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DUKAS_4512834_EYE
Surface Tension: Greenland Ice Images.
The edge of a melt lake South of Swiss Camp occuring in the ice cap, near where it joins The Ilulissat glacier photographed, during a flight Eastwards from Ilulissat, west Greenland coast. Ice has formed on the surface, refreezing in the sub-zero temperatures.
(FOTO: DUKAS/EYEVINE)
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Surface Tension: Greenland Ice Images.
The edge or 'shore-line' of a melt lake, made by melt water filling indents in the ice on the inland ice cap of Western Greenland. The cracks are visible on the lake's bed, through which it is feared melt water may seep to the bottom of the ice cap.
(FOTO: DUKAS/EYEVINE)
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DUKAS_4512818_EYE
Surface Tension: Greenland Ice Images.
The surface of a melt lake made by melt water filling indents in the ice on the inland ice cap of Western Greenland. The strips of white are fingers of ice that have refrozen on the water's colder surface in the sub zero temperatures.
(FOTO: DUKAS/EYEVINE)
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DUKAS_4512813_EYE
Surface Tension: Greenland Ice Images.
Melt rivers flow away from the edges of the retreated glacier of Frederiksh (FOTO: DUKAS/EYEVINE)
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Surface Tension: Greenland Ice Images.
Melt rivers flow away from the edges of the retreated glacier of Frederiksh (FOTO: DUKAS/EYEVINE)
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DUKAS_4512790_EYE
Surface Tension: Greenland Ice Images.
Patterns made by melt rivers and pieces of ice that form the edges of the retreated glacier of Frederiksh (FOTO: DUKAS/EYEVINE)
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DUKAS_4512783_EYE
Surface Tension: Greenland Ice Images.
Patterns made by melt rivers and pieces of ice that form the edges of the retreated glacier of Frederiksh (FOTO: DUKAS/EYEVINE)
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DUKAS_4512777_EYE
Surface Tension: Greenland Ice Images.
Various features apparent in the Helheim glacier, on Eastern Greenland. Photographs made close to where the glacier feeds into the Sermalik Fjord. This is a melt pool made by a glacier which has receded and melted away. The lines in the earth bank are sculpted by the movement of the glacier's retreat.
(FOTO: DUKAS/EYEVINE)
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Surface Tension: Greenland Ice Images.
The glacier close to the town of Narsaq at 61 (FOTO: DUKAS/EYEVINE)
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Surface Tension: Greenland Ice Images.
'Pancake Ice' close to the town of Narsaq (South of Nulugssuaq and North of Manitsoq). visited as a tourist spot. Greenlanders ocasionally take tourists to see the glacier. The pancake is covered in a light dirty coloured dust.
(FOTO: DUKAS/EYEVINE)
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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)
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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)
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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)
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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)
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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)
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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)
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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)
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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)
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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)
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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)
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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)
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RETRO - Victoria Station in London 1951
Victoria Station , London
A young boy sitting down with a messy face and hands eating .
1951 (FOTO:DUKAS/TOPFOTO)
(c) Dukas -
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Mono Print
WINTER'S TALE IN FOUR ICY EPISODES
29 January 1950
This grim tale of treachery, opportunism, disillusion and good comradeship unfolded on the gleaming ice of the frozen pond on Wimbledon Common, london today ( Sunday)
Villain of he piece was the ice, which enticed crowds of skaters on to its smiling surface but singled out Betty Dodd and William Sowan as its victims, when it cracked and drew them into its freezing depths.
Opportunist was Mr Samuelson Movietone cameraman, who seized his chance for some good pictures but was sadly let down when he too sank through a suddenly yeilding surface.
Hero of this frosty melodrama was the St John's Ambulance man who threw the strugglers a rope and was ready with a flask of hot tea when they floundered to the bank.
EPISODE THREE: A St John's Ambulance Man wading in the icy water throws a succouring rope to Betty Dodd and William Sowan splashing to the bank. (FOTO:DUKAS/TOPFOTO)
TopFoto