Fiescherhorli
   HOME
*





Fiescherhorli
The Eggishorn is a mountain in the southeastern part of the Bernese Alps, located north of Fiesch in the Swiss canton of Valais. A cable car station is located on a secondary summit named ''Fiescherhorli'' (2,893 m), 500 metres south of the main peak. The Eggishorn lies within the Jungfrau-Aletsch-Bietschhorn region, which in 2001 was designated by UNESCO as a World Heritage Site. On its northern flank is the Aletsch Glacier. From the summit the view extends also to the Lepontine and Pennine Alps (Dom, Matterhorn, Weisshorn). Together with Fiescherhorli and Bettmerhorn, Eggishorn forms a ridge, running in a direction from north-northeast to south-southwest, with steep slopes on both sides, facing Aletsch Glacier in the west and the mountain plateau of Fiescheralpe above the Rhone valley in the east. In terms of its geology, this mountain ridge is part of the metamorphic coat of the granitic Aarmassif; predominant rock types are gneiss and schist. Pictures Image:Aletch ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

List Of Mountains Of Switzerland Accessible By Public Transport
This is a list of mountains of Switzerland above 800 metres whose summits are accessible by public transport. This list includes mountains with a topographic prominence of at least 30 metres that have a station above the height of their key col and within 120 metres (height difference) from the summit. The station can be reached by cable car, funicular, railway or bus. This list notably includes the Klein Matterhorn and the Säntis, respectively the highest and the most prominentInformation retrieved on 5 March 2014 froCore Europe 50 Most Prominent Peaks (peakbagger.com)an/ref> peaks of Europe with public transport access. It also includes the Chasseral, the most isolated summit of the country accessible to pedestrians. This list does not include ski lifts. For a list of ski areas, see List of ski areas and resorts in Switzerland. For a general list of mountains, see List of mountains of Switzerland. List See also *List of aerial tramways in Switzerland *List of funiculars ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Swisstopo
Swisstopo is the official name for the Swiss Federal Office of Topography (in German language, German: ''Bundesamt für Landestopografie''; French language, French: ''Office fédéral de topographie''; Italian language, Italian: ''Ufficio federale di topografia''; Romansh language, Romansh: ''Uffizi federal da topografia''), Switzerland's national mapping agency. The current name was made official in 2002. It had been in use as the domain name for the institute's homepage, swisstopo.ch, since 1997. Maps The main class of products produced by Swisstopo are topographical maps on seven different Scale (map), scales. Swiss maps have been praised for their accuracy and quality. Regular maps * 1:25.000. This is the most detailed map, useful for many purposes. Those are popular with tourists, especially for famous areas like Zermatt and St. Moritz. These maps cost CHF 13.50 each (2004). 208 maps on this scale are published at regular intervals. The first map published on this scale ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Dom (Mischabel)
The Dom is a mountain of the Pennine Alps, located between Randa, Switzerland, Randa and Saas-Fee in the canton of Valais in Switzerland. With a height of , it is the List of Alpine four-thousanders, seventh highest summit in the Alps, overall. Based on topographic prominence, prominence, it can be regarded as the List of prominent mountains of the Alps above 3000 m, third highest mountain in the Alps, and the List of prominent mountains of Switzerland, second highest in Switzerland, after Monte Rosa. The Dom is the main summit of the Mischabel group (German: ''Mischabelhörner''), which is the highest massif lying entirely in Switzerland. The Dom is noteworthy for its 'normal route' of ascent having the greatest vertical height gain of all the alpine 4000 metre peaks, and none of that route's 3,100 metres of height can be achieved using mechanical means. Although ''Dom'' is a German language, German cognate for 'dome', it can also mean 'cathedral' and the mountain is named after ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Cable Cars In Switzerland
Cable may refer to: Mechanical * Nautical cable, an assembly of three or more ropes woven against the weave of the ropes, rendering it virtually waterproof * Wire rope, a type of rope that consists of several strands of metal wire laid into a helix ** Arresting cable, part of a system used to rapidly decelerate an aircraft as it lands ** Bowden cable, a mechanical cable for transmitting forces * Rope generally, especially a thick, heavy ("cable laid") variety Transmission * Electrical cable, an assembly of one or more wires which may be insulated, used for transmission of electrical power or signals ** Coaxial cable, an electrical cable comprising an inner conductor surrounded by a flexible, tubular insulating layer, coated or surrounded by a tubular conducting shield ** Power cable, a cable used to transmit electrical power ** Submarine communications cable, a cable laid on the sea bed to carry telecommunication signals between land-based stations * Fiber-optic cable, a cable co ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Mountains Of Valais
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]  


picture info

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]  


picture info

Schist
Schist ( ) is a medium-grained metamorphic rock showing pronounced schistosity. This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture (geology), texture reflects a high content of platy minerals, such as micas, talc, chlorite group, chlorite, or graphite. These are often interleaved with more granular minerals, such as feldspar or quartz. Schist typically forms during regional metamorphism accompanying the process of mountain building (orogeny) and usually reflects a medium Metamorphism#Metamorphic grades, grade of metamorphism. Schist can form from many different kinds of rocks, including sedimentary rocks such as mudstones and igneous rocks such as tuffs. Schist metamorphosed from mudstone is particularly common and is often very rich in mica (a ''mica schist''). Where the type of the original rock (the protolith) is discernible, the schist is us ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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]  


Aarmassif
The Aarmassif or Aaremassif (German: ''Aarmassiv'') is a geology, geologic massif in the Swiss Alps. It contains a number of large mountain chains and parts of mountain chains. Name The massif is named after the Aar, a river that has its source in the Aarmassif. Geography The Aarmassif outcrop, crops out in the eastern part of the Bernese Alps and the Lepontine Alps, roughly form Leukerbad in the west to the Tödi in the east. Further east the massif only appears in small window (geology), windows like the ''Vättner window'' between Gigerwald and Vättis in Canton of St. Gallen, Sankt Gallen and at the Limmerensee in the same Cantons of Switzerland, canton. Tectonics and lithology The Aarmassif is part of the Helvetic zone of the Alps, which consists of material originally from the European tectonic plate. The Aarmassif has Lithology, lithologies common for Paleozoic basement (geology), basement rocks all over Europe, deformation (geology), deformed and metamorphism, metamorpho ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  




Bettmerhorn
The Bettmerhorn is a mountain of the Bernese Alps, located north of Bettmeralp in the Swiss canton of Valais. The summit can be reached with a 30-minute vertical hike after ascending most of the mountain by cable car from the car free village of Bettmeralp. Bettmeralp is accessible by cable car from the Betten train station (Matterhorn Gotthard Bahn). The Bettmerhorn summit station offers impressive views on the Bernese Alps and the Aletsch Glacier, the largest in the Alps. The view also extends to the Lepontine and Pennine Alps (Dom, Matterhorn, Weisshorn The Weisshorn (German, lit. ''white peak/mountain'') is a major peak of Switzerland and the Alps, culminating at above sea level. It is part of the Pennine Alps and is located between the valleys of Anniviers and Zermatt in the canton of Valai ...). References External links Bettmerhorn cable car Mountains of Valais Mountains of the Alps Tourist attractions in Switzerland Cable cars in Switzerland Bernese Alps ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]