Aletsch Glacier

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Template:Short description Template:Use dmy dates Template:Infobox glacier The Aletsch Glacier (Template:Langx Template:IPA) or Great Aletsch Glacier (Template:Lang) is the largest glacier in the Alps. It has a length of about Template:Convert (2014),<ref name=ETHZGLAMOS/> a volume of Template:Convert (2011), and covers about Template:Convert (2011) in the eastern Bernese Alps in the Swiss canton of Valais.<ref name=GW>Template:Cite web</ref> The Aletsch Glacier is composed of four smaller glaciers converging at Konkordiaplatz, where its thickness was measured to reach a maximum of Template:Convert.<ref>Template:Cite journal</ref> It then continues towards the Template:Lang valley before giving birth to the Massa. The Aletsch Glacier is – like most glaciers in the world today – a retreating glacier. As of 2016, since 1980 it lost Template:Convert of its length, since 1870 Template:Convert, and lost also more than Template:Convert of its thickness.<ref name=ETHZGLAMOS/>

The whole area, including other glaciers is part of the [[Jungfrau-Aletsch protected area|Template:Lang Protected Area]], which was declared a UNESCO World Heritage Site in 2001.<ref name=GW/><ref name=UNWHC/>

Geography

ISS image of the Bernese Alps showing the Wetterhorn (right), Eiger (centre), Jungfrau (left), Lake Brienz (background) and Aletsch glacier (foreground).

The Aletsch Glacier is one of the many glaciers located between the cantons of Bern and Valais on the Bernese Alps located east of the Gemmi Pass. The whole area is considered to be the largest glaciated area in western Eurasia.<ref name=UNWHC>Template:Cite web</ref> The Fiescher and Aar Glaciers lying on the east have similar extensions.

At Konkordiaplatz
The beginning of the river Massa (the glacier is visible on the right)
View downhill, from the top of Jungfraufirn

Except the Template:Lang, all the highest summits of the Bernese Alps are located within the drainage basin of the glacier. The Template:Lang and Template:Lang constitute the northern boundary; the Template:Lang and Template:Lang lie on its east side; finally the culminating point, the Template:Lang (Template:Convert) is located on the west side.

Before reaching the maximum flow, four smaller glaciers converge at Konkordiaplatz:

South of Konkordiaplatz, the glacier runs towards the valley of the Template:Lang (Upper Valais); on the east side, near Template:Lang, lies a small glacier lake, Template:Lang (Template:Convert); from the western side used to enter the Template:Lang, but since the end of the 20th century the connection with the Aletsch Glacier has been lost. Further down, until about 1880, the Template:Lang did also enter the Aletsch Glacier at its mouth. But since then both glaciers have been retreating so far that they do not connect anymore (the Upper Aletsch Glacier did retreat about Template:Convert from its connecting point with the Aletsch Glacier), but both serve now only as the source of the river Massa. The river flows through the [[Stausee Gibidum|Lake Template:Lang]] (a reservoir, and coincidentally representing the glacier's mouth region in the 19th century, which is a retreat of more than Template:Convert) and a gorge of the same name before reaching the Template:Lang near Template:Lang.

Tourism

The area of the Aletsch Glacier and some surrounding valleys is on the UNESCO World Heritage list, thus it is protected and the facilities are mostly restricted to the external zones. The region between Template:Lang, Template:Lang and Template:Lang (which is called Aletsch Region) in Valais gives access to the lower part of the glacier. The Template:Lang and Template:Lang are popular view points and are accessible by cable car. The Template:Lang river can be crossed since 2008 by a suspension bridge, thus allowing hikes between the left and the right part of the glacier.

The Template:Lang railway station (3,450 m) gives a direct access to the upper Aletsch Glacier as well as the normal route to the Template:Lang. It can be reached only from Template:Lang in the canton Bern. Hiking paths pass the [[Konkordia Hut|Template:Lang Hut]] or the Hollandia Hut, eventually reaching other glaciers in the massif.

On the Template:Lang, at 2,065 metres between Template:Lang and the glacier, is located the historic Villa Cassel, former summer residence of many famous and influential guests from the worlds of politics and finance. The house is now one of the centers of the environmental organization Pro Natura, which hosts a permanent exhibition about the site.<ref>Template:Cite web</ref>

Panorama

[[Image:070915 Panorama Aletschgletscher von Konkordiahütte.jpg|thumb|600px|center|Aletsch Glacier and Template:Lang seen from [[Konkordia Hut|Template:Lang Hut]] (Sept. 2007)]] Also at the mouth of the Template:Lang from the east is the small but important Template:Lang (3 km long and averaging 600 m wide). This firn is connected in the over the glacier pass Template:Lang (3280 m high) to the [[Fiescher Glacier|Template:Lang Glacier]] in the east.

From the Template:Lang, the Aletsch Glacier has a width of approximately 1.5 km and moves at a rate of 180 m per year to the southeast on course with the Template:Lang valley, bordering the Template:Lang in the west and the great Template:Lang in the east. It then takes a great right turn and bends ever closer to the southwest, running through the edge of the Template:Lang and Template:Lang of the Rhône valley. The lowest part of the great Aletsch Glacier is largely covered with detritus of the lateral and medial moraines. The glacier's toe currently lies about 1560 m high, far beneath the local tree line. From it springs the Massa stream, which flows through the Massa Canyon and is used to generate hydroelectric power. It continues through the upper half of the Template:Lang, eventually entering into the Template:Lang.

Aletsch Glacier from Template:Lang (Sept. 2007)

The great Aletsch Glacier shows considerable ice cover. At the Konkordiaplatz, it has an ice cover of more than 900 m, but as it moves to the south, the greater part of the ice melts, gradually decreasing the cover to around 150 m.

The characteristically dark medial moraine, situated almost in the middle of the glacier, runs protracted in two bands from the Template:Lang along the whole length to the glacier's toe-zone. This medial moraine is collected from the ice of three large ice fields, which all run together. The westernmost medial moraine has been named the Template:Lang, and the easternmost carries the name Template:Lang.

Formation and evolution

Slight retreat and some thinning can be seen between 1990 and 2000

The Aletsch Glacier resulted from the accumulation and compaction of snow. Glaciers generally form where snow and ice accumulation exceed snow and ice melt. As the snow and ice thicken it reaches a point where it begins to move due to a combination of gravity and pressure of the overlying snow and ice.

During the last glacial periods, the Aletsch Glacier was much larger than now. 18,000 years ago the lower part of the ridge, between Template:Lang and the glacier, was completely covered by ice. Only the summits of the Template:Lang, Template:Lang and the Template:Lang were above the glacier. After an important retreat, the glacier again advanced 11,000 years ago during the last glacial period. The glacier reached the Rhône valley, and its ice the Template:Lang. Remaining moraines are still visible in the Aletsch Forest.

The retreat of Aletsch Glacier in the Swiss Alps (situation in 1979, 1991 and 2002), due to global warming.

Since the last glaciation, the glacier generally retreated. However slight climatic changes happened and, in 1860, the glacier was 3 km longer and the ice level 200 m higher.<ref>Template:Cite web</ref>

As for many other glaciers, records show a major longer-term retreat trend.<ref name=ETHZGLAMOS>Template:Cite web</ref><ref name=SGMN>Template:Cite web</ref> The Aletsch Glacier receded by Template:Convert since 1870, including Template:Convert since 1980.<ref name=SGMN/> A record retreat of Template:Convert happened in 2006 alone.<ref>Template:Cite news</ref><ref>Template:Cite web</ref>

Since the end of the Little Ice Age in 1850 the glacier has lost 20 percent of its ice mass, considerably less than other glaciers in Switzerland, which have lost up to 50 percent. This is explained with the large size of the Aletsch Glacier, which reacts much slower to climate change than smaller glaciers. It is however estimated that, by 2100, the glacier will have only one tenth of its 2018 ice mass.<ref>Template:Cite news</ref>

Photo opportunity

On August 18, 2007, photographer Spencer Tunick used hundreds of naked people in a "living sculpture" on the Aletsch Glacier in a photo shoot which he said was intended to draw attention to global warming and the shrinking of the world's glaciers. The temperature was about 10 °C (50 °F) at the time of the photo shoot. The 600 participants on the shrinking glacier said that they had volunteered for Tunick (a collaboration with Greenpeace) to let the world know about the effects of global warming on the melting Swiss glaciers.<ref>Template:Cite news</ref>

See also

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Notes and references

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Further reading

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