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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- Satellite image - Mýrdalsjökull Ice Cap, south Iceland - Clic to enlarge -
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Satellite image - Mýrdalsjökull Ice Cap, south Iceland - Clic to enlarge

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- Satellite image - Kronebreen, Svalbard - Clic to enlarge -
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Satellite image - Kronebreen, Svalbard - Clic to enlarge

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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)

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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- Satellite image - Helheim Glacier, South-east Greenland - Clic to enlarge -
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Satellite image - Helheim Glacier, South-east Greenland - Clic to enlarge

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- Satellite image - Kangerdlugssuaq Glacier, eastern Greenland - Clic to enlarge -
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Satellite image - Kangerdlugssuaq Glacier, eastern Greenland - Clic to enlarge

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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

Totten Glacier
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Totten Glacier, Budd Coast of Wilkes Land, Australian Antarctica.

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- Satellite image - Totten Glacier, Australian Antarctica - Clic to enlarge -
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Satellite image - Totten Glacier, Australian Antarctica - Clic to enlarge

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- Satellite image - Wilczek Land Ice Cap, Franz Josef Archipelago - Clic to enlarge -
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Satellite image - Wilczek Land Ice Cap, Franz Josef Archipelago - Clic to enlarge

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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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- Satellite image - Wilczek Land Ice Cap, Franz Josef Archipelago - Clic to enlarge -
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Satellite image - Wilczek Land Ice Cap, Franz Josef Archipelago - Clic to enlarge

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- Satellite image - Belcher Glacier, Canada - Clic to enlarge -
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Satellite image - Belcher Glacier, Canada - Clic to enlarge

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Belcher Glacier
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Belcher Glacier, Devon Ice Cap, Devon Island, Canada.

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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- Satellite image - Astrolabe Glacier, Adelie Land, French Antarctica - Clic to enlarge -
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Satellite image - Astrolabe Glacier, Adelie Land, French Antarctica - Clic to enlarge

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- Satellite image - Barnard Glacier, Alaska - Clic to enlarge -
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Satellite image - Barnard Glacier, Alaska - Clic to enlarge

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Barnard Glacier
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Barnard Glacier is a 53-km-long (33 mi) glacier in the U.S. state of Alaska. It trends southwest to the Chitina River east of Hawkins Glacier, 64 km (40 mi) southeast of McCarthy in the Saint Elias Mountains.

The glacier is named for United States Geological Survey surveyor Edward Chester Barnard (1863–1921), Commissioner for the United States for the defining and marking of the boundary between Alaska and Canada.

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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- Satellite image - Mc Murdo Dry Valleys, Antarctica - Clic to enlarge -
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Satellite image - Mc Murdo Dry Valleys, Antarctica - Clic to enlarge

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- Mount Erebus - Clic to enlarge -
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Mount Erebus - Clic to enlarge

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Mount Erebus
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Mount Erebus, Antarctica. Located on Ross Island, Mount Erebus is the southernmost active volcano on Earth. Discovered on January 27, 1841 by Sir James Clark Ross, it now faces the McMurdo research station. Mount Erebus is 3794 m high. 
 
Source: wiki / Global Volcanism Program

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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- Satellite image - Hofsjökull Ice Cap, Iceland - Clic to enlarge -
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Satellite image - Hofsjökull Ice Cap, Iceland - Clic to enlarge

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- Satellite image, SPOT 5 3D - Northern Patagonian Ice Field, Chile - Clic to enlarge -
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Satellite image, SPOT 5 3D - Northern Patagonian Ice Field, Chile - Clic to enlarge

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Northern Patagonian Ice Field
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Northern Patagonian Ice Field, Chile. SPOT 5 3D View over a portion of the Northern Patagonian Icefield in the Chilean Patagonia. Background, the San Valentín (also named San Clemente) Mount, the highest mountain of the Chilean Patagonia (4070m) and also the highest mountain south of 40°S, apart from the Antarctic ranges. Halfway, the accumulation areas of the two largest glaciers of the ice cap, San Rafael and San Quintín, which have shown a fast acceleration of their retreating and shrinking in the past decades. Foreground, the San Quintín glacier, which terminus is a piedmont lobe just short of the Golfo de Penas on the Pacific Ocean.

Source: wiki / USGS

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