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Former municipality of Switzerland in Bern, Switzerland Gadmen Former municipality of Switzerland Valley of Gadmen Coat of arms Gadmen Location of Gadmen Show map of Switzerland Gadmen Gadmen (Canton of Bern) Show map of Canton of Bern Coordinates: 46°44′N 8°20′E  /  46.733°N 8.333°E  / 46.733; 8.333 Coordinates: 46°44′N 8°20′E  /  46.733°N 8.333°E  / 46.733; 8.333 Country Switzerland Canton Bern District Interlaken-Oberhasli Government  • Mayor Barbara Kehrli Area  • Total 116.4 km 2 (44.9 sq mi) Elevation 1,205 m (3,953 ft) Population (Dec 2011)  • Total 228  • Density 2.0/km 2 (5.1/sq mi) Postal code 3863 SFOS number 0781 Surrounded by Engelberg (OW), Göschenen (UR), Guttannen, Innertkirchen, Oberwald (VS), Wassen (UR) Twin towns Volketswil (Switzerland) Website www.gadmen.ch SFSO statistics Gadmen is a former municipality in the Interlaken-Oberhasli administrative district in the canton of Bern in Switzerland. On 1 January 2014, the former municipality of Gadmen merged

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The Titlis Cliff Walk is a pedestrian bridge along the cliff of Mount Titlis in the Swiss Alps. Built at around 10,000 feet (3,000 m) above sea level, it is believed to be the highest elevation suspension bridge in Europe. [1] [2] It broke the record held by Salbit Bridge, also located in Switzerland. [3] The bridge spans a distance of around 320 feet (98 m) but is just 3 feet (0.91 m) wide. [1] The project was designed as a celebration of the 100th anniversary of the opening of the Engelberg–Gerschnialp funicular railway in January 1913. It was officially opened on 7 December 2012 during a snow storm, leaving dignitaries from 15 countries unable to see more than just a few feet; the public opening occurred a day later. [1] On a clear day, those on the bridge are able to see the glacier 1,500 feet (460 m) below them along with the Uri Alps and parts of Italy. [4] Constructed over a period of five months, the bridge was built when weather conditions permitted. It was designed to wit

This article includes a list of references, but its sources remain unclear because it has insufficient inline citations . Please help to improve this article by introducing more precise citations. (December 2013) (Learn how and when to remove this template message) A partly submerged glacier cave on Perito Moreno Glacier. The ice facade is approximately 60 m high Ice formations in the Titlis glacier cave A glacier cave is a cave formed within the ice of a glacier. Glacier caves are often called ice caves, but the latter term is properly used to describe bedrock caves that contain year-round ice. [1] Contents 1 Overview 2 Examples 3 See also 4 Further reading 5 References 6 External links Overview This glacier cave has been excavated by a hot spring underneath a snow field in south central Iceland, a country where such formations are common due to the high geothermal and volcanic activity, plus the high latitude, cold weather, and frequent snowfall. Most glacier caves are sta

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This article is about the geological formation. For other uses, see Glacier (disambiguation). The Baltoro Glacier in northern Pakistan. At 62 kilometres (39 mi) in length, it is one of the longest alpine glaciers on earth. Eastern face of Kangchenjunga, the third highest mountain in the world, near the Zemu Glacier, in the Himalayan region of Sikkim, India. Ice calving from the terminus of the Perito Moreno Glacier in western Patagonia, Argentina The Aletsch Glacier, the largest glacier of the Alps, in Switzerland The Quelccaya Ice Cap is the second largest glaciated area in the tropics, in Peru A glacier ( US: / ˈ ɡ l eɪ ʃ ər / or UK: / ˈ ɡ l æ s i ər / ) is a persistent body of dense ice that is constantly moving under its own weight; it forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many years, often centuries. Glaciers slowly deform and flow due to stresses induced by their weight, creating crevasses, seracs, and other distinguishing fea