1 ff Signa by Ole Søndergaard · 1 ff Signa by Ole Søndergaard ff Signa Pro ff Signa Slab ff Signa Stencil ff Signa Serif ff Signa Serif Stencil • osgrafik@osgrafik.dk • Denmark
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ff Signa by Ole Søndergaard
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ff Signa by Ole Søndergaard
ff Signa Pro ff Signa Slab ff Signa Stencil ff Signa Serif ff Signa Serif Stencil
www.osgrafik.dk • osgrafik@osgrafik.dk • Denmark
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along thecoast of Canada. Every year some 400 ice-
Fagatogo
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along thecoast of Canada. Every year some 400 ice-
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along thecoast of Canada. Every year some 400
Samoa
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along thecoast of Canada. Every year some 400 ice-
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along thecoast of Canada. Every year some 400 ice-
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along thecoast of Canada. Every year some 400
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along thecoast of Canada. Every year some 400 ice-
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along thecoast of Canada. Every year some 400 ice-
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along thecoast of Canada. Every year some 400
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along thecoast of Canada. Every year some 400 ice-
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along thecoast of Canada. Every year some 400 ice-
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along thecoast of Canada. Every year some 400 icebergs
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs survive this journey and reach the48th parallel, where the Grand
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs survive this journey and reach the48th parallel, where the Grand
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs survive this journey and reach the48th parallel, where the Grand
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs survive this journey and reach the48th parallel, where the Grand
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs survive this journey and reach the48th parallel, where the Grand
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs survive this journey and reach the48th parallel, where the Grand
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs survive this journey and reach the48th parallel, where the Grand
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs survive this journey and reach the48th parallel, where the Grand
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs survive this journey and reach the48th parallel, where the Grand
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice that the heat of the sun can not melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from
Kinshasa
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice that the heat of the sun can not melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice that the heat of the sun can not melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from
Congo
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice that the heat of the sun can not melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from
Miami
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice that the heat of the sun can not melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice that the heat of the sun can not melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from
Florida
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun can not melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the
Bukhara
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun can not melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun can not melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun can not melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the
Houston
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun can not melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun can not melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the
Texas
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun can not melt the snow. The resulting drop in tem-perature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Cur
Århus
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun can not melt the snow. The resulting drop in tem-perature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Cur
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun can not melt the snow. The resulting drop in tem-perature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Cur
Denmark
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun can not melt the snow. The resulting drop in tem-perature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Cur
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun can not melt the snow. The resulting drop in tem-perature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Cur
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun can not melt the snow. The resulting drop in tem-perature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Cur
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun can not melt the snow. The resulting drop in tem-perature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Cur
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun can not melt the snow. The resulting drop in tem-perature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Cur
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun can not melt the snow. The resulting drop in tem-perature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Cur
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CaliforniaCasablanca Morocco
Istanbul TurkeyMontreal Canada
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Green-landic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs sur-
Unawatuna
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Green-landic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs sur-
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Green-landic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs sur-
Sri Lanka
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Green-landic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs sur-
Abidjan
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Green-landic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs sur-
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Green-landic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs sur-
Cotê ďIvoire
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Green-landic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs sur-
Kuala Lumpur
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Green-landic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs sur-
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Green-landic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs sur-
Malaysia
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Green-landic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs sur-
Yaounde
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Green-landic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs sur-
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Green-landic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every year some 400 icebergs sur-
Cameroun
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every
Beijing
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45
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the icebergs from the west coast of Greenland and move south along the coast of Canada. Every
China
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46
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsist-ence of the ice cap. Ice drift with the East Greenlandic Current around southern Green-land and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the ice-
Helsinki
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47
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsist-ence of the ice cap. Ice drift with the East Greenlandic Current around southern Green-land and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the ice-
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsist-ence of the ice cap. Ice drift with the East Greenlandic Current around southern Green-land and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the ice-
Finland
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48
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsist-ence of the ice cap. Ice drift with the East Greenlandic Current around southern Green-land and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs
Thimphu
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49
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsist-ence of the ice cap. Ice drift with the East Greenlandic Current around southern Green-land and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsist-ence of the ice cap. Ice drift with the East Greenlandic Current around southern Green-land and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs
Bhutan
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50
51
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Pro Slab
52
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
Бангкок
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53
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
Таиланд
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
Manila
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
Philippines
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56
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
Madrid
Pro Slab BookFF Signa
57
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
Spain
Pro Slab Book ItalicFF Signa
58
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
Sydney
Pro Slab Demi BoldFF Signa
59
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
Australia
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60
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around south Greenland and on to Baffin Bay with the West Greenlandic current.
Athens
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61
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around south Greenland and on to Baffin Bay with the West Greenlandic current.
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around south Greenland and on to Baffin Bay with the West Greenlandic current.
Greece
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62
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around south Greenland and on to Baffin Bay with the West Greenlandic current.
Kyoto
Pro Slab BlackFF Signa
63
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around south Greenland and on to Baffin Bay with the West Greenlandic current.
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around south Greenland and on to Baffin Bay with the West Greenlandic current.
Japan
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64
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around south Greenland and on to Baffin Bay with the West Greenlandic current.
Москва
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65
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around south Greenland and on to Baffin Bay with the West Greenlandic current.
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around south Greenland and on to Baffin Bay with the West Greenlandic current.
Россия
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Serif Pro
68
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
Toronto
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69
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
Canada
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70
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
Istanbul
Pro Serif BookFF Signa
71
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
Turkey
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72
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
Riga
Pro Serif Semi BoldFF Signa
73
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
Letland
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74
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
Paris
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75
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Green-land and Canada, they join the icebergs from the west coast of Greenland and
France
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76
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around south Greenland and on to Baffin Bay with the West Greenlandic current.
Isfahan
Pro Serif BlackFF Signa
77
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around south Greenland and on to Baffin Bay with the West Greenlandic current.
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around south Greenland and on to Baffin Bay with the West Greenlandic current.
Iran
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78
Kathmandu Nepal
Birmingham England
Thessanoliki Greece
Unawatuna Sri Lanka
Jaisalmer RajasthanHonolulu Hawaii
Barranquilla Colombia
Antarctica
Краматорськ УкраїніKuala Lumpur Malaysia
Новгород Россия
Sumatra Indonesia
Samarkand Uzbekisthan
Rio de Janeiro Brazil
79
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Pro Stencil &Pro Serif Stencil
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the ice-bergs from the west coast of Green-
Jaisalmer
Stencil Pro BookFF Signa
81
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the ice-bergs from the west coast of Green-
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the ice-bergs from the west coast of Green-
Rajasthan
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82
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join bergs from the west coast of Green-
London
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83
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join bergs from the west coast of Green-
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main reasons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between Greenland and Canada, they join the ice-bergs from the west coast of Green-
England
Serif Pro Stencil BookFF Signa
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main rea-sons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between
Lisbon
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body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main rea-sons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between
body of ice over a period of thousands of years. When a layer of snow reaches a certain size and depth, it begins to create its own climate. The surface of the ice reflects the sunlight back into space, so that the heat of the sun cannot melt the snow. The resulting drop in temperature as well as the persistent snowfall are the main rea-sons for the continued exsistence of the ice cap. Ice drift with the East Greenlandic Current around southern Greenland and on to Baffin Bay with the West Greenlandic current. Here, between
Portugal
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ff Signa by Ole Søndergaard
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ff Signa by Ole Søndergaard
ff Signa Pro ff Signa Slab ff Signa Stencil ff Signa Serif ff Signa Serif Stencil
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