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Gornergrat railway station

Gornergrat Railway stationsRailway stations in Switzerland opened in 1898Railway stations in the canton of ValaisSwiss railway station stubs
Gornergrat railway station
Gornergrat railway station

Gornergrat is the upper terminal railway station of the Gornergrat railway, a rack railway which links it with the resort of Zermatt. The station is situated at the summit of the Gornergrat, in the Swiss municipality of Zermatt and canton of Valais. At an altitude of 3,089 m (10,135 ft) above mean sea level, it is the highest open-air railway station in Europe.Near the station is the Kulm Hotel, a hotel and observatory.

Excerpt from the Wikipedia article Gornergrat railway station (License: CC BY-SA 3.0, Authors, Images).

Gornergrat railway station
Gornergrat - Hohtälli,

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Latitude Longitude
N 45.983333333333 ° E 7.7822222222222 °
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Gornergrat

Gornergrat - Hohtälli
3920
Wallis, Switzerland
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Gornergrat railway station
Gornergrat railway station
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Gorner Glacier
Gorner Glacier

The Gorner Glacier (German: Gornergletscher) is a valley glacier found on the west side of the Monte Rosa massif close to Zermatt in the canton of Valais, Switzerland. It is about 12.4 km (7.7 mi) long (2014) and 1 to 1.5 km (0.62 to 0.93 mi) wide. The entire glacial area of the glacier related to Gorner Glacier is 53 km2 (20 sq mi) (2007), which makes it the second largest glacial system in the Alps after the Aletsch Glacier system; however it ranks only third in length behind the Aletsch and Fiescher Glacier, respectively. Numerous smaller glaciers connect with the Gorner Glacier. Its (former) tributaries are (clockwise on this map): Gornergletscher (after which the whole system is named, but the upper part is now disconnected from the lower part), Monte Rosa Gletscher, Grenzgletscher (nowadays by far its main tributary, now disconnected from the actual Gornergletscher), Zwillingsgletscher, Schwärzegletscher, Breithorngletscher, Triftjigletscher, and Unterer Theodulgletscher (although the last three ones are actually disconnected now). The Grenzgletscher (English: Border Glacier) between the central Monte Rosa massif and the Liskamm to the south is nowadays by far the lower Gorner Glacier's main tributary. The Gorner Glacier's upper part is almost already disconnected from its lower part. Also the former tributaries Breithorngletscher, Triftjigletscher, and Unterer Theodulgletscher lost their connections to the Gorner Glacier during the last century; the Lower Theodul Glacier became disconnected in the 1980s. An interesting feature of this glacier is the Gornersee, an ice marginal lake at the confluence area of the Gorner- and Grenzgletscher. This lake fills every year and drains in summer, usually as a Glacial lake outburst flood. This is one of few glacial lakes in the Alps exhibiting this kind of behavior. There are also several interesting surface features including crevasses and "table top" forms where large surface boulders have been left stranded above the glaciers surface. These tabular rocks are supported by ice that the boulder has sheltered from melting that has effected the more exposed surrounding ice. Due to the immense information about the glacier, it is perfect for a glacier project. It is the source of the river Gornera, which flows down through Zermatt itself. However, most of its water is captured by a water catchment station of the Grande Dixence hydroelectric power plant. This water then ends up in the Lac des Dix, the main reservoir of Grande Dixence. The glacier as well as the surrounding mountains can be seen from the Gornergrat (3,100 m or 10,200 ft), connected from Zermatt by the Gornergrat Railway.