Grosser Aletschgletscher

Grosser Aletschgletscher is by far the longest glacier in the Alps. From head to toe it measures 22 km. The glacier descends from the summits of Jungfrau and Mönch to only 1700 m above sea level.

Konkordiaplatz

Grosser Aletschgletscher comprises of three different glaciers at its top. Grosser Aletschfirn is coming from the southwest, Jungfraufirn from the northwest and Ewigschneefäld from the north. They merge at Konkordiaplatz, an enormous ice field at 2700 m. There, the ice is an impressive 800 m thick, more than anywhere in the Alps.

Satellite imagery of Grosser Aletschgletscher, August 2023. Source: Sentinel-2 via Copernicus Browser.
Satellite imagery of Grosser Aletschgletscher, August 2023. Source: Sentinel-2 via Copernicus Browser.
Grosser Aletschgletscher, juni 2020.
Grosser Aletschgletscher, juni 2020.
The glacier's two medial moraines run over its full length.
The glacier's two medial moraines run over its full length.

Medial Moraines

All three glaciers scrape the valley sides. Falling rocks land on the sides of the glacier and are transported down. Where the glaciers converge, their sides become the middle part. Suddenly, the rocks on top of the glacier are no longer at the edge, but form a trail of debris at the seam. These lines of rocks are called medial moraines and run all the way to the glacier’s snout, as conveyor belts. At Grosser Aletschgletscher, the ice moves at 150 m per year.

Viewpoint Eggishorn

From Konkordiaplatz downwards, the Grosser Aletschgletscher changes its direction from southeast to southwest. At its outer bend stand mountains of 3000 m high and one of them is accessible by cable car. A short hike brings you to the top of Eggishorn, from where you can see the entire Grosser Aletschgletscher.

Grosser Aletschgletscher from the Eggishorn, June 2020.
Grosser Aletschgletscher from the Eggishorn, June 2020.
Märjelensee in 1897. The trimline at the valley side marks the maximum water level. Photographer: University of Lausanne, Library ETH Zürich Hs_1458-GK-B005-1897-0001.
Märjelensee in 1897. The trimline at the valley side marks the maximum water level. Photographer: University of Lausanne, Library ETH Zürich Hs_1458-GK-B005-1897-0001.

Märjelensee

The chain of mountains along Grosser Aletschgletscher’s outer bend is interrupted by the Märjela valley. Back in the days, when Aletschgletscher was much thicker, the ice dammed this valley. Water couldn’t escape Märjela and formed an ice-dammed lake. Ice bergs calved into it, making it a popular destination.

Märjelensee in 1865. Photographer: Adolphe Braun, Library ETH Zürich Hs_1458-GK-B005-1865.
Märjelensee in 1865. Photographer: Adolphe Braun, Library ETH Zürich Hs_1458-GK-B005-1865.
Location where Grosser Aletschgletscher used to dam Märjela valley.
Location where Grosser Aletschgletscher used to dam Märjela valley.

Fifty Meters Annually

Grosser Aletschgletscher is shrinking since 1870. It receded by 3.5 km and its surface has lowered by hundreds of meters. Over the course of this 150 year period the melt rates have increased considerably. While the glacier used to lose 10 to 20 meters annually, it now recedes at least 50 meters every year.

Aletschgletscher in 1942Aletschgletscher 2020

Grosser Aletschgletscher in 1942 (left) and 2020. Photograph 1942: Leo Wehrli, Library ETH Zürich Dia_247-13519.

Konkordiaplatz, 2015Konkordiaplatz, 2023

View over Konkordiaplatz from the Konkordiahütte in 2015 (left) and 2023. Source: fotowebcam.eu.

Step by Step

By melting so much, Grosser Aletschgletscher lost its connection with Oberalteschgletscher and Mittelaletschgletscher (upper and middle Aletschgletscher) already a long time ago. Glacial thinning also makes glacier hikes increasingly difficult, because accessing the glacier gets harder. This is best illustrated at the Konkordiahütte, a mountain hut right above Konkordiaplatz. When the hut was built, it was almost at the same level as the glacier. But nowadays, the gap in elevation is bridged by a long series of ladders. Every few years a new one has to be added, until the valley floor is reached.

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