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64 Ergebnis(se) in 4 ms

  • Surface Tension: Greenland Ice Images.
    DUKAS_4512745_EYE
    Surface Tension: Greenland Ice Images.
    The edge of a glacier on Greenland where it meets the fjord which will take bergs and ice towards the sea. The bright blue patches are the underlying ice core exposed by 'calving' pieces that drop into the fjord forming bergs. Greenland.

    (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Surface Tension: Greenland Ice Images.
    DUKAS_4512723_EYE
    Surface Tension: Greenland Ice Images.
    The glacier close to the town of Narsaq often visited as a tourist spot. Greenlanders ocasionally take tourists to see the glacier. Testimony from locals suggests that the edge of the glacier has retreated. Quotes available. The bright blue patches are the underlying ice core exposed by 'calving' pieces that drop into the fjord forming bergs.

    (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Surface Tension: Greenland Ice Images.
    DUKAS_4512718_EYE
    Surface Tension: Greenland Ice Images.
    The Greenlandic town of Narsaq partially visible through a small wind blown opening in a large ice berg floating in the town's bay. The photographer approached the berg on a small inflatable boat. The drip above the town is from the berg as it slowly melts in the warmer Greenlandic summer season.

    (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Surface Tension: Greenland Ice Images.
    DUKAS_4512711_EYE
    Surface Tension: Greenland Ice Images.
    'Slab' Icebergs viewed across the bay from the Greenlandic town of Narsaaq. This one is .75 Kilometre long. It will drift further out into the Atlantic ocean, eventually melting in the warmer currents.

    (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Surface Tension: Greenland Ice Images.
    DUKAS_4512705_EYE
    Surface Tension: Greenland Ice Images.
    An iceberg weathered spectacularly by the wind. Fierce winds whip across the entrance to this fjord sculpting the softer surface of the bergs which they find in their path.

    (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Surface Tension: Greenland Ice Images.
    DUKAS_4512270_EYE
    Surface Tension: Greenland Ice Images.
    Strong winds channel plumes of water vapour and ice crystals upwards. Eroding an iceberg slowly away. South Greenland.


    (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Surface Tension: Greenland Ice Images.
    DUKAS_4512255_EYE
    Surface Tension: Greenland Ice Images.
    Close-up of an iceberg made of densely formed ice, shows light transmitted through it. Suggesting it as older than the other ice formations surrounding it. The denser the ice, the more it channels light. It is possible that it is older than the other ice formations surrounding it or it may have been formed by water collecting and freezing rapidly. Sermilik Fjord, next to Ingmikerteq Island, near the mouth of Johan Peterson Fjord. South Eastern

    (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Surface Tension: Greenland Ice Images.
    DUKAS_4512253_EYE
    Surface Tension: Greenland Ice Images.
    A massive series of air bubbles trapped inside ice at the point of freezing. Seen in the side of a piece of recently calved hard dense ice. It is possible that it is older than the other ice formations surrounding it or it may have been formed by water collecting and freezing rapidly.

    (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Surface Tension: Greenland Ice Images.
    DUKAS_4512251_EYE
    Surface Tension: Greenland Ice Images.
    An iceberg made of densely formed ice, shows light transmitted through it. Suggesting it as older than the other ice formations surrounding it. The denser the ice, the more it channels light. Sermilik Fjord, next to Ingmikerteq Island, near the mouth of Johan Peterson Fjord. South Eastern Greenland.

    (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Surface Tension: Greenland Ice Images.
    DUKAS_4512250_EYE
    Surface Tension: Greenland Ice Images.
    Ice bergs close to the shore, just south of Timmiarmiut, north of Kap Cort Adelaer, on the South Eastern tip of Greenland. July 2005.

    (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Poland - Feb 2013
    DUKAS_30462814_REX
    Poland - Feb 2013
    Mandatory Credit: Photo by Stuart Forster / Rex Features (2246747s)
    Guard tower outside of Birkenau (Auschwitz II) concentration camp, part of Auschwitz-Birkenau State Museum at Oswiecim. The area around Oswiecim was the site of three Nazi concentration camps during World War Two and used to kill Jews, Poles, gypsies and Russian prisoners of war.
    Poland - Feb 2013

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • Poland - Feb 2013
    DUKAS_30462803_REX
    Poland - Feb 2013
    Mandatory Credit: Photo by Stuart Forster / Rex Features (2246747h)
    Scaffold on which Camp Commander Rudolf Hoess was executed on 16 April 1947 at Auschwitz I concentration camp, part of Auschwitz-Birkenau State Museum at Oswiecim. The area around Oswiecim was the site of three Nazi concentration camps during World War Two and used to kill Jews, Poles, gypsies and Russian prisoners of war.
    Poland - Feb 2013

    (FOTO:DUKAS/REX)

    DUKAS/REX

     

  • Surface Tension: Greenland Ice Images.
    DUKAS_4512863_EYE
    Surface Tension: Greenland Ice Images.
    A melt lake made by melt water filling indents in the ice on the inland ice cap of Western Greenland. Evidence of old lakes which have refrozen is visible in the foreground as faint grey circles.

    (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE

     

  • Surface Tension: Greenland Ice Images.
    DUKAS_4512264_EYE
    Surface Tension: Greenland Ice Images.
    Drips of meltwater refreeze as they trickle down the side of a piece of recently calved hard dense ice. It is possible that it is older than the other ice formations surrounding it or it may have been formed by water collecting and freezing rapidly.

    (FOTO: DUKAS/EYEVINE)

    DUKAS/EYEVINE