Jump to content

Jostedal Glacier

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by 72.161.207.79 (talk) at 02:36, 5 July 2012 (External links). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Jostedalsbreen
Jostedalsbreen glacier
Map showing the location of Jostedalsbreen
Map showing the location of Jostedalsbreen
TypeMountain glacier
LocationSogn og Fjordane, Norway
Area487 km2 (188 sq mi)
Length60 km (37 mi)
Thickness600 m (2,000 ft)

Jostedalsbreen (Template:Lang-en) is the largest glacier in continental Europe. It is situated in Sogn og Fjordane county in Western Norway.[1] Jostedalsbreen lies in the municipalities of Luster, Balestrand, Jølster, and Stryn. The highest peak in the area is Lodalskåpa at a height of 2,083 metres (6,834 ft).

Jostedalsbreen has a total area of 487 square kilometres (188 sq mi). The highest point is Høgste Breakulen at 1,957 metres (6,421 ft) above mean sea level. Branches of the glacier reach down into the valleys, for instance Bøyabreen in Fjærland and Nigardsbreen, both at 300 metres (980 ft) above sea level. The thickest part of the glacier is 600 metres (2,000 ft). Jostedalsbreen has a length of a little more than 60 kilometres (37 mi) and covers over half of the national park which was established in 1991 and covers 1,310 square kilometres (510 sq mi).[1]

The glacier is maintained by the high snowfall rates in the region, not the cold temperatures. This means the glacier has high melting rates in its snouts. The Jostedalsbreen has around 50 glacier arms such as the Nigardsbreen and Tunsbergdalsbreen in Jostedal, the Briksdalsbreen near Olden, the Bøyabreen by Fjærland, the Kjenndalsbreen and Tindefjellbreen near Loen, and Austerdalsbreen.[1]

In 2006, the glacier arm Briksdalsbreen lost 50 metres (160 ft) of ice in a few months. More recent measurements now show that Briksdalsbreen retreated 146 metres (479 ft) in 2006, and could be in danger of breaking away from the upper icefield. Ice climbing has now been terminated because of this event.

See also

References

  1. ^ a b c Luhr, James F., ed. (2003). Illustrated Encyclopedia of the Earth. Dorling Kindersley. ISBN 978-1-4053-3270-5.

Further reading