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ff Signa by Ole Søndergaard
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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 • [email protected] • Denmark
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FF 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 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-
Sãn Paulo
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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
Brazil
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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-
Caracas
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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
Venezuela
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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-
Nairobi
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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
Kenya
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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
Kingston
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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
Jamaica
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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
Jakarta
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15
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
Indonesia
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16
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
Cuszco
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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
Peru
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19
FF 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 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
Pro Extended Extra LightFF Signa
21
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
Pro Extended Extra Light ItalicFF Signa
22
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
Pro Extended LightFF Signa
23
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
Pro Extended Light ItalicFF Signa
24
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
Pro Extended BookFF Signa
25
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
Uzbekistan
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26
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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27
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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30
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
Havana
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31
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
Cuba
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32
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
Pape’ete
Pro Extended UltraFF Signa
33
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
Tahiti
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CaliforniaCasablanca Morocco
Istanbul TurkeyMontreal Canada
Miami Beach FloridaAcapulcu Mexico
San Francisco United StatesGuayaquil Ecuador
Copenhagen Denmark
Mindanao PhilippinesFagatogo Samoa Island
Orange River Africa
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FF Signa
Pro Condensed
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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
Pro Condensed Extra LightFF Signa
37
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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38
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
Pro Condensed LightFF Signa
39
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
Pro Condensed Light Italic FF Signa
40
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
Pro Condensed BookFF Signa
41
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
Pro Condensed Book Italic FF Signa
42
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
Pro Condensed BoldFF Signa
43
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
Pro Condensed Bold Italic FF Signa
44
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
Pro Condensed Black Italic FF Signa
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
Pro Condensed Extra BlackFF Signa
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
Pro Condensed Extra Black Italic FF Signa
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
Pro Condensed UltraFF Signa
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
Pro Condensed Ultra Italic FF Signa
50
51
FF Signa
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
Pro Slab Extra LightFF Signa
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
Pro Slab Extra Light ItalicFF Signa
54
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
Pro Slab LightFF Signa
55
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
Pro Slab Light ItalicFF Signa
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
Pro Slab Demi Bold ItalicFF Signa
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
Pro Slab BoldFF Signa
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
Pro Slab Bold ItalicFF Signa
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
Pro Slab Black ItalicFF Signa
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
Pro Slab Extra BlackFF Signa
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
Pro Slab Extra Black ItalicFF Signa
66
67
FF Signa
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
Pro Serif LightFF Signa
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
Pro Serif Light ItalicFF Signa
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
Pro Serif Book ItalicFF Signa
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
Pro Serif Semi Bold ItalicFF Signa
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
Pro Serif BoldFF Signa
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
Pro Serif Bold ItalicFF Signa
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
Pro Serif Black ItalicFF Signa
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
FF Signa
Pro Stencil &Pro Serif Stencil
80
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
Stencil Pro BoldFF Signa
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
Stencil Pro BlackFF Signa
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
84
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
Serif Pro Stencil BoldFF Signa
85
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
Serif Pro Stencil BlackFF Signa
86
87
88
89
ff Signa by Ole Søndergaard
90
91
ff Signa by Ole Søndergaard
ff Signa Pro ff Signa Slab ff Signa Stencil ff Signa Serif ff Signa Serif Stencil
www.osgrafik.dk • [email protected] • Denmark
92
93
FF Signa
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