was caused by the African continent, the Arabian Peninsula, the Indian subcontinent, and the Cimmerian plate colliding with Eurasia in the north. Convergent movements between the African, Arabian and Indian plates from the south, and the Eurasian plate and the Anatolian sub-plate from the north – as well as many smaller (micro)plates – had already begun during the early Cretaceous, but the major phases of mountain building began during the Paleocene to the Eocene. The process continues currently in some of the Alpide mountain ranges. The Alpine orogeny is considered one of the three major phases of orogeny in Europe that define the geology of that continent, along with the Caledonian orogeny that formed the Old Red Sandstone Continent when the continents ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Tyrol (federal 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 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 climate, mountains t ... [...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 (2,3 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kompass Karten
Kompass Karten is an Austrian map publisher based in Innsbruck, which specialises in hiking maps, and guides, digital maps, and cycling maps and guides. Its range has over 1,000 titles. History The publishers was founded in December 1953 by Heinz Fleischmann under the name ''Fleischmann KG - KOMPASS Karten'' in Bavaria. In 1968 ''Mairs Geografischer Verlag'' became a shareholder in the firm that now took the name ''Fleischmann & Mair''. In 1996 the publishers became a subsidiary of the publishing group of MairDumont and its name was changed to ''Kompass Karten'' GmbH. Since 2002 the Tyrolean hiking map publishers, ''Walter Mayr'' has been part of KOMPASS Karten. In 2011 the firm had a turnover of around 12 M euros. Products KOMPASS has about 1,000 titles in its programme, including 700 hiking, cycling and ski touring maps. Just under 500 hiking maps have been published covering the hiking areas of Austria, South Tyrol, Germany, the Balearic and Canary Islands. Hik ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nesselwängle
Nesselwängle is a municipality in the district of Reutte in the Austrian state of Tyrol. Geography Nesselwängle lies at the entrance to the Tannheim Valley The Tannheimer Tal ("Tannheim valley") is a high valley, at an elevation of about 1,100 metres, in the Tannheim Mountains, which are part of the Allgäu Alps in the Austrian state of Tyrol (state), Tyrol (Bezirk Reutte, county of Reutte).It is .... References External links Official website Website of the skiing area Nesselwängle Cities and towns in Reutte District {{Tyrol-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Normal Route
A normal route or normal way (; ) is the most frequently used climbing route for ascending and descending a given mountain peak; it is usually the easiest and often the most straightforward route. Other generic names include the ''Tourism, tourist route'' or ''trade route'', and some climbing routes have specific 'normal route' names such as the "Yak Route" on Mount Everest. References Hiking Climbing terminology {{Climbing-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muschelkalk
The Muschelkalk (German for "shell-bearing limestone"; ) is a sequence of sedimentary rock, sedimentary rock strata (a lithostratigraphy, lithostratigraphic unit) in the geology of central and western Europe. It has a Middle Triassic (240 to 230 million years) age and forms the middle part of the three-part Germanic Trias (that gives the Triassic its name) lying above the older Buntsandstein and below the younger Keuper. The Muschelkalk ("mussel-chalk") consists of a sequence of limestone and Dolomite (rock), dolomite Bed (geology), beds. In the past, the time span in which the Muschelkalk was deposited could also be called "Muschelkalk". In modern stratigraphy, however, the name only applies to the layers of rock. Occurrence The name ''Muschelkalk'' was first used by German geologist Georg Christian Füchsel (1722-1773). In 1834, Friedrich August von Alberti included it into the Triassic system (stratigraphy), system. The name indicates a characteristic feature of the unit, name ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Main Dolomite
Main Dolomite (, , ) is a lithostratigraphic unit in the Alps of Europe. Formation was defined by K.W. Gümbel in 1857. Middle to Late Triassic sedimentary record in the Alpine realm is characterized by presence of various masses of dolomitic rock formations. In the Northern Calcareous Alps the dolomitic mass of Ladinian - Norian age is divided by the Carnian sandstones and shales of Lunz Formation to the Ladinian - Carnian Wetterstein Dolomite and Norian Main Dolomite.Tollmann, A., 1976: Analyse des klassischen nordalpinen Mesozoikums, Wien, Franz Deuticke, 580 pp. The Main Dolomite reaches higher thickness than underlying dolomites in Alps, therefore it is considered as more important "Main". Extent The formation is found in: * the Northern Limestone Alps and Southern Limestone Alps of the Limestone Alps, a mountain system of the western and Central Eastern Alps. * the Apennines in Italy * the Western Carpathians (Tatric, Fatric, Hronic, Silicic units) Description It ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Raibl Beds
The Raibl Formation is an Upper Triassic geologic formation in the Northern and Southern Limestone mountain ranges of the Eastern Alps, in Central Europe. Google Books: ''The Geology of Central Europe: Mesozoic and Cenozoic'' edited by Tom McCan; pages 790-797. Description It preserves dating back to the Norian Middle Triassic sub-period of the[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Partnach Gorge
The Partnach Gorge () is a deep gorge that has been incised by a mountain stream, the Partnach, in the Reintal valley near the south German town of Garmisch-Partenkirchen. The gorge is long and, in places, over deep. It was designated a natural monument in 1912. Geology and origin In the Triassic, about 240 million years ago, on the bed of a shallow sea, dark grey, relatively hard layers of Alpine muschelkalk (shell-bearing limestone), so-called ''Wurstelkalk'', were laid down in the area of the present day Partnach Gorge. On the bead-like strata of this rock the traces of the burrowing and feeding of marine animals can still be seen. Importantly, about 5 million years later, softer marls were deposited in the same marine basin, which today are known as Partnach Strata (''Partnach-schichten''). In the course of the subsequent Alpine mountain folding the so-called Warnberg Saddle (''Warnberger Sattel'') was formed from these rock strata. The erosion force of the Partnach ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
