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Leutasch Gorge
The Leutasch Gorge (german: Leutaschklamm or ''Leutascher Geisterklamm'') is a gorge near Mittenwald and Unterleutasch in the Bavarian-Tyrolean border area through which the Leutascher Ache river flows. It is very steep-sided and was not opened to tourists until 2006. To do this a 1.4 million euro, EU-supported, Austro-German project was undertaken to build steel walkways and bridges over a distance of 970 metres. With a total length of 1,650 metres it is the longest accessible gorge in the Eastern Limestone Alps. The gorge was opened on 24 May 2006. Marketing As a tourist project the gorge was marketed as the so-called ''Geisterklamm'' ("Spirit Gorge"), in conjunction with the ''Koboldpfad'' ("Kobold Path") as a family-friendly leisure paradise. There are 40 boards with information on myths, geology, flora and fauna in the surround area, as well as a spirit with winking eyes and coloured, sound-oriented games. The walkways are horizontal wherever possible and are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Innsbruck
Innsbruck (; bar, Innschbruck, label=Bavarian language, Austro-Bavarian ) is the capital of Tyrol (state), Tyrol and the List of cities and towns in Austria, fifth-largest city in Austria. On the Inn (river), River Inn, at its junction with the Wipptal, Wipp Valley, which provides access to the Brenner Pass to the south, it had a population of 132,493 in 2018. In the broad valley between high mountains, the so-called North Chain in the Karwendel Alps (Hafelekarspitze, ) to the north and Patscherkofel () and Serles () to the south, Innsbruck is an internationally renowned winter sports centre; it hosted the 1964 Winter Olympics, 1964 and 1976 Winter Olympics as well as the 1984 Winter Paralympics, 1984 and 1988 Winter Paralympics. It also hosted the first 2012 Winter Youth Olympics, Winter Youth Olympics in 2012. The name means "bridge over the Inn". History Antiquity The earliest traces suggest initial inhabitation in the early Stone Age. Surviving Ancient Rome, pre-Roman pla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Limestone Alps
The Northern Limestone Alps (german: Nördliche Kalkalpen), also called the Northern Calcareous Alps, are the ranges of the Eastern Alps north of the Central Eastern Alps located in Austria and the adjacent Bavarian lands of southeastern Germany. The distinction from the latter group, where the higher peaks are located, is based on differences in geological composition. Geography If viewed on a west–east axis, the Northern Limestone Alps extend from the Rhine valley and the Bregenz Forest in Vorarlberg, Austria in the west extending along the border between the German federal-state of Bavaria and Austrian Tyrol, through Salzburg, Upper Austria, Styria and Lower Austria and finally ending at the Wienerwald at the city-limits of Vienna in the east. The highest peaks in the Northern Limestone Alps are the Parseierspitze () in the Lechtal Alps,Reynolds, Kev (2010). ''Walking in the Alps'', Cicerone, . and the Hoher Dachstein (). Other notable peaks in this range include the Zugs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Tyrol (state)
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Bavaria
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyons And Gorges Of Germany
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyons And Gorges Of Austria
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hammersbach (Grainau)
Hammersbach (758 m above sea level) is a village in the municipality of Grainau at the foot of the Wetterstein Mountains in South Germany. It is located at the southwestern end of the market town of Garmisch-Partenkirchen and is an important base for tours by mountaineers and hikers. There is a halt on the Bavarian Zugspitze Railway and Eibsee bus within the parish, which runs from Garmisch-Partenkirchen to the Eibsee. Summits From Hammersbach the following summits may be ascended by experienced Alpinists: *Waxenstein (2,277 m) *Alpspitze (2,628 m) via the ''Höllentorkopf'' and Osterfelderkopf or ''Matheisenkar'' cirque and ''Grieskarscharte'' col *Zugspitze (2,962 m) through the Höllental valley and over the Höllentalferner Trails *Eibsee Circular Trail (''Eibsee-Rundweg''): From Hammersbach along the ridgeway (''Höhenweg'') to the Eibsee Hotel, then around the Eibsee lake and back (ca. 15 km/height difference 500 m) * Höllental valley via the Höllental entrance h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grainau
Grainau is a municipality in the district of Garmisch-Partenkirchen, in southern Bavaria, Germany. It is located at the foot of the Zugspitze mountain, the tallest mountain in Germany in the sub-mountain range of the Wetterstein Alps which is a branch off the main mountain range it is connected to, the Alps. Lake Eibsee in Grainau lies at the foot of the Zugspitze surrounded by forest. Geography Grainau lies at the foot of the Zugspitze in the Wetterstein Mountains. It is part of the seven municipalities of the former County of Werdenfels, along with Garmisch-Partenkirchen, Farchant, Mittenwald, Krün and Wallgau. Grainau is also home to two mountain lakes, the Badersee and the Eibsee. Waxenstein mountain sits to the south, while the Kramerspitz mountain and Ammergau Alps sit to the north. The district of Grainau is made up of: * Obergrainau (parish village) * Untergrainau and Hammersbach (church village) * Schmölz (village) * Eibsee (hamlet) Notable people * Lorenz ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Höllental Gorge
Hell Valley or Valley of Hell may refer to: * Höllental (Black Forest), a deep valley in the state of Baden-Württemberg, Germany ** Hell Valley Railway, a line that runs through the valley * Höllental (Franconian Forest), a protected nature reserve in Bavaria, Germany * Höllental (Lower Austria), a valley in the Alps along the River Schwarza * Höllental (Wetterstein), a mountain path up the Zugspitze on the German-Austrian border * Val d'Enfer, a valley in Provence, France * ''The Valley of Hell'' (film), a 1927 American Western * Thermal Valley, Taiwan See also * Heil Valley Heil Valley () is an ice-free valley, long, that indents the northern part of V-shaped Mount Littlepage in the Head Mountains of Victoria Land. Named by the Advisory Committee on Antarctic Names in 2007 after Joseph J. Heil III, supervisor of the ..., Victoria Land, Antarctica * Hill Valley (other) {{Disambiguation, geo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Partnach Gorge
The Partnach Gorge (german: Partnachklamm) 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, 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 str ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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