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Geological Formation

Pasterze Glacier

Glaciers and Ice Formations

The Pasterze is the longest glacier in Austria and the longest glacier in the Eastern Alps, lying in the Glockner Group of the High Tauern range in Carinthia, directly beneath the highest peak in the country, the Grossglockner. As of a 2006 survey it measured about 8.3 kilometers long and covered about 18.5 square kilometers, ranging in elevation from about 3,453 to 2,100 meters with an ice thickness of roughly 120 meters, and it originates below the Johannisberg peak, feeding the Moll river. The glacier is a major tourist destination, reached by the Grossglockner High Alpine Road and a funicular railway, but it is retreating rapidly, its margin having pulled back roughly 300 meters from the lower funicular station since the railway opened in 1963. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Facts
Classification
Protected Status
National Park or Reserve 1
Connections

Caused By

Glaciation, Processes

Wikidata P31 formation-type mapped to formative process Glaciation via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Pasterze Glacier

In Discipline

Wikidata P31 formation-type mapped to discipline Glaciology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Pasterze Glacier
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Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Pasterze Glacier
Sources
1. Pasterze Glacier (Wikipedia)
  • Lead section
    The Pasterze, at approximately 8.4 kilometres (5.2 mi) in length, is the longest glacier in Austria and in the Eastern Alps.
  • Lead
    The surrounding area was purchased by the German and Austrian Alpine Club in 1918; today the glacier is part of the High Tauern National Park.
View the Source
Wikidata: Pasterze Glacier
Wikidata Q684169, class allow-list match (w-wdresolver-0926)View the Source
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