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Strahlkogel SW
The Strahlkogel, at , is the highest peak in the Larstiger Mountains (''Larstiger Berge''), a subgroup of the Stubai Alps in the Austrian state of Tyrol. The Strahlkogel is also the highest mountain in the municipality of Umhausen. Its name comes from its great, white, light-reflecting, quartz layers, which allegedly cause the mountain to "radiate" (''strahlen''). It has the shape of a well-proportioned, steep and pointed pyramid. Ascending the Strahlkogel is difficult and it is thus only rarely visited, unlike the neighbouring 3,287-metre-high Breiter Grieskogel. The first ascent of the mountain was in 1833 by Peter Carl Thurwieser, but his route and the precise circumstances of the climb have not been passed on. On 28 August 1887 Ludwig Purtscheller and Fritz Drasch from Salzburg climbed the mountain. Their route led along the west arête. Today, this is the normal route and easiest way to reach the summit. Area The Strahlkogel lies a good five kilometres as the crow flies no ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Längenfeld
Längenfeld is a municipality and a village the Imst (district) and is located 25 km southeast of Imst in the Ötztal valley, 14 km north of Sölden Sölden is a municipality in the Ötztal valley of Tyrol, Austria. Geography At c. , it is the largest municipality in the country. The population of 3,449 (as of 2003) is outnumbered by tourists, of which 15,000 can be accommodated. With tou .... With an area size of 195.8 km2, 21 village parts and 4333 inhabitants it is the biggest location in the valley. Sights are the late Gothic-baroque church which was built in 1303. The main source of income is tourism. Population Gallery File:Oberlängenfeld, wegpanorama naar Astlehn IMG 0877 2019-07-31 15.51.jpg, Panorama to Astlehn from Oberlängenfeld File:Huben, de Pfarrkirche IMG 0847 2019-07-31 13.49.jpg, Church in Huben File:Dorf, Kapelle Mariahilf Dm13462 IMG 0888 2019-07-31 16.23.jpg, Chapel (Kapelle Mariahilf) in Dorf File:Aschbach, keien bij de Waldwegbr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpine Three-thousanders
Three-thousanders are mountains with a height of between , but less than above sea level. Similar terms are commonly used for mountains of other height brackets e. g. four-thousanders or eight-thousanders. In Britain, the term may refer to mountains above . Climatological significance In temperate latitudes three-thousanders play an important role, because even in summer they lie below the zero degree line for weeks. Thus the chains of three-thousanders always form important climatic divides and support glaciation - in the Alps the contour is roughly the general limit of the "nival step"; only a few glaciated mountains are under (the Dachstein, the easternmost glaciated mountain in the Alps, is, at , not a three-thousander). In the Mediterranean, however, the three-thousanders remain free of ice and, in the tropics, they are almost insignificant from a climatic perspective; here the snow line lies at around to , and in the dry continental areas (Trans-Himalayas, Ande ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpine Club Map
Alpine Club maps (german: Alpenvereinskarten, often abbreviated to ''AV-Karten'' i.e. AV maps) are specially detailed maps for summer and winter mountain climbers (mountaineers, hikers and ski tourers). They are predominantly published at a scale of 1:25.000, although some individual sheets have scales of 1:50.000 and 1:100.000. The cartographic library of the German (DAV) and Austrian Alpine Clubs (OeAV) currently has about 70 different high mountain maps. Also, individual map sheets of the Alpine region or other interesting mountain areas in the world are continually being published. The publication of its maps has been a function of the Alpine Club since 1865. The reason the two clubs still issue their maps is to complement the range of more or less good official maps of the high mountains with special large-scale maps. This is especially true for the Austrian Alpine region, which is the classical field for Alpine Club branches (sections). Here, there are no official maps at a s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpine Club Guide
The ''Alpine Club Guides'' (german: Alpenvereinsführer, commonly shortened to ''AV Führer'' or ''AVF'') are the standard series of Alpine guides that cover all the important mountain groups in the Eastern Alps. They are produced jointly by the German (DAV), Austrian (ÖAV) and South Tyrol Alpine Clubs (AVS). They have been published since 1950 by the firm of Bergverlag Rother in Munich, Germany. The AV guides contain all the routes – hiking trails, mountain hut approaches and summit climbs as well as ice and high mountain routes and ''klettersteigs'' in each mountain range. The descriptions are factual and dry, with few illustrations - rather unlike mountain books by e.g. Walter Pause – and despite introductory sections require general Alpine knowledge and experience. Examples are the ''AVF Allgäuer Alpen'' and the ''AVF Verwallgruppe''.The AV guides are often used as the basis for other publications and complement the Alpine Club maps or other map series. Available guid ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gries Im Sulztal
Gries may refer to: Places *Gries am Brenner, a municipality in Tyrol, Austria *Gries, Bas-Rhin, a municipality in the department Bas-Rhin, France *Gries im Sellrain, a municipality in Tyrol, Austria *Gries, Germany, a municipality in Rhineland-Palatinate, Germany * Gries (Graz), the 5th city district of Graz, Austria * (German: Gries-Quirein), a borough of Bozen-Bolzano, Italy **, Bolzano **Old Parish Church of Gries, Bolzano *Gries Glacier (Griesgletscher), a 5 km long glacier (2005) situated in the Lepontine Alps in the canton of Valais in Switzerland *Gries Pass, a mountain pass in the Alps, between Switzerland and Italy * Corno Gries, a mountain in the Lepontine Alps on the Swiss -Italian border Surname *David Gries (born 1939), computer scientist at Cornell University *Gerhard Gries (born 1955), German ecologist *Jon Gries (born 1957), American actor, writer and director * Moses J. Gries (1866–1918), American rabbi *Peter Gries, Harold J. & Ruth Newman Chair in US-China Is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Climbing Grade
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 ascensi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Tour
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] |
Strahlkogel SW
The Strahlkogel, at , is the highest peak in the Larstiger Mountains (''Larstiger Berge''), a subgroup of the Stubai Alps in the Austrian state of Tyrol. The Strahlkogel is also the highest mountain in the municipality of Umhausen. Its name comes from its great, white, light-reflecting, quartz layers, which allegedly cause the mountain to "radiate" (''strahlen''). It has the shape of a well-proportioned, steep and pointed pyramid. Ascending the Strahlkogel is difficult and it is thus only rarely visited, unlike the neighbouring 3,287-metre-high Breiter Grieskogel. The first ascent of the mountain was in 1833 by Peter Carl Thurwieser, but his route and the precise circumstances of the climb have not been passed on. On 28 August 1887 Ludwig Purtscheller and Fritz Drasch from Salzburg climbed the mountain. Their route led along the west arête. Today, this is the normal route and easiest way to reach the summit. Area The Strahlkogel lies a good five kilometres as the crow flies no ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Divide
An ice divide is the boundary on an ice sheet, ice cap or glacier separating opposing flow directions of ice, analogous to a water divide. Ice divides are important for geochronological investigations that use ice cores, since such coring is typically made at highest point of an ice sheet dome to avoid disturbances arising from horizontal ice movement. Ice divides are used for looking at how the atmosphere varied over time. Coring at dome peaks increases precision of reconstructions as it is the place where horizontal motion is at its least. The Raymond Effect operates at ice divides, creating anticlines in the radar-detected isochrones, allowing greater capture of older ice when coring. Analysis of ice cores relies on the downward motion of ice, trapping changes of atmospheric gases through time into its layers. Scientist locate ice divides and take ice cores from them, which are typically long cylindrical poles of ice, and analyse them to find chemical elements that the snow an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
