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Zwölferkogel (Stubai Alps)
The Zwölferkogel is a mountain, , in the Stubai Alps in the Austrian state of Tyrol. Topography The Zwölferkogel lies about 2.7 kilometres south of the winter sport resort of Kühtai. The northwest face of the Zwölferkogel falls around 500 metres into the ''Längental'' valley. To the east below the ''Finstertal'' is the ''Finstertalspeicher'', a reservoir belonging to the Sellrain-Silz Power Station. To the south, along a sharp arête, are the ''Mittagsköpfe'' (), the ''Mittagsturm'' tower () and the Sulzkogel The Sulzkogel is a mountain, , in the Stubai Alps in the Austrian state of Tyrol. Topography The Sulzkogel lies about 3.5 kilometres south of the winter sports resort of Kühtai. To the west a sharp arête drops away from the summit of the Sulz ... (). Gallery File:Sulzkogel und Zwölferkogel.jpg, The Zwölferkogel behind the dam wall of the ''Finstertalspeicher'' File:Zwölferkogel im Kühtai.jpg, The Zwölferkogel References External links {{DEFA ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sulzkogel
The Sulzkogel is a mountain, , in the Stubai Alps in the Austrian state of Tyrol. Topography The Sulzkogel lies about 3.5 kilometres south of the winter sports resort of Kühtai. To the west a sharp arête drops away from the summit of the Sulzkogel into the valley of ''Längental'', separating the cirques of ''Mittagskar'' in the northwest and ''Stierkar'' in the south. To the northeast below the steep northeast face and east arête lies the ''Finstertal'' valley and the ''Finstertalspeicher'', a reservoir belonging to the Sellrain-Silz Power Station. To the north along a sharp arête are the ''Mittagsturm'' pinnacle (), the twin peaks of the ''Mittagsköpfe'' ( and ) and the Zwölferkogel (). To the south is the ''Gamskogel'' (). Between the Sulzkogel and the Gamskogel below a wide rocky ridge lies the Gamskogelferner, a glacier that descends to an elevation of . Paths The normal route, in winter a popular ski tour, runs up the northern edge of the Gamskogelferner glacier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stubai Alps
The Stubai Alps (in German ''Stubaier Alpen'') is a mountain range in the Central Eastern Alps of Europe. It derives its name from the Stubaital valley to its east and is located southwest of Innsbruck, Austria. Several peaks form the border between Austria and Italy. The range is bounded by the Inn River valley to the north; the Sill River valley (''Wipptal'') and the Brenner Pass to the east (separating it from the Zillertal Alps); the Ötztal and Timmelsjoch to the west (separating it from the Ötztal Alps), and to the south by tributaries of the Passer River and Eisack. Geography Important parts of the Stubai Alps show signs of glaciation. The northern part around the Sellrain valley and the Kühtai is now only lightly glaciated and a popular ski touring destination ( Zischgeles, Lampsenspitze, Pirchkogel, Sulzkogel). The High Stubai around the upper Stubai valley is still heavily glaciated and a classic high mountain touring region in the Eastern Alps. Here there is a glacie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kühtai
Kühtai is a winter sports village in the Stubai Alps on the Kühtai Saddle between the Nedertal valley in the west and the Sellrain valley in the east. It is part of the municipality of Silz, in the district of Imst, in the Austrian state of Tyrol. Location and population The village is located at a height of around 2,020 metres and is one of the highest ski resorts in Austria. History Originally there was a ' here, the ''Chutay'' ("cow alp"). This was first mentioned around 1280 in an urbarium of the counts of Tyrol. In 1497 the later Emperor Maximilian I was give the right to hunt in the area of the Kühtai. In 1622, Archduke Leopold V had the ''schwaighof'' converted into a hunting lodge and, in 1624, a road was built from Sellrain. Emperor Franz Joseph I bought the hunting lodge back in 1893 and used it as a base for hunting Alpine marmots. The property passed via his granddaughter, Hedwig to the counts of Stolberg-Stolberg, who turned it into ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tyrol (state)
Tyrol (; german: Tirol ; it, Tirolo) is a States of Austria, state (''Land'') in western Austria. It comprises the Austrian part of the historical County of Tyrol, Princely County of Tyrol. It is a constituent part of the present-day Euroregion Tyrol–South Tyrol–Trentino (together with South Tyrol and Trentino in Italy). The capital of Tyrol is Innsbruck. Geography The state of Tyrol is separated into two parts, divided by a strip. The larger territory is called North Tyrol (''Nordtirol'') and the smaller area is called East Tyrol (''Osttirol''). The neighbouring Austrian state of Salzburg (state), Salzburg stands to the east, while on the south Tyrol has a border with the Italy, Italian province of South Tyrol (Trentino-Alto Adige/Südtirol) which was part of the Austro-Hungarian Empire before the First World War. With a land area of , Tyrol is the third-largest state in Austria. Tyrol shares its borders with the federal state of Salzburg in the east and Vorarlberg in th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gneiss
Gneiss ( ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage. Gneisses are common in the ancient crust of continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture ... [...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] |
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] |
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] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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