Английская Википедия:Gorner Glacier
Шаблон:Short description Шаблон:Redirect Шаблон:Infobox glacier
The Gorner Glacier (Шаблон:Lang-de) 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 Шаблон:Convert long (2014) and Шаблон:Convert wide. The entire glacial area of the glacier related to Gorner Glacier is Шаблон:Convert (2007),[1] which makes it the second largest glacial system in the Alps after the Aletsch Glacier system; however, in length it ranks third behind the Aletsch and Fiescher Glaciers. Numerous smaller glaciers connect with the Gorner Glacier. Its (former) tributaries are (clockwise on this map) the Gorner Glacier (after which the whole system is named, although the upper part is now disconnected from the lower part), Monte Rosa Glacier, Grenzgletscher (nowadays by far its main tributary, now disconnected from the Gorner Glacier proper[2]), Zwillingsgletscher, Schwärzegletscher, Breithorngletscher, Triftjigletscher, and Unterer Theodulgletscher (the last three now disconnected).
The Grenzgletscher (Шаблон:Lang-en) between the central Monte Rosa massif and the Liskamm to the south is nowadays the main contributor to the lower Gorner Glacier. The Gorner Glacier's upper part is almost already disconnected from its lower part. The former tributaries Breithorngletscher, Triftjigletscher, and Unterer Theodulgletscher lost their connections to the Gorner Glacier during the twentieth century; the Unterer Theodulgletscher became disconnected in the 1980s.
A notable feature of this glacier is the Gornersee, an ice marginal lake at the confluence area of the Gorner Glacier and Grenzgletscher. This lake fills every year and drains in summer, usually as a glacial lake outburst flood. This is one of only a few glacial lakes in the Alps exhibiting this behavior.
There are also notable 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 affected the more exposed surrounding ice.
The glacier is the source of the river Шаблон:Ill, 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 (Шаблон:Convert), connected from Zermatt by the Gornergrat Railway.
Glacial retreat
Like almost all other glaciers in the Alps, and most glaciers on the globe as well, the Gorner Glacier is retreating as a result of global warming—in this case, dramatically so. As of 2014, Gorner Glacier had been retreating about Шаблон:Convert every year, but with a record loss of Шаблон:Convert in 2008. Since its last major expansion (in the modern era, after the last glacial period) in 1859, it had lost more than Шаблон:Convert in distance.[3]
As of about 2015, the Gorner Glacier had retreated to the point where it lost touch with its main tributary: the Grenzgletscher (Шаблон:Lang-en) on the south side of the Monte Rosa massif. The Gorner Glacier proper is found on the north side. Now the prominent flow visible from Gornergrat is properly called the Grenzgletscher and can no longer be considered part of the Gorner Glacier. The Monte Rosa Glacier in the middle has also lost touch with the Gorner Glacier. This can be seen in a comparison of photographs over the years:
See also
References
External links
- Gorner Glacier glaciology.ethz.ch
- Gorner Glacier swisseduc.ch
Шаблон:Matter Valley Шаблон:Authority control
