The IPY - SPIRIT image gallery
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Mýrdalsjökull Ice Cap
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Mýrdalsjökull, south Iceland, “the ice cap in the marsh valley”.
The ice-cap covers an active volcano called Katla. The crater of the volcano has a diameter of 10 km and the volcano erupts normally every 40 - 80 years.
As the last eruption took place in 1918, scientists are monitoring the volcano very carefully. Since 930, 16 eruptions have been documented.
Source: wiki
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Kronebreen
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Kronebreen, Svalbard, tidewater 42km-long glacier with a drainage basin of approx. 600 km²
source : UNIS (University of Svalbard) |
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Helheim Glacier
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Helheim Glacier, South-east Greenland.
The Helheim glacier's rate of flow has increased from 8 km per year (5 miles per year) in 2000 to 11 km per year (6.8 miles per year) in 2005. In addition to flowing more rapidly the glacier thinned by 40 meters (130 feet) between 2001 and 2003.
The calving front of the glacier has retreated by approximately 5 km (3.1 miles).
Source: Geophysical Research Letters, Ian Howat, I. Joughin, S. Tulaczyk, and S. Gogineni.
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Kangerdlugssuaq Glacier
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Kangerdlugssuaq Glacier, eastern Greenland
Its rate of flow more than doubled between 2000 and 2005 reaching a speed of 14 km per year (1.6 meters per hour).
It had been retreating 25 to 100 meters per year in the period between 1992 and 2000, retreated more than 4 km between April 2004 and April 2005.
Source: UNEP Atlas |
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Totten Glacier
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Totten Glacier, Budd Coast of Wilkes Land, Australian Antarctica. |
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Wilczek Land Ice Cap
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Wilczek Land Ice Cap, the second largest island of the Franz Josef Archipelago. It is almost completely glaciarized.
The highest point is 606m.
Source: Wiki
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Astrolabe Glacier
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Astrolabe Glacier, Adelie Land, French Antarctica. The glacier is 6 km wide and 16 km long. Its tongue is 4.8km wide and 6km long. |
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Dry Valleys
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Dry Valleys, Antarctica. The McMurdo Dry Valleys are located within Victoria Land, west of McMurdo Sound, Antarctica. Their name is due to the extremely low humidity and their lack of snow or ice cover, which place the region as one of the world’s most extreme deserts. These conditions are caused by katabatic winds, which can reach 320 km/h, evaporating all moisture, ice and snow.
Source: wiki |
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Hofsjökull Ice Cap
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Hofsjökull Ice Cap, Iceland. Hofsjökull is the third largest ice cap in Iceland and covers a subglacial volcano. The maximum altitude of the ice surface is 1800m.
Source: IWA Publishing online |
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