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Morteratsch Glacier

Morteratsch Glacier


The Morteratsch Glacier (romansh: Vadret da Morteratsch) is the largest glacier by area in the Bernina Range of the Bündner Alps in Switzerland.

It is, just after Pasterze Glacier and Gepatschferner, the third largest and by volume (1.2 km³) the most massive glacier in the eastern alps. The Morteratsch Glacier is a typical valley glacier with a pronounced ice front. The accumulation zone lies between the peaks of Piz Morteratsch, Piz Bernina, Crast' Agüzza, Piz Argient, Piz Zupò and Bellavista. From Piz Argient to the ice front in the Val Morteratsch, its horizontal extent is about approx. 7 km, with an altitude difference of up to 2,000 m. Together with the Pers Glacier, originating at Piz Palü, which joins the Morteratsch just below the rock formation Isla Persa ("Lost Isle"), it covers an area of about 16 km². The volume of the ice is estimated to be about 1.2 km³. The Morteratsch Glacier drains through Inn River and Danube into the Black Sea.

View of the Morteratsch Glacier from the ski run


In spring, depending on the snow conditions, a 10 km long ski-run accessible to skilled skiers is marked on the glacier. It leads from the Diavolezza aerial tramway terminus to the Morteratsch inn and has an altitude difference of 1100 m. Along the run, which takes about 1-2 hours, spectacular panoramic views of the glacier and the valley arise. The RhB Station Morteratsch used to be situated directly at the ice front of the glacier. The ice front has receded over 1800 m in the meantime, and cannot be seen from the station today.

Yearly length change measurements have been recorded since 1878. For the period to 1998, the overall retreat was over 1.8 km with a mean annual retreat rate of approximately 17.2 m/y. This long-term average has markedly increased in recent years, receding 30 m/y from 1999-2005. Substantial retreat was ongoing through 2006 as well.[1]

During the time that measurements have been taken, the glacier has advanced a few meters in only four years. Since the large glaciers react slowly to short-term climate changes, these advances cannot be accounted for by increased precipitation in the accumulation zone. On the high morraines to the left and right of the ice front, which are still nearly free of overgrowth, the enormous quantities of ice which were still being pushed down here at the end of the "Little Ice Age" in the middle of the 19th century can be seen.

 

 



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