Holzleiten Saddle
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Holzleiten Saddle
The Holzleiten Saddle (german: Holzleitensattel, ) is a mountain pass between Nassereith and Obsteig in the Austrian state of Tyrol. The B 189 runs over the saddle and is about 25 km long. It is the only important and very busy link from the Inn valley to the Fern Pass. Whilst it ascends gradually in the east over the Mieming Plateau {{Coord, 47, 19, N, 10, 59, E, type:mountain_region:AT-7_dim:15000_map:right_maptype: relief, display=title The Mieming Plateau (german: Mieminger Plateau) is a mountain terrace between 850 and 1000 metres high above the Upper Inn valley in th ..., the saddle drops relatively steeply in the west into the Gurgltal (ca. ). Its maximum gradient is 12 %. The saddle is named after the scattered hamlet (''Rotte'') of Holzleiten (municipality of Obsteig), which is located near the summit of the pass. References {{Austrian mountain passes Mountain passes of the Alps Mountain passes of Tyrol (state) ...
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Tyrol (Bundesland)
Tyrol (; german: Tirol ; it, Tirolo) is a state (''Land'') in western Austria. It comprises the Austrian part of the historical 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 stands to the east, while on the south Tyrol has a border with the 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 the west. In the north, it adjoins to the German state of Ba ...
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Mieming Chain
The Mieming(er) Range, Mieminger Chain (german: Mieminger Kette) or Mieminger Mountains (''Mieminger Gebirge''), is a mountain range of the Northern Limestone Alps in the Eastern Alps. It is located entirely in Austria within the state of Tyrol. This sub-group is somewhat in the shadows of its more famous neighbour, the Wetterstein to the north. Whilst the region around the Coburger Hut and the lakes of Seebensee and Drachensee in the west ( Ehrwalder Sonnenspitze and Vorderer Tajakopf with its new ''klettersteig'' over the Tajakante) and the Hohe Munde in the extreme east receive large numbers of visitors, the less developed central area remains very quiet. The Hohe Munde is also a popular and challenging ski touring destination. Public transport links: The Außerfern Railway stops at Ehrwald on the western side of the range. Busses run from Leutasch on the southern side of the mountains to Mittenwald and Seefeld in Tirol. Geology The Mieminger Mountains lie in a partic ...
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Mountain Pass
A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the world's mountain ranges have presented formidable barriers to travel, passes have played a key role in trade, war, and both Human migration, human and animal migration throughout history. At lower elevations it may be called a hill pass. A mountain pass is typically formed between two volcanic peaks or created by erosion from water or wind. Overview Mountain passes make use of a gap (landform), gap, saddle (landform), saddle, col or notch (landform), notch. A topographic saddle is analogous to the mathematical concept of a saddle surface, with a saddle point marking the highest point between two valleys and the lowest point along a ridge. On a topographic map, passes are characterized by contour lines with an hourglass shape, which indicates a low spot between two higher points. In the high mountains, a difference of between the summit and the mountain is defined as a mountain pas ...
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Nassereith
Nassereith is a municipality and a village in the Imst district of Austria and is located 11 km north of Imst on the upper course of the Gurgl brook The Gurglbach is a river of Tyrol, Austria. The Gurglbach originates on the rock face near Nassereith. It flows from west to east to Tarrenz, the only village that it passes completely through. There, it changes its route and flows south to Imst .... The village was mentioned in documents for the first time in 1150 but settlement had already began 200-300BC. The main source of income is tourism but Nassereith is now also a community for commuters. Population Gallery File:Dormitz, dorpszicht foto1 2012-08-14 18.31.jpg, Dormitz, view to the village File:Dormitz, die Wahlfahrtskirche Dm799 foto6 2012-08-15 09.33.jpg, Dormitz, church / Wahlfahrtskirche File:Tussen Nassereith en Dormitz, panorama foto2 2012-08-15 10.04.JPG, between Nassereith and Dormitz, panorama File:Nassereith, Pfarrkirche hl. Drei König Dm779 2012-08-15 ...
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Obsteig
Obsteig is a municipality in the Imst district and is located 15 km northeast of Imst and 3 km above Mötz. The village has 14 parts and is a popular area for skiing Skiing is the use of skis to glide on snow. Variations of purpose include basic transport, a recreational activity, or a competitive winter sport. Many types of competitive skiing events are recognized by the International Olympic Committee (IO .... Main sources of income is Winter tourism. Population References External links Cities and towns in Imst District {{Tyrol-geo-stub ...
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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 ...
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Inn Valley
, image = UnterinntalWest.JPG , image_caption = Lower Inn valley from Rattenberg castle , source1_location = Swiss Alps (Lägh dal Lunghin) , source1_elevation = , source1_coordinates= , mouth_location = Danube (Passau) , mouth_elevation = , mouth_coordinates = , progression = , subdivision_type1 = Countries , subdivision_name1 = , subdivision_type2 = Cities , subdivision_name2 = , length = , discharge1_location= mouth , discharge1_avg = , basin_size = The Inn ( la, Aenus; rm, En) is a river in Switzerland, Austria and Germany. The river is long. It is a right tributary of the Danube and it is the third largest tributary of the Danube by discharge. The highest point of its drainage basin is the summit of Piz Bernina at . The Engadine, the valley of the En, is the only Swiss valley whose waters end up in the Black Sea (via the Danube). Etymology The name Inn is derived from the old Celtic words ''en'' and ''enios'', ...
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Fern Pass
Fern Pass (elevation 1212 m) is a mountain pass in the Tyrolean Alps in Austria. It is located between the Lechtal Alps on the west and the Mieming Mountains on the east. The highest peak in Germany, the Zugspitze is only 13.5 km away to the northeast. The pass lies between the Grubigstein (2233 m) on the northwest, the Wannig (2493 m) on the southeast, and the Loreakopf (2471 m) on the west. History The pass was created when a huge mountain slide (actually the collapse of an entire mountain, with an estimated volume of 1 km3; the third-largest mountain slide ever in the eastern Alps) filled part of the valley to a height of 300–400 meters, distributing its boulders up to 16 km away. While it was initially believed that this had happened at least 12,000 years B.P. as a consequence of the strong temperature increase and intense run-off after the end of the last deglaciation, pollen analysis performed as early as 1940 had already indicated an age of not much ...
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Mieming Plateau
{{Coord, 47, 19, N, 10, 59, E, type:mountain_region:AT-7_dim:15000_map:right_maptype: relief, display=title The Mieming Plateau (german: Mieminger Plateau) is a mountain terrace between 850 and 1000 metres high above the Upper Inn valley in the Austrian state of Tyrol at the southern foot of the Mieming Chain. It lies in the municipalities of Wildermieming, Mieming, Obsteig and Mötz. The low mountain terrace is composed of ground moraines and gravels, probably from the Würm glaciation. In the south the terrace is bounded by the so-called Achberg range (''Achbergzug''), a chain of mountains made of main dolomite, the other side of which is the Inn valley. The plateau is about 14 kilometres long and up to 4 kilometres wide. Except near Telfs and Mötz it drops steeply 200 metres down to the Inn valley and ends in the west at the Holzleiten Saddle, where the road continues to the Gurgltal and the Fern Pass section. From Telfs and Mötz there are transit rout ...
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Mountain Passes Of The Alps
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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