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Hexenkopf
The Hexenkopf is a mountain, , in the Samnaun Group in the Alps in the Austrian state of Tyrol. Location and surrounding area The Hexenkopf lies on the northern chain of the Samnaun Group between the valleys of Paznauntal in the north and Oberinntal in the south. Its neighbouring peak to the west is the 2,914 m high ''Gmaierkopf''; to the south, separated by the Hexen Saddle, is the 2,828 m high Masnerkopf. To the southeast is the ''Masneralpe'', which has been developed for winter sports by the Serfaus-Fiss-Ladis ski region. The Hexensee Hut (2,588 m) on the lake of ''Hexensee'' is one of the most important bases for an ascent of the Hexenkopfs. In the east the 2,685 m high ''Masnerjoch'' col separates the Hexenkopf from the 2,845 m high ''Arrezkopf''; this chain runs eastwards to the 3,004 m high Furgler. To the north another ridge to the ''Plattkopf'' (2,893 m) separates the alpine meadows of ''Hinterflathalpe'' in the west from ''Ber ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains Of The Alps Above 3000 M
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] |
Samnaun Group
The Samnaun Alps are a mountain range of the Central Eastern Alps, named after the Swiss municipality of Samnaun. They are located at the border of the Austrian state of Tyrol and the Graubünden canton of Switzerland. The Samnaun Alps are separated from the Sesvenna Alps in the south by the Engadine Valley; from the Silvretta Alps in the west by the Fimber Pass; from the Verwall Alps and the Lechtal Alps in the north by the Paznauntal; from the Ötztal Alps in the east by the Inn valley. All the range is drained by the river Inn, through the Trisanna, Schergenbach, Brancla and Fimbabach. Peaks The range includes the following peaks: For a list of passes, see Passes of the Silvretta and Rätikon Ranges. Muttler vom Alptrider Sattel 2.jpg, Muttler from north Silvretta-Grenzstelle-A-CH-Fimbatal-(1980).jpg, Fimbatal border crossing Switzerland and Austria Piz Rots.JPG, Piz Rots in the skiarea Silvretta Arena Samnaungruppe, Piz Mundin, Muttler.JPG, Piz Mundin and Muttler ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Furgler
The Furgler (also ''Großer Furgler'', ) is one of the most visited mountains of the Samnaun Alps in the Austrian state of Tyrol. The tourist resort of Serfaus, which is in the immediate vicinity, is often selected as the start point for tours of the mountain. Ascents The ski area of Serfaus-Fiss-Ladis runs close to the mountain, which makes it much easier to climb. Start points here are the middle or top stations of the Komperdell lift on the Lazidkopf. An ascent from the lift may be made on one of two waymarked paths: *The northern route runs from the middle station (1,980 m) along the long-distance path no. 702 past the Furglersee (2,458 m), westwards through the Furgler valley, over the Furglerjoch col (2,748 m) and along the north arête to the summit cross. *The southern route runs from the ''Lassida'' top station (2,351 m) over the Böderköpfe to the Scheid (2,429 m), continues to the Tieftalsee lake (2,783 m) and circumnavigates this ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Top Station
A top station or upper stationFor example, se''Chairlift Blausee (upper station)''at www.outdooractive.com. Retrieved 15 May 2019. is usually the highest station of an aerial lift, a funicular, a T-bar lift or a rack railway. The lowest station is the valley station. Passengers or skiers usually alight at the top station. Top stations on a cable car may be ordinary buildings with a docking bay or open steel structures. Gondola lifts have horizontally arranged top stations. The top stations on chair lifts may have a simple jump-off point or a more substantial design. Gallery File:Dachstein-berg2.jpg, Dachstein cable car, Austria File:Saentis-Gebaeude.jpg, The ''Saentisbahn'', Switzerland File:Mount Roberts Tramway in Juneau, Alaska.jpg, Mount Roberts Tramway, Juneau, Alaska File:Telecabina Masada.JPG, Masada cableway, Israel File:10_Sommet_TS.JPG, Top station of a simple chair lift File:Bergstation Carmenna.jpg, Top station of the Aroser Weisshorn, Carmenna Chairlift, Arosa File ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Amphibolite
Amphibolite () is a metamorphic rock that contains amphibole, especially hornblende and actinolite, as well as plagioclase feldspar, but with little or no quartz. It is typically dark-colored and dense, with a weakly foliated or schistose (flaky) structure. The small flakes of black and white in the rock often give it a salt-and-pepper appearance. Amphibolite frequently forms by metamorphism of mafic igneous rocks, such as basalt. However, because metamorphism creates minerals entirely based upon the chemistry of the protolith, certain 'dirty marls' and volcanic sediments may also metamorphose to an amphibolite assemblage. Deposits containing dolomite and siderite also readily yield amphibolite (tremolite-schist, grunerite-schist, and others) especially where there has been a certain amount of contact metamorphism by adjacent granitic masses. Metamorphosed basalt (metabasalt) creates ''ortho-amphibolite'' and other chemically appropriate lithologies create ''para-amphibolite''. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deutscher Alpenverein
The German Alpine Club (german: links=no, Deutscher Alpenverein, DAV for short) is the world's largest climbing association and the eighth-largest sporting association in Germany. It is a member of the German Olympic Sports Confederation and the competent body for sport and competition climbing, hiking, mountaineering, hill walking, ice climbing, mountain expeditions, as well as ski mountaineering. It is an association made up of local branches known as 'sections'. History The German Alpine Club was founded as on 9 May 1869 in Munich by 36 former members of the Austrian Alpine Club around the Ötztal curate Franz Senn. It was founded in order to promote the development of tourism in the Eastern Alps through the building of mountain huts, and establishment of hiking trails, and via ferratas. The association had a large membership from the beginning, attracting 1,070 members in the first ten months. The German and the Austrian societies merged in 1873 to form the German and Aus ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Österreichischer Alpenverein
The Austrian Alpine Club (german: Österreichischer Alpenverein) has about 573,000 members in 196 sections and is the largest mountaineering organisation in Austria. It is responsible for the upkeep of over 234 alpine huts in Austria and neighbouring countries. It also maintains over 26,000 kilometres of footpaths, and produces detailed maps of key mountain areas within Austria. Much of this work is done by the association's 22,000 volunteers. The association has a museum in Innsbruck dedicated to the history of alpinism. It also has sections in Belgium and the United Kingdom, and a group in Poland. See also * South Tyrol Alpine Club (Alpenverein Südtirol, AVS) * German Alpine Club The German Alpine Club (german: links=no, Deutscher Alpenverein, DAV for short) is the world's largest climbing association and the eighth-largest sporting association in Germany. It is a member of the German Olympic Sports Confederation and the ... (Deutscher Alpenverein, DAV) References E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpenverein Südtirol
The South Tyrol Alpine Club (german: Alpenverein Südtirol), abbreviated AVS, is an association of German and Ladin-speaking mountain climbers in South Tyrol, northern Italy. Founded in 1946, it is sub-divided into 32 sections and 58 local divisions. The AVS is based in Bolzano and has more than 60,000 members. History Originally, the South Tyrolean alpine club sections were members of the German and Austrian Alpine Club (''Deutscher und Österreichischer Alpenverein''). In 1869 the first sections were founded in Bozen and Niederdorf, Puster Valley. By 1910, 15 more sections had been established in South Tyrol. They initiated the construction of 19 mountain huts, an extensive network of paths through the mountains and training for mountain guides. After the end of the First World War, the annexation of South Tyrol by Italy and the coming into power of the fascists, the South Tyrolean sections were disappropriated and banned in 1923 (see Italianization of South Tyrol). After th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waymarked
Trail blazing or way marking is the practice of marking paths in outdoor recreational areas with signs or markings that follow each other at certain, though not necessarily exactly defined, distances and mark the direction of the trail. A blaze in the beginning meant "a mark made on a tree by slashing the bark" (''The Canadian Oxford Dictionary''). Originally a waymark was "any conspicuous object which serves as a guide to travellers; a landmark" (''Oxford English Dictionary''). There are several ways of marking trails, including paint, carvings, affixed markers, posts, flagging, cairns, and crosses, with paint being the most widely used. Types of signage Paint A painted marking of a consistent shape or shapes (often rectangular), dimension and colour or combination of colours is used along the trail route. The system by which blazes are used to signify turns and endpoints in trails (see below) strongly favors the use of paint blazes. European countries usually use systems ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Serfaus
Serfaus is a municipality in the district of Landeck in the Austrian state of Tyrol. It is well known as part of the ski-region "Serfaus-Fiss-Ladis", which was formed when Serfaus teamed up with the two nearby municipalities of Fiss and Ladis in 1999. Serfaus is also known for its small hovertrain subway system, the U-Bahn Serfaus. With four stations and a length of 1280 m (the second-shortest underground train line in the world) it allows for a complete ban of cars within the town, while at the same time maintaining the village's attractiveness to tourists, particularly skiers. Geography Serfaus is a small town located on a plateau 500m above the upper Inn valley in Tyrol, western Austria. Above the town a high ridge rises, linking Mount Furgler (3004 metres above sea level) with Mount Schönjoch (2491m). On the opposite side of the valley is a 20 km-long ridge named Glockturmkamm with Pfroslkopf peak (3148m). History The oldest evidence of civilisation in the region ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granitic
A granitoid is a generic term for a diverse category of coarse-grained igneous rocks that consist predominantly of quartz, plagioclase, and alkali feldspar. Granitoids range from plagioclase-rich tonalites to alkali-rich syenites and from quartz-poor monzonites to quartz-rich quartzolites. As only two of the three defining mineral groups (quartz, plagioclase, and alkali feldspar) need to be present for the rock to be called a granitoid, foid-bearing rocks, which predominantly contain feldspars but no quartz, are also granitoids. The terms ''granite'' and ''granitic rock'' are often used interchangeably for granitoids; however, granite is just one particular type of granitoid. Granitoids are diverse; no classification system for granitoids can give a complete and unique characterization of the origin, compositional evolution, and geodynamic environment for the genesis of a granitoid. Accordingly, multiple granitoid classification systems have been developed such as those based ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
