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  • Glacier - GUTH
    DUKAS_16016504_CAT
    Glacier - GUTH
    PIC FROM CATERS NEWS/Eric Guth
    Inside the Mendenhall Glacier in Alaska. The white lines are pressure cracks from the continual strain on the ice.
    Taken in 2007 with a Nikon D200 digital SLR using a Tamron 18-200mm lens at 18mm. SEE CATERS COPY............. (FOTO: DUKAS/CATERSNEWS)

    DUKAS/CATERSNEWS

     

  • Nepal - 2010
    DUKAS_13728442_REX
    Nepal - 2010
    Mandatory Credit: Photo by Ellen Thornell / Rex Features ( 1167172s )
    Mountain view with Glacier near Duglha, Nepal
    Nepal - 2010

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • New Zealand - Mar 2010
    DUKAS_13769714_REX
    New Zealand - Mar 2010
    Mandatory Credit: Photo by Richard Sowersby / Rex Features ( 1168158cg )
    Franz Josef glacier, South Island, New Zealand
    New Zealand - Mar 2010

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • New Zealand - Mar 2010
    DUKAS_13769713_REX
    New Zealand - Mar 2010
    Mandatory Credit: Photo by Richard Sowersby / Rex Features ( 1168158ch )
    Franz Josef glacier, South Island, New Zealand
    New Zealand - Mar 2010

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • New Zealand - Mar 2010
    DUKAS_13769701_REX
    New Zealand - Mar 2010
    Mandatory Credit: Photo by Richard Sowersby / Rex Features ( 1168158ca )
    Franz Josef Glacier, South Island, New Zealand.
    New Zealand - Mar 2010

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • New Zealand - Mar 2010
    DUKAS_13769696_REX
    New Zealand - Mar 2010
    Mandatory Credit: Photo by Richard Sowersby / Rex Features ( 1168158bz )
    Franz Josef Glacier, South Island, New Zealand.
    New Zealand - Mar 2010

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • New Zealand - Mar 2010
    DUKAS_13769694_REX
    New Zealand - Mar 2010
    Mandatory Credit: Photo by Richard Sowersby / Rex Features ( 1168158bx )
    Franz Josef glacier, South Island, New Zealand
    New Zealand - Mar 2010

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • New Zealand - Mar 2010
    DUKAS_13769692_REX
    New Zealand - Mar 2010
    Mandatory Credit: Photo by Richard Sowersby / Rex Features ( 1168158bw )
    Franz Josef Glacier, South Island, New Zealand
    New Zealand - Mar 2010

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • New Zealand - Mar 2010
    DUKAS_13769662_REX
    New Zealand - Mar 2010
    Mandatory Credit: Photo by Richard Sowersby / Rex Features ( 1168158bi )
    A heleicopter flight over Franz Josef glacier, South Island, New Zealand
    New Zealand - Mar 2010

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • Nadine Salzmann
    RDB00391160
    Nadine Salzmann
    FOTO: TOINI LINDROOS, 04.11.2009, ZUERICH, DR.NADINE SALZMANN.- RDB BY DUKAS
    RDB

     

  • VARIOUS
    DUKAS_12527020_REX
    VARIOUS
    Mandatory Credit: Photo by Ashley Cooper / SpecialistStock / SplashdownDirect / Rex Features ( 1048127a )
    the Bernina Glacier express that goes from Chur in Switzerland to Tirano in Italy crossing the famous Landwasser viaduct
    VARIOUS

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • VARIOUS
    DUKAS_12527276_REX
    VARIOUS
    Mandatory Credit: Photo by Ashley Cooper / SpecialistStock / SplashdownDirect / Rex Features ( 1047736a )
    Igloos outside the Arctic Hotel in Ilulissat on Greenland. Ilulissat is a UNESCO World Heritage Site because of the Jacobshavn Glacier or Sermeq Kujalleq which is the largest glacier outside Antarctica. The glacier drains 7% of the Greenland ice sheet and produces enough water from calving icebergs in one day to provide New York with water for 1 year. Climate change has meant the glacier has speeded up and is now one of the fastest glaciers in the world at up to 40 metres per day and is also receeding rapidly
    VARIOUS

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • VARIOUS
    DUKAS_12527199_REX
    VARIOUS
    Mandatory Credit: Photo by Ashley Cooper / SpecialistStock / SplashdownDirect / Rex Features ( 1048269a )
    Igloos outside the Arctic Hotel in Ilulissat on Greenland. Ilulissat is a UNESCO World Heritage Site because of the Jacobshavn Glacier or Sermeq Kujalleq which is the largest glacier outside Antarctica. The glacier drains 7% of the Greenland ice sheet and produces enough water from calving icebergs in one day to provide New York with water for 1 year. Climate change has meant the glacier has speeded up and is now one of the fastest glaciers in the world at up to 40 metres per day and is also receeding rapidly
    VARIOUS

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • VARIOUS
    DUKAS_12527197_REX
    VARIOUS
    Mandatory Credit: Photo by Ashley Cooper / SpecialistStock / SplashdownDirect / Rex Features ( 1048266a )
    Meltwater from the Russell Galcier that drains the Greenland Ice Sheet 26 km inland from Kangerlussuaq. Like most Greenland glaciers it is both receeding and speeding up as a result of global warming and the rivers that drain them are becoming more swollen by greater quantities of melt water
    VARIOUS

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • VARIOUS
    DUKAS_12527118_REX
    VARIOUS
    Mandatory Credit: Photo by Ashley Cooper / SpecialistStock / SplashdownDirect / Rex Features ( 1048185a )
    Lake Emerson on the French Swiss border to generate hydro electric
    VARIOUS

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • VARIOUS
    DUKAS_12526990_REX
    VARIOUS
    Mandatory Credit: Photo by Ashley Cooper / SpecialistStock / SplashdownDirect / Rex Features ( 1048093a )
    The Eqip sermia glacier that is receeding rapidly due to global warming on the west coast of Greenland.
    VARIOUS

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • VARIOUS
    DUKAS_12526895_REX
    VARIOUS
    Mandatory Credit: Photo by Ashley Cooper / SpecialistStock / SplashdownDirect / Rex Features ( 1047987a )
    The view from the summit of the 4000 metre peak of Mont Blanc Du Tacul above Chamonix France
    VARIOUS

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • VARIOUS
    DUKAS_12526869_REX
    VARIOUS
    Mandatory Credit: Photo by Ashley Cooper / SpecialistStock / SplashdownDirect / Rex Features ( 1048515a )
    Icebergs from the Jacobshavn glacier or Sermeq Kujalleq drains 7% of the Greenland ice sheet and is the largest glacier outside of Antarctica. It calves enough ice in one day to supply New York with water for one year. It is one of the fastest moving glaciers in the world at up to 40 metres per day (19 metres per day before 2002) and has also receeded rapidly (40 km since 1850) due to human induced climate change as temperatures have risen in Greenland by 9 degrees fahrenheit in the last 60 years. An underwater moraine at the mouth of the fjord grounds the largest icebergs causing a backlog of ice completely blocking the entire length of the fjord with ice.
    VARIOUS

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • VARIOUS
    DUKAS_12526863_REX
    VARIOUS
    Mandatory Credit: Photo by Ashley Cooper / SpecialistStock / SplashdownDirect / Rex Features ( 1048509a )
    Colourful houses in Illulisat on Greenland. Ilulissat is a UNESCO World Heritage Site because of the Jacobshavn Glacier or Sermeq Kujalleq which is the largest glacier outside Antarctica. The glacier drains 7% of the Greenland ice sheet and produces enough water from calving icebergs in one day to provide New York with water for 1 year. Climate change has meant the glacier has speeded up and is now one of the fastest glaciers in the world at up to 40 metres per day and is also receeding rapidly
    VARIOUS

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • VARIOUS
    DUKAS_12526728_REX
    VARIOUS
    Mandatory Credit: Photo by Ashley Cooper / SpecialistStock / SplashdownDirect / Rex Features ( 1048397a )
    Aialick Glacier in Kenai Fjords National Park in Alaska receeding rapidly due to climate change
    VARIOUS

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • VARIOUS
    DUKAS_12526727_REX
    VARIOUS
    Mandatory Credit: Photo by Ashley Cooper / SpecialistStock / SplashdownDirect / Rex Features ( 1048394a )
    Colourful houses and hospital in Illulisat in the midnight sun on Greenland. Ilulissat is a UNESCO World Heritage Site because of the Jacobshavn Glacier or Sermeq Kujalleq which is the largest glacier outside Antarctica. The glacier drains 7% of the Greenland ice sheet and produces enough water from calving icebergs in one day to provide New York with water for 1 year. Climate change has meant the glacier has speeded up and is now one of the fastest glaciers in the world at up to 40 metres per day and is also receeding rapidly
    VARIOUS

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • VARIOUS
    DUKAS_12526650_REX
    VARIOUS
    Mandatory Credit: Photo by Ashley Cooper / SpecialistStock / SplashdownDirect / Rex Features ( 1048338a )
    The Jacobshavn glacier or Sermeq Kujalleq drains 7% of the Greenland ice sheet and is the largest glacier outside of Antarctica. It calves enough ice in one day to supply New York with water for one year. It is one of the fastest moving glaciers in the world at up to 40 metres per day (19 metres per day before 2002) and has also receeded rapidly (40 km since 1850) due to human induced climate change as temperatures have risen in Greenland by 9 degrees fahrenheit in the last 60 years. An underwater moraine at the mouth of the fjord grounds the largest icebergs causing a backlog of ice completely blocking the entire length of the fjord with ice.
    VARIOUS

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • VARIOUS
    DUKAS_12526634_REX
    VARIOUS
    Mandatory Credit: Photo by Ashley Cooper / SpecialistStock / SplashdownDirect / Rex Features ( 1048321a )
    Igloos outside the Arctic Hotel in Ilulissat on Greenland. Ilulissat is a UNESCO World Heritage Site because of the Jacobshavn Glacier or Sermeq Kujalleq which is the largest glacier outside Antarctica. The glacier drains 7% of the Greenland ice sheet and produces enough water from calving icebergs in one day to provide New York with water for 1 year. Climate change has meant the glacier has speeded up and is now one of the fastest glaciers in the world at up to 40 metres per day and is also receeding rapidly
    VARIOUS

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • VARIOUS
    DUKAS_12526610_REX
    VARIOUS
    Mandatory Credit: Photo by Ashley Cooper / SpecialistStock / SplashdownDirect / Rex Features ( 1048298a )
    A pasrk ranger at Exit Glacier has retreated rapidly due to global warming Kenai Fjords National Park Alaska
    VARIOUS

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • VARIOUS
    DUKAS_12527353_REX
    VARIOUS
    Mandatory Credit: Photo by Ashley Cooper / SpecialistStock / SplashdownDirect / Rex Features ( 1047811a )
    Icebergs from the Jacobshavn glacier or Sermeq Kujalleq drains 7% of the Greenland ice sheet and is the largest glacier outside of Antarctica. It calves enough ice in one day to supply New York with water for one year. It is one of the fastest moving glaciers in the world at up to 40 metres per day (19 metres per day before 2002) and has also receeded rapidly (40 km since 1850) due to human induced climate change as temperatures have risen in Greenland by 9 degrees fahrenheit in the last 60 years. An underwater moraine at the mouth of the fjord grounds the largest icebergs causing a backlog of ice completely blocking the entire length of the fjord with ice.
    VARIOUS

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • VARIOUS
    DUKAS_12527330_REX
    VARIOUS
    Mandatory Credit: Photo by Ashley Cooper / SpecialistStock / SplashdownDirect / Rex Features ( 1047787a )
    Climbers on the 4000 metre peak of Mont Blanc Du Tacul above Chamonix France
    VARIOUS

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • VARIOUS
    DUKAS_12527304_REX
    VARIOUS
    Mandatory Credit: Photo by Nicky Brown / SpecialistStock / SplashdownDirect / Rex Features ( 1047761a )
    Trekkers Nr Everest. On the Low Kumbu Glacier, Nepal
    VARIOUS

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • Mit ReiseBlick in Crans-Montana
    DUKAS_91158190_WIL
    Mit ReiseBlick in Crans-Montana
    Gletscher Plaine Morte.
    CH-Crans-Montana (VS), 10.07.2009
    Foto: Michael Wildi

    DUKAS/Michael Wildi

     

  • Mit ReiseBlick in Crans-Montana
    DUKAS_91158189_WIL
    Mit ReiseBlick in Crans-Montana
    Gletscher Plaine Morte.
    CH-Crans-Montana (VS), 10.07.2009
    Foto: Michael Wildi

    DUKAS/Michael Wildi

     

  • Mit ReiseBlick in Crans-Montana
    DUKAS_91158185_WIL
    Mit ReiseBlick in Crans-Montana
    Gletscher Plaine Morte.
    CH-Crans-Montana (VS), 10.07.2009
    Foto: Michael Wildi

    DUKAS/Michael Wildi

     

  • dukas 91144806 sut
    DUKAS_91144806_SUT
    dukas 91144806 sut
    Chamonix, Mt. Blanc 4810 m, höchchster Berg der Alpen
    DUKAS/Thedi Suter

     

  • Switzerland
    DUKAS_11967762_REX
    Switzerland
    Mandatory Credit: Photo by Patrick Frilet / Rex Features ( 1005143af )

    Switzerland
    THE PICTURE PERFECT BEAUTY OF ZERMATT

    The picture-postcard town of Zermatt is one of Switzerland's best-known ski resorts.

    This charming village is nestled in the upper Valais, one of the alpine cantons of Switzerland, and is around 10 km (6 miles) from the border with Italy.

    Found on a 1,620 m (5,315 ft) high plateau, it sits at the foot of the highest and most photographed peak in the country, the 4,478m (14,692ft) tall Matterhorn.

    This mighty mountain was one of the last alpine peaks to be conquered. And the expedition that did eventually reach the top in 1865 ended dramatically, with only three of the seven climbers surviving the attempt.

    Until the mid-19th century, Zermatt was predominantly an agricultural community - its name, as well as that of the Matterhorn itself, derives from the surrounding alpine meadows, or matten.

    In the German language, the town is "Zur Matte" or "in the meadow."

    Zermatt has the longest winter skiing season in Europe and some of its ski runs and lifts are even open year-round.

    The area boasts some 114 miles of skiing with a 5,315 foot vertical, with most of the skiing being best for intermediate and advanced skiers.

    The village of Zermatt itself is geographically small, with cobbled pedestrian streets and tiny alleyways dating from the middle ages.

    Traditional wooden chalets are a common sight but Zermatt also has a distinctly cosmopolitan, not to mention upmarket, atmosphere

    The village can only be reached via a spectacular cog railway from the valley below.

    This forms part of an extensive network of super-efficient cable cars, gondolas and cog railways that whisk skiers to the separate ski areas.

    To prevent air pollution, which could obscure the panoramic views of the Matterhorn, the entire village is a combustion-engine car-f...
    For more information visit http://www.rexfeatures.com/stacklink/HDBKRRRE

    DUKAS/REX

     

  • Switzerland
    DUKAS_11967738_REX
    Switzerland
    Mandatory Credit: Photo by Patrick Frilet / Rex Features ( 1005143ah )

    Switzerland
    THE PICTURE PERFECT BEAUTY OF ZERMATT

    The picture-postcard town of Zermatt is one of Switzerland's best-known ski resorts.

    This charming village is nestled in the upper Valais, one of the alpine cantons of Switzerland, and is around 10 km (6 miles) from the border with Italy.

    Found on a 1,620 m (5,315 ft) high plateau, it sits at the foot of the highest and most photographed peak in the country, the 4,478m (14,692ft) tall Matterhorn.

    This mighty mountain was one of the last alpine peaks to be conquered. And the expedition that did eventually reach the top in 1865 ended dramatically, with only three of the seven climbers surviving the attempt.

    Until the mid-19th century, Zermatt was predominantly an agricultural community - its name, as well as that of the Matterhorn itself, derives from the surrounding alpine meadows, or matten.

    In the German language, the town is "Zur Matte" or "in the meadow."

    Zermatt has the longest winter skiing season in Europe and some of its ski runs and lifts are even open year-round.

    The area boasts some 114 miles of skiing with a 5,315 foot vertical, with most of the skiing being best for intermediate and advanced skiers.

    The village of Zermatt itself is geographically small, with cobbled pedestrian streets and tiny alleyways dating from the middle ages.

    Traditional wooden chalets are a common sight but Zermatt also has a distinctly cosmopolitan, not to mention upmarket, atmosphere

    The village can only be reached via a spectacular cog railway from the valley below.

    This forms part of an extensive network of super-efficient cable cars, gondolas and cog railways that whisk skiers to the separate ski areas.

    To prevent air pollution, which could obscure the panoramic views of the Matterhorn, the entire village is a combustion-engine car-f...
    For more information visit http://www.rexfeatures.com/stacklink/HDBKRRRE

    DUKAS/REX

     

  • Switzerland
    DUKAS_11967737_REX
    Switzerland
    Mandatory Credit: Photo by Patrick Frilet / Rex Features ( 1005143ag )

    Switzerland
    THE PICTURE PERFECT BEAUTY OF ZERMATT

    The picture-postcard town of Zermatt is one of Switzerland's best-known ski resorts.

    This charming village is nestled in the upper Valais, one of the alpine cantons of Switzerland, and is around 10 km (6 miles) from the border with Italy.

    Found on a 1,620 m (5,315 ft) high plateau, it sits at the foot of the highest and most photographed peak in the country, the 4,478m (14,692ft) tall Matterhorn.

    This mighty mountain was one of the last alpine peaks to be conquered. And the expedition that did eventually reach the top in 1865 ended dramatically, with only three of the seven climbers surviving the attempt.

    Until the mid-19th century, Zermatt was predominantly an agricultural community - its name, as well as that of the Matterhorn itself, derives from the surrounding alpine meadows, or matten.

    In the German language, the town is "Zur Matte" or "in the meadow."

    Zermatt has the longest winter skiing season in Europe and some of its ski runs and lifts are even open year-round.

    The area boasts some 114 miles of skiing with a 5,315 foot vertical, with most of the skiing being best for intermediate and advanced skiers.

    The village of Zermatt itself is geographically small, with cobbled pedestrian streets and tiny alleyways dating from the middle ages.

    Traditional wooden chalets are a common sight but Zermatt also has a distinctly cosmopolitan, not to mention upmarket, atmosphere

    The village can only be reached via a spectacular cog railway from the valley below.

    This forms part of an extensive network of super-efficient cable cars, gondolas and cog railways that whisk skiers to the separate ski areas.

    To prevent air pollution, which could obscure the panoramic views of the Matterhorn, the entire village is a combustion-engine car-f...
    For more information visit http://www.rexfeatures.com/stacklink/HDBKRRRE

    DUKAS/REX

     

  • Switzerland
    DUKAS_11967728_REX
    Switzerland
    Mandatory Credit: Photo by Patrick Frilet / Rex Features ( 1005143ai )

    Switzerland
    THE PICTURE PERFECT BEAUTY OF ZERMATT

    The picture-postcard town of Zermatt is one of Switzerland's best-known ski resorts.

    This charming village is nestled in the upper Valais, one of the alpine cantons of Switzerland, and is around 10 km (6 miles) from the border with Italy.

    Found on a 1,620 m (5,315 ft) high plateau, it sits at the foot of the highest and most photographed peak in the country, the 4,478m (14,692ft) tall Matterhorn.

    This mighty mountain was one of the last alpine peaks to be conquered. And the expedition that did eventually reach the top in 1865 ended dramatically, with only three of the seven climbers surviving the attempt.

    Until the mid-19th century, Zermatt was predominantly an agricultural community - its name, as well as that of the Matterhorn itself, derives from the surrounding alpine meadows, or matten.

    In the German language, the town is "Zur Matte" or "in the meadow."

    Zermatt has the longest winter skiing season in Europe and some of its ski runs and lifts are even open year-round.

    The area boasts some 114 miles of skiing with a 5,315 foot vertical, with most of the skiing being best for intermediate and advanced skiers.

    The village of Zermatt itself is geographically small, with cobbled pedestrian streets and tiny alleyways dating from the middle ages.

    Traditional wooden chalets are a common sight but Zermatt also has a distinctly cosmopolitan, not to mention upmarket, atmosphere

    The village can only be reached via a spectacular cog railway from the valley below.

    This forms part of an extensive network of super-efficient cable cars, gondolas and cog railways that whisk skiers to the separate ski areas.

    To prevent air pollution, which could obscure the panoramic views of the Matterhorn, the entire village is a combustion-engine car-f...
    For more information visit http://www.rexfeatures.com/stacklink/HDBKRRRE

    DUKAS/REX

     

  • Langtang Valley before the Nepal earthquake
    DUKAS_50297048_EYE
    Langtang Valley before the Nepal earthquake
    A Tamang woman in the doorway of a building in Langtang village, Langtang Valley, Nepal, 30th May 2009.

    According to Dorothea Stumm, a glaciologist at the Nepal-based International Centre for Integrated Mountain Development, a massive hanging glacier cracked when an earthquake struck at 11.56am on the 25th April 2015. The ice formed a cloud that gathered snow and rocks and then funnelled down the mountain, burying Langtang village, and creating an enormous pressurised blast. 400 residents of the village and up to 100 trekkers are believed to have been killed.

    © Simon de Trey-White / eyevine

    Contact eyevine for more information about using this image:
    T: +44 (0) 20 8709 8709
    E: info@eyevine.com
    http:///www.eyevine.com (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Langtang Valley before the Nepal earthquake
    DUKAS_50297043_EYE
    Langtang Valley before the Nepal earthquake
    A general view of Langtang Village in the Langtang Valley, Nepal, 30th May 2009

    According to Dorothea Stumm, a glaciologist at the Nepal-based International Centre for Integrated Mountain Development, a massive hanging glacier cracked when an earthquake struck at 11.56am on the 25th April 2015. The ice formed a cloud that gathered snow and rocks and then funnelled down the mountain, burying the village, and creating an enormous pressurised blast. 400 residents of the village and up to 100 trekkers are believed to have been killed.

    © Simon de Trey-White / eyevine

    Contact eyevine for more information about using this image:
    T: +44 (0) 20 8709 8709
    E: info@eyevine.com
    http:///www.eyevine.com (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Langtang Valley before the Nepal earthquake
    DUKAS_50297042_EYE
    Langtang Valley before the Nepal earthquake
    An elderly Tamang woman in a field of millet, Langtang Valley, Langtang region, Nepal, 30th May 2009

    According to Dorothea Stumm, a glaciologist at the Nepal-based International Centre for Integrated Mountain Development, a massive hanging glacier cracked when an earthquake struck at 11.56am on the 25th April 2015. The ice formed a cloud that gathered snow and rocks and then funnelled down the mountain, burying the village, and creating an enormous pressurised blast. 400 residents of the village and up to 100 trekkers are believed to have been killed.

    © Simon de Trey-White / eyevine

    Contact eyevine for more information about using this image:
    T: +44 (0) 20 8709 8709
    E: info@eyevine.com
    http:///www.eyevine.com (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Langtang Valley before the Nepal earthquake
    DUKAS_50297031_EYE
    Langtang Valley before the Nepal earthquake
    Traditional Tibetan dress of a Tamang woman in the Langtang Valley, Nepal, 30th May 2009. The 'Pangden' (striped, woven woollen apron) is belted with an ornate brass belt from which hangs a silver medicine spoon.

    According to Dorothea Stumm, a glaciologist at the Nepal-based International Centre for Integrated Mountain Development, a massive hanging glacier cracked when an earthquake struck at 11.56am on the 25th April 2015. The ice formed a cloud that gathered snow and rocks and then funnelled down the mountain, burying Langtang village, and creating an enormous pressurised blast. 400 residents of the village and up to 100 trekkers are believed to have been killed.

    © Simon de Trey-White / eyevine

    Contact eyevine for more information about using this image:
    T: +44 (0) 20 8709 8709
    E: info@eyevine.com
    http:///www.eyevine.com (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Langtang Valley before the Nepal earthquake
    DUKAS_50297065_EYE
    Langtang Valley before the Nepal earthquake
    Women do their washing in a stream in Langtang Village, Nepal, on the 28th May 2009

    According to Dorothea Stumm, a glaciologist at the Nepal-based International Centre for Integrated Mountain Development, a massive hanging glacier cracked when an earthquake struck at 11.56am on the 25th April 2015. The ice formed a cloud that gathered snow and rocks and then funnelled down the mountain, burying the village, and creating an enormous pressurised blast. 400 residents of the village and up to 100 trekkers are believed to have been killed.

    © Simon de Trey-White / eyevine

    Contact eyevine for more information about using this image:
    T: +44 (0) 20 8709 8709
    E: info@eyevine.com
    http:///www.eyevine.com (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Langtang Valley before the Nepal earthquake
    DUKAS_50297061_EYE
    Langtang Valley before the Nepal earthquake
    80 year old Tshring Zhang Mo, a Tamang woman, pictured in her home in Langtang Village, Langtang Valley, Nepal, 27th May 2009

    According to Dorothea Stumm, a glaciologist at the Nepal-based International Centre for Integrated Mountain Development, a massive hanging glacier cracked when an earthquake struck at 11.56am on the 25th April 2015. The ice formed a cloud that gathered snow and rocks and then funnelled down the mountain, burying the village, and creating an enormous pressurised blast. 400 residents of the village and up to 100 trekkers are believed to have been killed.

    © Simon de Trey-White / eyevine

    Contact eyevine for more information about using this image:
    T: +44 (0) 20 8709 8709
    E: info@eyevine.com
    http:///www.eyevine.com (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Langtang Valley before the Nepal earthquake
    DUKAS_50297059_EYE
    Langtang Valley before the Nepal earthquake
    Female Tamang porters in traditional Tibetan dress having tea in a trailside restaurant in the Langtang Valley, Nepal, 27th May 2009.

    According to Dorothea Stumm, a glaciologist at the Nepal-based International Centre for Integrated Mountain Development, a massive hanging glacier cracked when an earthquake struck at 11.56am on the 25th April 2015. The ice formed a cloud that gathered snow and rocks and then funnelled down the mountain, burying Langtang village, and creating an enormous pressurised blast. 400 residents of the village and up to 100 trekkers are believed to have been killed.

    © Simon de Trey-White / eyevine

    Contact eyevine for more information about using this image:
    T: +44 (0) 20 8709 8709
    E: info@eyevine.com
    http:///www.eyevine.com (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Langtang Valley before the Nepal earthquake
    DUKAS_50297052_EYE
    Langtang Valley before the Nepal earthquake
    Tshring Tamang wearing traditional Tibetan dress splits bamboo, in the Langtang Valley, Nepal, 27th May 2009.

    According to Dorothea Stumm, a glaciologist at the Nepal-based International Centre for Integrated Mountain Development, a massive hanging glacier cracked when an earthquake struck at 11.56am on the 25th April 2015. The ice formed a cloud that gathered snow and rocks and then funnelled down the mountain, burying Langtang village, and creating an enormous pressurised blast. 400 residents of the village and up to 100 trekkers are believed to have been killed.

    © Simon de Trey-White / eyevine

    Contact eyevine for more information about using this image:
    T: +44 (0) 20 8709 8709
    E: info@eyevine.com
    http:///www.eyevine.com (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Langtang Valley before the Nepal earthquake
    DUKAS_50297049_EYE
    Langtang Valley before the Nepal earthquake
    A steaming stainless steel mug in a kitchen of a trailside restaurant in the Langtang Valley, Nepal, 27th May 2009.

    According to Dorothea Stumm, a glaciologist at the Nepal-based International Centre for Integrated Mountain Development, a massive hanging glacier cracked when an earthquake struck at 11.56am on the 25th April 2015. The ice formed a cloud that gathered snow and rocks and then funnelled down the mountain, burying Langtang village, and creating an enormous pressurised blast. 400 residents of the village and up to 100 trekkers are believed to have been killed.

    © Simon de Trey-White / eyevine

    Contact eyevine for more information about using this image:
    T: +44 (0) 20 8709 8709
    E: info@eyevine.com
    http:///www.eyevine.com (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Langtang Valley before the Nepal earthquake
    DUKAS_50297046_EYE
    Langtang Valley before the Nepal earthquake
    Female Tamang porters in traditional Tibetan dress walk together carrying loads in the Langtang Valley, Nepal, 27th May 2009. The 'Pangden' (striped, woven woollen apron) is belted with an ornate brass belt at the waist from which hangs a silver medicine spoon.

    According to Dorothea Stumm, a glaciologist at the Nepal-based International Centre for Integrated Mountain Development, a massive hanging glacier cracked when an earthquake struck at 11.56am on the 25th April 2015. The ice formed a cloud that gathered snow and rocks and then funnelled down the mountain, burying Langtang village, and creating an enormous pressurised blast. 400 residents of the village and up to 100 trekkers are believed to have been killed.

    © Simon de Trey-White / eyevine

    Contact eyevine for more information about using this image:
    T: +44 (0) 20 8709 8709
    E: info@eyevine.com
    http:///www.eyevine.com (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • 2008-07-24: Einsamer Wanderer am Eisfjord von Ilulissat (Gršnland, UNESCO-Welterbe). Die im Fjord langsam vorbeiziehenden Eisberge stammen vom Ilulissat-Gletscher, dem aktivsten Gletscher der nšrdlichsten HemisphŠre. Er bewegt sich mit bis zu einem Mete
    DUKAS_19384333_WAL
    2008-07-24: Einsamer Wanderer am Eisfjord von Ilulissat (Gršnland, UNESCO-Welterbe). Die im Fjord langsam vorbeiziehenden Eisberge stammen vom Ilulissat-Gletscher, dem aktivsten Gletscher der nšrdlichsten HemisphŠre. Er bewegt sich mit bis zu einem Mete
    2008-07-24: Einsamer Wanderer am Eisfjord von Ilulissat (Gršnland, UNESCO-Welterbe). Die im Fjord langsam vorbeiziehenden Eisberge stammen vom Ilulissat-Gletscher, dem aktivsten Gletscher der nšrdlichsten HemisphŠre. Er bewegt sich mit bis zu einem Meter pro Stunde vorwŠrts, und durch diese Bewegung brechen an seiner Front tŠglich 20 Millionen Tonnen Eis ab - das entspricht dem Wasservolumen, das die Metropole New York in einem Jahr verbraucht! FOTO: DUKAS/SANDRA WALSER
    DUKAS/SANDRA WALSER DUKAS

     

  • Anniverary of the first ascent of Mount Everest
    DUKAS_52834211_PSO
    Anniverary of the first ascent of Mount Everest
    File image dated 24/09/2007 of the summit of Mount Everest (centre peak) in Nepal. The 29th May is the anniversary of the first ascent of the mountain by a British expedition led by Col John Hunt. Climbers Tenzing Norgay and Edmund Hillary reached the summit on the 29th May 1953. News of their achievement arrived on the day Queen Elizabeth II was crowned in the same year. (FOTO: DUKAS/PHOTOSHOT)
    DUKAS/PHOTOSHOT

     

  • Canada Global Warming in the Arctic Circle
    DUKAS_3305537_WPN
    Canada Global Warming in the Arctic Circle
    The landscape of Resolute Bay in Nunavut, Canada, in the Canadian High Arctic region, reveals a patch of water in June 2007. The area has become a hotbed of scientific environmental study, as the lakes, ponds, and other bodies of water are responding to recent climate warming in the region.
    There is various evidence observed in the Canadian High Arctic region to suggest that ecological changes are occurring at a noticeable rapid pace and could be attributed to global warming. Scientists are observing a greater amount of fresh water surface melt from the outlying tidewater glaciers, a possible result of lengthened melt seasons, averaging over 5 more days per decade. Image data from a time span of under 50 years reveals a 2.4% reduced surface area of the Devon Island Ice Cap. American scientists report that the Arctic ice is currently the smallest it had for the last century. Also, temperatures are being recorded well above the seasonal averages for the last half century, sometimes over 10 degrees Fahrenheit (or between 3 and 6 degrees Celsius).
    In addition to rapidly melting ice and decreased surface areas, both the danger to familiar animal species (polar bears and caribou), and the emergence of new ones (mosquitoes, dolphins, robins, and finches), are further indications that the region is experiencing environmental conditions it has not previously known.
    (FOTO: DUKAS/WORLDPICTURENEWS)

    DUKAS/WPN

     

  • Canada Global Warming in the Arctic Circle
    DUKAS_3305507_WPN
    Canada Global Warming in the Arctic Circle
    The landscape of Devon Island in Nunavut, Canada, in the Canadian High Arctic region, stretches out bright and clear in June 2007. Devon Island is the largest uninhabited island in the world, 500 kilometers southwest of the North Pole. The area has become a hotbed of scientific environmental study, as the lakes, ponds, and other bodies of water are responding to recent climate warming in the region.
    There is various evidence observed in the Canadian High Arctic region to suggest that ecological changes are occurring at a noticeable rapid pace and could be attributed to global warming. Scientists are observing a greater amount of fresh water surface melt from the outlying tidewater glaciers, a possible result of lengthened melt seasons, averaging over 5 more days per decade. Image data from a time span of under 50 years reveals a 2.4% reduced surface area of the Devon Island Ice Cap. American scientists report that the Arctic ice is currently the smallest it had for the last century. Also, temperatures are being recorded well above the seasonal averages for the last half century, sometimes over 10 degrees Fahrenheit (or between 3 and 6 degrees Celsius).
    In addition to rapidly melting ice and decreased surface areas, both the danger to familiar animal species (polar bears and caribou), and the emergence of new ones (mosquitoes, dolphins, robins, and finches), are further indications that the region is experiencing environmental conditions it has not previously known.
    (FOTO: DUKAS/WORLDPICTURENEWS)

    DUKAS/WPN

     

  • Canada Global Warming in the Arctic Circle
    DUKAS_3305503_WPN
    Canada Global Warming in the Arctic Circle
    The landscape of Devon Island in Nunavut, Canada, in the Canadian High Arctic region, reveals a patch of in June 2007. Devon Island is the largest uninhabited island in the world, 500 kilometers southwest of the North Pole. The area has become a hotbed of scientific environmental study, as the lakes, ponds, and other bodies of water are responding to recent climate warming in the region.
    There is various evidence observed in the Canadian High Arctic region to suggest that ecological changes are occurring at a noticeable rapid pace and could be attributed to global warming. Scientists are observing a greater amount of fresh water surface melt from the outlying tidewater glaciers, a possible result of lengthened melt seasons, averaging over 5 more days per decade. Image data from a time span of under 50 years reveals a 2.4% reduced surface area of the Devon Island Ice Cap. American scientists report that the Arctic ice is currently the smallest it had for the last century. Also, temperatures are being recorded well above the seasonal averages for the last half century, sometimes over 10 degrees Fahrenheit (or between 3 and 6 degrees Celsius).
    In addition to rapidly melting ice and decreased surface areas, both the danger to familiar animal species (polar bears and caribou), and the emergence of new ones (mosquitoes, dolphins, robins, and finches), are further indications that the region is experiencing environmental conditions it has not previously known.
    (FOTO: DUKAS/WORLDPICTURENEWS)

    DUKAS/WPN

     

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